On the public citation graph
High-pressure Partial Melting of Mafic Lithologies in the Mantle
0 signed · 367 inferred · view as graph
Inferred edges come from two machine sources: sweeps of open repository metadata (mostly SSRN and Zenodo), and a bulk OpenAlex citation snapshot. Every row below is labelled with the one it came from. Neither is a complete citation index — absence here is not evidence of absence.
Is this your work? Sign in with ORCID and put your name on the
claims that are yours.
Reference health. See whether every reference in this work resolves to a
known work and none has been retracted — and get a dated CiteStamped
badge you can embed.
What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1002/9781118782064.ch5openalex-snapshot
Solidus Curves, Mantle Plumes, and Magma Generation Beneath Hawaii
inferredcites →https://doi.org/10.1007/bf00310752openalex-snapshot
Petrogenesis of Hawaiian tholeiites: 1, phase equilibria constraints
inferredcites →https://doi.org/10.1007/bf00310753openalex-snapshot
Petrogenesis of Hawaiian tholeiites: 2, aspects of dynamic melt segregation
inferredcites →https://doi.org/10.1007/bf00320905openalex-snapshot
An experimental study of two garnet pyroxenite xenoliths from the Bullenmerri and Gnotuk Maars of western Victoria, Australia
inferredcites →https://doi.org/10.1007/bf00371277openalex-snapshot
Les p�ridotites et les pyrox�nolites du massif ultrabasique des Beni Bouchera: une �tude exp�rimentale entre 1100 et 1550� C, sous 15 � 30 kilobars de pression s�che
inferredcites →https://doi.org/10.1007/bf00372159openalex-snapshot
Liquidus phase relations on the join diopside-forsterite-anorthite from 1 atm to 20 kbar: Their bearing on the generation and crystallization of basaltic magma
inferredcites →https://doi.org/10.1007/bf00381447openalex-snapshot
Anhydrous melting of peridotite at 0?15 Kb pressure and the genesis of tholeiitic basalts
inferredcites →https://doi.org/10.1007/bf00572166openalex-snapshot
Anhydrous P-T phase relations of near-primary high-alumina basalt from the South Sandwich Islands
inferredcites →https://doi.org/10.1007/bf00636522openalex-snapshot
The transition between spinel lherzolite and garnet lherzolite, and its use as a Geobarometer
inferredcites →https://doi.org/10.1007/s00410-002-0376-3openalex-snapshot
MORB melting processes beneath the southern Mid-Atlantic Ridge (40–55°S): a role for mantle plume-derived pyroxenite
inferredcites →https://doi.org/10.1007/s004100000134openalex-snapshot
Experimental study of the phase and melting relations of homogeneous basalt + peridotite mixtures and implications for the petrogenesis of flood basalts
inferredcites →https://doi.org/10.1007/s004100050184openalex-snapshot
A possible role for garnet pyroxenite in the origin of the "garnet signature" in MORB
inferredcites →https://doi.org/10.1007/s004100050374openalex-snapshot
Melt/harzburgite reaction in the petrogenesis of tholeiitic magma from Kilauea volcano, Hawaii
inferredcites →https://doi.org/10.1007/s004100100295openalex-snapshot
Experimental study of clinopyroxenite partial melting and the origin of ultra-calcic melt inclusions
inferredcites →https://doi.org/10.1016/0009-2541(94)00140-4openalex-snapshot
The composition of the Earth
inferredcites →https://doi.org/10.1016/0012-821x(77)90012-7openalex-snapshot
A coesite-sanidine grospydite from the Roberts Victor kimberlite
inferredcites →https://doi.org/10.1016/0012-821x(81)90182-5openalex-snapshot
Oceanic island Pb: Two-stage histories and mantle evolution
inferredcites →https://doi.org/10.1016/0012-821x(82)90161-3openalex-snapshot
Mantle plumes from ancient oceanic crust
inferredcites →https://doi.org/10.1016/0012-821x(93)90077-mopenalex-snapshot
Partial melting of dry peridotites at high pressures: Determination of compositions of melts segregated from peridotite using aggregates of diamond
inferredcites →https://doi.org/10.1016/0012-821x(95)00097-vopenalex-snapshot
Incompatible trace elements in OIB and MORB and source enrichment in the sub-oceanic mantle
inferredcites →https://doi.org/10.1016/0012-821x(95)00122-sopenalex-snapshot
Melt generation by isentropic mantle upwelling
inferredcites →https://doi.org/10.1016/0012-8252(68)90147-5openalex-snapshot
The bearing of phase equilibria studies in synthetic and natural systems on the origin and evolution of basic and ultrabasic rocks
inferredcites →https://doi.org/10.1016/0016-7037(94)90116-3openalex-snapshot
Determining the composition of high-pressure mantle melts using diamond aggregates
inferredcites →https://doi.org/10.1016/0016-7037(95)00111-copenalex-snapshot
Liquidus equilibria of some primary lunar and terrestrial melts in the garnet stability field
inferredcites →https://doi.org/10.1016/0040-1951(89)90154-6openalex-snapshot
An open boundary between lower continental crust and mantle: its role in crust formation and crustal recycling
inferredcites →https://doi.org/10.1016/0198-0254(86)91143-xopenalex-snapshot
Trace element and isotopic geochemistry of lavas from Haleakala volcano, East Maui, Hawaii: implications for the origin of Hawaiian basalts
inferredcites →https://doi.org/10.1016/0967-0653(96)81998-3openalex-snapshot
10.1016/0967-0653(96)81998-3
inferredcites →https://doi.org/10.1016/s0012-821x(03)00538-7openalex-snapshot
High-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basalts
inferredcites →https://doi.org/10.1016/s0012-821x(97)00089-7openalex-snapshot
Plume-lithosphere interactions in the ocean basins: constraints from the source mineralogy
inferredcites →https://doi.org/10.1016/s0012-821x(98)00156-3openalex-snapshot
Melting experiments on homogeneous mixtures of peridotite and basalt: application to the genesis of ocean island basalts
inferredcites →https://doi.org/10.1016/s0012-821x(98)00157-5openalex-snapshot
Origin of the Columbia River basalts: melting model of a heterogeneous plume head
inferredcites →https://doi.org/10.1016/s0031-9201(97)00130-1openalex-snapshot
Melting study of an alkali basalt JB-1 up to 12.5 GPa: behavior of potassium in the deep mantle
inferredcites →https://doi.org/10.1029/1999gc000013openalex-snapshot
Assessing the presence of garnet‐pyroxenite in the mantle sources of basalts through combined hafnium‐neodymium‐thorium isotope systematics
inferredcites →https://doi.org/10.1029/2000gc000070openalex-snapshot
Mantle solidus: Experimental constraints and the effects of peridotite composition
inferredcites →https://doi.org/10.1029/2000gc000089openalex-snapshot
New experimental observations on the anhydrous solidus for peridotite KLB‐1
inferredcites →https://doi.org/10.1029/2000jb000118openalex-snapshot
Partial melting experiments on a MORB‐like pyroxenite between 2 and 3 GPa: Constraints on the presence of pyroxenite in basalt source regions from solidus location and melting rate
inferredcites →https://doi.org/10.1029/2000jb900357openalex-snapshot
On the conditions for lower crustal convective instability
inferredcites →https://doi.org/10.1029/2002jb002048openalex-snapshot
Origin of ocean island basalts: A new perspective from petrology, geochemistry, and mineral physics considerations
inferredcites →https://doi.org/10.1029/91jb02840openalex-snapshot
Primary magmas of mid‐ocean ridge basalts 1. Experiments and methods
inferredcites →https://doi.org/10.1029/91jb02841openalex-snapshot
Primary magmas of mid‐ocean ridge basalts 2. Applications
inferredcites →https://doi.org/10.1029/92jb00068openalex-snapshot
Petrology, elasticity, and composition of the mantle transition zone
inferredcites →https://doi.org/10.1029/92jb02072openalex-snapshot
Petrology of the East Pacific Rise crust and upper mantle exposed in Hess deep (eastern equatorial Pacific)
inferredcites →https://doi.org/10.1029/93jb03205openalex-snapshot
Melting phase relations of an anhydrous mid‐ocean ridge basalt from 3 to 20 GPa: Implications for the behavior of subducted oceanic crust in the mantle
inferredcites →https://doi.org/10.1029/94jb01406openalex-snapshot
Melting experiments on anhydrous peridotite KLB‐1 from 5.0 to 22.5 GPa
inferredcites →https://doi.org/10.1029/96jb00988openalex-snapshot
Melting of mantle peridotite at pressures approaching the spinel to garnet transition: Application to mid‐ocean ridge basalt petrogenesis
inferredcites →https://doi.org/10.1029/96jb03892openalex-snapshot
High μ (HIMU) ocean island basalts in southern Polynesia: New evidence for whole mantle scale recycling of subducted oceanic crust
inferredcites →https://doi.org/10.1029/97gl02956openalex-snapshot
Partial melt compositions of carbonated peridotite at 3 GPa and role of CO2 in alkali‐basalt magma generation
inferredcites →https://doi.org/10.1029/gm095openalex-snapshot
Earth Processes: Reading the Isotopic Code
inferredcites →https://doi.org/10.1029/gm095p0109openalex-snapshot
Partial Melting of a Fertile Mantle Peridotite at High Pressures: An Experimental Study Using Aggregates of Diamond
inferredcites →https://doi.org/10.1029/gm128p0403openalex-snapshot
Melting process in the Hawaiian plume: An experimental study
inferredcites →https://doi.org/10.1029/jb090ib10p08743openalex-snapshot
Trace element and isotopic geochemistry of lavas from Haleakala Volcano, east Maui, Hawaii: Implications for the origin of Hawaiian basalts
inferredcites →https://doi.org/10.1029/jb092ib08p08089openalex-snapshot
Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness
inferredcites →https://doi.org/10.1029/jb093ib05p04171openalex-snapshot
Solidus curves, mantle plumes, and magma generation beneath Hawaii
inferredcites →https://doi.org/10.1029/jb094ib04p04205openalex-snapshot
Constraints on the abundance of eclogite in the upper mantle
inferredcites →https://doi.org/10.1029/jb095ib10p15817openalex-snapshot
Phase relations of aluminum‐undepleted and aluminum‐depleted komatiites at pressures of 4–12 GPa
inferredcites →https://doi.org/10.1038/16225openalex-snapshot
The fate of subducted basaltic crust in the Earth's lower mantle
inferredcites →https://doi.org/10.1038/332823a0openalex-snapshot
Majorite fractionation recorded in the geochemistry of peridotites from South Africa
inferredcites →https://doi.org/10.1038/382415a0openalex-snapshot
Major-element variability in the Hawaiian mantle plume
inferredcites →https://doi.org/10.1038/385219a0openalex-snapshot
Mantle geochemistry: the message from oceanic volcanism
inferredcites →https://doi.org/10.1038/nature00798openalex-snapshot
Mineralogy of the mid-ocean-ridge basalt source from neodymium isotopic composition of abyssal peridotites
inferredcites →https://doi.org/10.1038/nature01704openalex-snapshot
Magmatic and amagmatic seafloor generation at the ultraslow-spreading Gakkel ridge, Arctic Ocean
inferredcites →https://doi.org/10.1086/627970openalex-snapshot
The Composition of Liquids Formed by Partial Melting of Eclogites at High Temperatures and Pressures
inferredcites →https://doi.org/10.1093/petroj/39.1.29openalex-snapshot
Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere
inferredcites →https://doi.org/10.1093/petroj/39.1.3openalex-snapshot
Liquidus Phase Relations in the CaO-MgO-Al2O3-SiO2 System at 3.0 GPa: the Aluminous Pyroxene Thermal Divide and High-Pressure Fractionation of Picritic and Komatiitic Magmas
inferredcites →https://doi.org/10.1093/petrology/15.1.1openalex-snapshot
Geochemical and High Pressure Experimental Studies of Garnet Pyroxenite and Pyroxene Granulite Xenoliths from the Delegate Basaltic Pipes, Australia
inferredcites →https://doi.org/10.1093/petrology/29.3.625openalex-snapshot
The Volume and Composition of Melt Generated by Extension of the Lithosphere
inferredcites →https://doi.org/10.1093/petrology/3.3.342openalex-snapshot
Origin of Basalt Magmas: An Experimental Study of Natural and Synthetic Rock Systems
inferredcites →https://doi.org/10.1093/petrology/32.5.1021openalex-snapshot
Partial Melt Distributions from Inversion of Rare Earth Element Concentrations
inferredcites →https://doi.org/10.1093/petrology/35.2.329openalex-snapshot
Melting Behavior of Simplified Lherzolite in the System CaO-MgO-Al2O3-SiO2-Na2O from 7 to 35 kbar
inferredcites →https://doi.org/10.1093/petrology/41.1.3openalex-snapshot
Liquidus Phase Relations in the System CaO–MgO–Al2O3–SiO2 at 2·0 GPa: Applications to Basalt Fractionation, Eclogites, and Igneous Sapphirine
inferredcites →https://doi.org/10.1093/petrology/43.10.1857openalex-snapshot
Plume-Associated Ultramafic Magmas of Phanerozoic Age
inferredcites →https://doi.org/10.1093/petrology/egg074openalex-snapshot
Anhydrous Partial Melting Experiments on MORB-like Eclogite: Phase Relations, Phase Compositions and Mineral-Melt Partitioning of Major Elements at 2-3 GPa
inferredcites →https://doi.org/10.1093/petrology/special_volume.1.379openalex-snapshot
Anhydrous Partial Melting of Peridotite from 8 to 35 kb and the Petrogenesis of MORB
inferredcites →https://doi.org/10.1098/rsta.1997.0010openalex-snapshot
A review of melt migration processes in the adiabatically upwelling mantle beneath oceanic spreading ridges
inferredcites →https://doi.org/10.1126/science.287.5451.278openalex-snapshot
Rutile-Bearing Refractory Eclogites: Missing Link Between Continents and Depleted Mantle
inferredcites →https://doi.org/10.1130/0091-7613(2003)031<0481:amgbpm>2.0.co;2openalex-snapshot
Alkalic magmas generated by partial melting of garnet pyroxenite
inferredcites →https://doi.org/10.1144/sjg03010067openalex-snapshot
Formation and fractionation of basic magmas at high pressures
inferredcites →https://doi.org/10.2475/001c.125224openalex-snapshot
The System Forsterite Diopside-Silica With and Without Water at High Pressures
inferredcites →https://doi.org/10.2475/ajs.265.6.475openalex-snapshot
Melting and phase relations in an anhydrous basalt to 40 kilobars
inferredcites →https://doi.org/10.2475/ajs.302.9.806openalex-snapshot
Intermediate-P/T type Archean metamorphism of the Isua supracrustal belt: Implications for secular change of geothermal gradients at subduction zones and for Archean plate tectonics
inferredcites →https://doi.org/10.2747/0020-6814.44.11.988openalex-snapshot
Petrology and Geochemistry of MORB and OIB in the Mid-Archean North Pole Region, Pilbara Craton, Western Australia: Implications for the Composition and Temperature of the Upper Mantle at 3.5 Ga
inferredcites →https://doi.org/10.2973/odp.proc.sr.118.128.1991openalex-snapshot
Lithostratigraphic Evolution of an In-Situ Section of Oceanic Layer 3
inferredcites →https://doi.org/10.5169/seals-59286openalex-snapshot
Reactions between eclogite and peridotite : mantle refertilisation by subduction of oceanic crust
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.2139/ssrn.4769607openalex-extracted
Geochronology and Geochemistry of the Camacan and Itaju Do Colônia Mafic Dykes Swarms, Eastern Brazil: Insights into Their Mantle Source and Geodynamic Implications
inferred← citeshttps://doi.org/10.1002/2013gc005132openalex-snapshot
Diverse magmatic effects of subducting a hot slab in SW Japan: Results from forward modeling
inferred← citeshttps://doi.org/10.1002/2014gc005333openalex-snapshot
Trace element mass balance in hydrous adiabatic mantle melting: The Hydrous Adiabatic Mantle Melting Simulator version 1 (HAMMS1)
inferred← citeshttps://doi.org/10.1002/2014gc005486openalex-snapshot
Geochemical insights into the role of metasomatic hornblendite in generating alkali basalts
inferred← citeshttps://doi.org/10.1002/2014gc005606openalex-snapshot
Ocean B asalt S imulator version 1 ( OBS 1): Trace element mass balance in adiabatic melting of a pyroxenite‐bearing peridotite
inferred← citeshttps://doi.org/10.1002/2015gc005885openalex-snapshot
Supercontinental inheritance and its influence on supercontinental breakup: The C entral A tlantic M agmatic P rovince and the breakup of P angea
inferred← citeshttps://doi.org/10.1002/2015jb012762openalex-snapshot
The role of pyroxenite in basalt genesis: Melt‐PX, a melting parameterization for mantle pyroxenites between 0.9 and 5 GPa
inferred← citeshttps://doi.org/10.1002/2016gl070346openalex-snapshot
Geodynamics of paleo‐Pacific plate subduction constrained by the source lithologies of Late Mesozoic basalts in southeastern China
inferred← citeshttps://doi.org/10.1002/2017jb014023openalex-snapshot
Magma‐magma interaction in the mantle beneath eastern China
inferred← citeshttps://doi.org/10.1002/9781119473206.ch5openalex-snapshot
Redox Melting in the Mantle
inferred← citeshttps://doi.org/10.1002/9781119528609.ch6openalex-snapshot
Tracking the Evolution of Magmas from Heterogeneous Mantle Sources to Eruption
inferred← citeshttps://doi.org/10.1002/gj.3150openalex-snapshot
Petrogenesis of basalt from the middle Okinawa Trough: New insights from olivine‐hosted melt inclusions
inferred← citeshttps://doi.org/10.1002/gj.3331openalex-snapshot
Major, trace element, and SrNd isotopic geochemistry of Cenozoic basalts in Central‐North and East Mongolia : Petrogenesis and tectonic implication
inferred← citeshttps://doi.org/10.1002/gj.5222openalex-snapshot
Source Lithology Characteristics of Different Tectonic Stages of Mariana Subduction Zone: Insights From Major and Trace Element Compositions of Olivine From Basalts
inferred← citeshttps://doi.org/10.1007/978-1-4020-5750-2_7openalex-snapshot
A Geochemical and Petrological View of Mantle Plume
inferred← citeshttps://doi.org/10.1007/s00410-004-0649-0openalex-snapshot
The effect of bulk composition on the solidus of carbonated eclogite from partial melting experiments at 3 GPa
inferred← citeshttps://doi.org/10.1007/s00410-006-0169-1openalex-snapshot
Intraplate volcanism in New Zealand: the role of fossil plume material and variable lithospheric properties
inferred← citeshttps://doi.org/10.1007/s00410-008-0304-2openalex-snapshot
Hydrogen partitioning between melt, clinopyroxene, and garnet at 3 GPa in a hydrous MORB with 6 wt.% H2O
inferred← citeshttps://doi.org/10.1007/s00410-008-0345-6openalex-snapshot
Pyroxenite xenoliths from Marsabit (Northern Kenya): evidence for different magmatic events in the lithospheric mantle and interaction between peridotite and pyroxenite
inferred← citeshttps://doi.org/10.1007/s00410-010-0573-4openalex-snapshot
Formation of cratonic subcontinental lithospheric mantle and complementary komatiite from hybrid plume sources
inferred← citeshttps://doi.org/10.1007/s00410-012-0810-0openalex-snapshot
Constraints from melt inclusions and their host olivines on the petrogenesis of Oligocene-Early Miocene Xindian basalts, Chifeng area, North China Craton
inferred← citeshttps://doi.org/10.1007/s00410-013-0899-9openalex-snapshot
Melts of garnet lherzolite: experiments, models and comparison to melts of pyroxenite and carbonated lherzolite
inferred← citeshttps://doi.org/10.1007/s00410-014-1052-0openalex-snapshot
The role of eclogite in the mantle heterogeneity at Cape Verde
inferred← citeshttps://doi.org/10.1007/s00410-016-1310-4openalex-snapshot
Continuous supply of recycled Pacific oceanic materials in the source of Cenozoic basalts in SE China: the Zhejiang case
inferred← citeshttps://doi.org/10.1007/s00410-017-1359-8openalex-snapshot
Volatile (Cl, F and S) and major element constraints on subduction-related mantle metasomatism along the alkaline basaltic backarc, Payenia, Argentina
inferred← citeshttps://doi.org/10.1007/s00410-017-1387-4openalex-snapshot
Partial melting of secondary pyroxenite at 1 and 1.5 GPa, and its role in upwelling heterogeneous mantle
inferred← citeshttps://doi.org/10.1007/s00410-017-1410-9openalex-snapshot
Unravelling the magmatic system beneath a monogenetic volcanic complex (Jagged Rocks Complex, Hopi Buttes, AZ, USA)
inferred← citeshttps://doi.org/10.1007/s00410-017-1431-4openalex-snapshot
Shallow-level differentiation of phonolitic lavas from Sumaco Volcano, Ecuador
inferred← citeshttps://doi.org/10.1007/s00410-019-1640-0openalex-snapshot
Origin of pyroxenites in the oceanic mantle and their implications on the reactive percolation of depleted melts
inferred← citeshttps://doi.org/10.1007/s00410-020-01687-zopenalex-snapshot
Geochemistry of continental alkali basalts in the Sabzevar region, northern Iran: implications for the role of pyroxenite in magma genesis
inferred← citeshttps://doi.org/10.1007/s00410-023-02052-6openalex-snapshot
The origin of Na-alkaline lavas revisited: new constraints from experimental melting of amphibole-rich metasomes+lherzolite at uppermost mantle pressure
inferred← citeshttps://doi.org/10.1007/s00410-023-02076-yopenalex-snapshot
Pyroxenite–harzburgite sequences in the Dazhuqu ophiolite (Southern Tibet) formed through hydrous melt infiltration and melt–peridotite reaction
inferred← citeshttps://doi.org/10.1007/s00410-024-02099-zopenalex-snapshot
Formation and prolonged preservation of dense arc root cumulates: insights from retrograded eclogite xenoliths in the western Yangtze craton
inferred← citeshttps://doi.org/10.1007/s00410-024-02112-5openalex-snapshot
Deep recycling of crustal materials by the Hainan mantle plume: evidence from Zn–Sr–Nd–Pb isotopes of Hainan Island basalts
inferred← citeshttps://doi.org/10.1007/s00410-024-02172-7openalex-snapshot
Petrogenesis of the Deccan high-Mg basalts and picrites
inferred← citeshttps://doi.org/10.1007/s00410-024-02186-1openalex-snapshot
W-Fe isotopes argue against OIB-like basalts in Inner Mongolia originating from primordial peridotite mantle
inferred← citeshttps://doi.org/10.1007/s00710-010-0115-9openalex-snapshot
Mineral chemical evidence for extremely magnesian subalkaline melts from the Antarctic extension of the Karoo large igneous province
inferred← citeshttps://doi.org/10.1007/s11430-007-0139-0openalex-snapshot
Petrogenetic significance of high Fe/Mn ratios of the Cenozoic basalts from eastern China
inferred← citeshttps://doi.org/10.1007/s11430-009-0134-8openalex-snapshot
Remelting of subducted continental lithosphere: Petrogenesis of Mesozoic magmatic rocks in the Dabie-Sulu orogenic belt
inferred← citeshttps://doi.org/10.1007/s11430-017-9090-4openalex-snapshot
Mantle geochemistry: Insights from ocean island basalts
inferred← citeshttps://doi.org/10.1007/s11430-023-1118-3openalex-snapshot
Pyroxenite melting at subduction zone: Implications for the origin of mafic arc magmas
inferred← citeshttps://doi.org/10.1007/s11430-025-1914-3openalex-snapshot
Petrogenesis of andesite: A century of conceptual evolution
inferred← citeshttps://doi.org/10.1007/s11631-021-00454-6openalex-snapshot
Olivine and Cr-spinel as indicators of the petrogenesis and partial melting conditions of the high-MgO ultramafic volcanic rocks from NW Ad Dhala Province—Yemen
inferred← citeshttps://doi.org/10.1007/s12583-021-1464-5openalex-snapshot
Mantle Source Components and Magmatic Evolution for the Comei Large Igneous Province: Evidence from the Early Cretaceous Niangzhong Mafic Magmatism in Tethyan Himalaya
inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.00303-xopenalex-snapshot
Continental Basaltic Rocks
inferred← citeshttps://doi.org/10.1016/b978-0-12-811301-1.00001-0openalex-snapshot
Primary Melt Compositions in the Earth's Mantle
inferred← citeshttps://doi.org/10.1016/j.cageo.2008.07.002openalex-snapshot
CMAS 3D, a new program to visualize and project major elements compositions in the CMAS system
inferred← citeshttps://doi.org/10.1016/j.chemer.2026.126387openalex-snapshot
Petrogenesis of Paleoproterozoic mafic magmatic rocks from Garhwal Lesser Himalayan Sequence: Implications for Precambrian crustal recycling and geodynamic evolution of proto-northern Indian continental margin
inferred← citeshttps://doi.org/10.1016/j.chemer.2026.126394openalex-snapshot
Hybrid pyroxenitic–peridotitic lithospheric mantle beneath the Dharwar Craton recorded by ∼550 Myr of Paleoproterozoic mafic magmatism
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2008.07.016openalex-snapshot
Eocene break-off of the Neo-Tethyan slab as inferred from intraplate-type mafic dykes in the Gaoligong orogenic belt, eastern Tibet
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2012.08.033openalex-snapshot
Geochemical constraints on a mixed pyroxenite–peridotite source for East Pacific Rise basalts
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2013.04.007openalex-snapshot
Payenia volcanic province, southern Mendoza, Argentina: OIB mantle upwelling in a backarc environment
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2013.06.022openalex-snapshot
In-situ trace elements and Li and Sr isotopes in peridotite xenoliths from Kuandian, North China Craton: Insights into Pacific slab subduction-related mantle modification
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2013.10.024openalex-snapshot
Melt–peridotite reactions in upwelling eclogite bodies: Constraints from EM1-type alkaline basalts in Payenia, Argentina
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2015.05.018openalex-snapshot
Melting in the mantle in the presence of carbon: Review of experiments and discussion on the origin of carbonatites
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2015.07.025openalex-snapshot
A model for the activity of silica along the carbonatite–kimberlite–mellilitite–basanite melt compositional joint
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2016.09.035openalex-snapshot
Exploring the role of mantle eclogite at mid-ocean ridges and hotspots: U-series constraints on Jan Mayen Island and the Kolbeinsey Ridge
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2017.05.002openalex-snapshot
An experimental study of trace element distribution during partial melting of mantle heterogeneities
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2019.07.027openalex-snapshot
Ligurian pyroxenite-peridotite sequences (Italy) and the role of melt-rock reaction in creating enriched-MORB mantle sources
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2021.120591openalex-snapshot
Enriched Hf Nd isotopic signature of veined pyroxenite-infiltrated peridotite as a possible source for E-MORB
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2021.120594openalex-snapshot
Multi-stage melting of enriched mantle components along the eastern Gakkel Ridge
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2022.120930openalex-snapshot
Spatial distribution and geochemical characterization of Icelandic mantle end-members: Implications for plume geometry and melting processes
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2022.121137openalex-snapshot
First-row transition elements in pyroxenites and peridotites: A promising tool for constraining mantle source mineralogy
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.122330openalex-snapshot
Rhenium–Os isotopic systematics of late Cenozoic intraplate basaltic rocks from Korea: Implications for recycled slab materials in their mantle source
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.122505openalex-snapshot
A new geochemical database for ocean island basalts: Inferring an OIB mantle source from unevenly sampled oceanic hotspots
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2026.123575openalex-snapshot
40Ar/39Ar geochronology, SrNd isotopes and melting conditions of the Dahongshan alkaline basalts: Constraints on mantle modification beneath the northern Yangtze Craton
inferred← citeshttps://doi.org/10.1016/j.earscirev.2005.03.004openalex-snapshot
How the delamination and detachment of lower crust can influence basaltic magmatism
inferred← citeshttps://doi.org/10.1016/j.earscirev.2016.04.001openalex-snapshot
On the chemical markers of pyroxenite contributions in continental basalts in Eastern China: Implications for source lithology and the origin of basalts
inferred← citeshttps://doi.org/10.1016/j.earscirev.2016.12.006openalex-snapshot
Geochemical and petrological insights into the tectonic origin of the Transmexican Volcanic Belt
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103174openalex-snapshot
Mantle heterogeneity through Zn systematics in oceanic basalts: Evidence for a deep carbon cycling
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103253openalex-snapshot
Melting of a hydrous peridotite mantle source under the Emeishan large igneous province
inferred← citeshttps://doi.org/10.1016/j.earscirev.2026.105489openalex-snapshot
Mantle plume dynamics and Gondwana breakup: Insights from the Comei large igneous province, Tethyan Himalaya
inferred← citeshttps://doi.org/10.1016/j.epsl.2005.10.024openalex-snapshot
Comment on “High-pressure melting experiments on garnet clinopyroxenite and the alkalic to tholeiitic transition in ocean-island basalts” by Keshav et al. [Earth Planet. Sci. Lett. 223 (2004) 365–379]
inferred← citeshttps://doi.org/10.1016/j.epsl.2006.07.016openalex-snapshot
Partial melting experiments of bimineralic eclogite and the role of recycled mafic oceanic crust in the genesis of ocean island basalts
inferred← citeshttps://doi.org/10.1016/j.epsl.2007.10.034openalex-snapshot
Partitioning of U and Th during garnet pyroxenite partial melting: Constraints on the source of alkaline ocean island basalts
inferred← citeshttps://doi.org/10.1016/j.epsl.2007.10.035openalex-snapshot
Hawaiian double volcanic chain triggered by an episodic involvement of recycled material: Constraints from temporal Sr–Nd–Hf–Pb isotopic trend of the Loa-type volcanoes
inferred← citeshttps://doi.org/10.1016/j.epsl.2008.02.012openalex-snapshot
Temporal–compositional trends over short and long time-scales in basalts of the Big Pine Volcanic Field, California
inferred← citeshttps://doi.org/10.1016/j.epsl.2008.09.023openalex-snapshot
Compositions of HIMU, EM1, and EM2 from global trends between radiogenic isotopes and major elements in ocean island basalts
inferred← citeshttps://doi.org/10.1016/j.epsl.2008.11.016openalex-snapshot
Mantle melting and magma supply to the Southeast Indian Ridge: The roles of lithology and melting conditions from U-series disequilibria
inferred← citeshttps://doi.org/10.1016/j.epsl.2010.06.039openalex-snapshot
The deep carbon cycle and melting in Earth's interior
inferred← citeshttps://doi.org/10.1016/j.epsl.2011.01.013openalex-snapshot
Formation of hybrid arc andesites beneath thick continental crust
inferred← citeshttps://doi.org/10.1016/j.epsl.2011.05.040openalex-snapshot
A comparative study of continental vs. intraoceanic arc mantle melting: Experimentally determined phase relations of hydrous primitive melts
inferred← citeshttps://doi.org/10.1016/j.epsl.2012.07.033openalex-snapshot
Garnet clinopyroxenite layers from the mantle sequences of the Northern Apennine ophiolites (Italy): Evidence for recycling of crustal material
inferred← citeshttps://doi.org/10.1016/j.epsl.2012.11.047openalex-snapshot
Mantle refertilization by melts of crustal-derived garnet pyroxenite: Evidence from the Ronda peridotite massif, southern Spain
inferred← citeshttps://doi.org/10.1016/j.epsl.2013.10.039openalex-snapshot
Traces of ancient mafic layers in the Tethys oceanic mantle
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.05.025openalex-snapshot
Fractionation of highly siderophile elements in refertilized mantle: Implications for the Os isotope composition of basalts
inferred← citeshttps://doi.org/10.1016/j.epsl.2015.03.033openalex-snapshot
Seismic wave speed structure of the Ontong Java Plateau
inferred← citeshttps://doi.org/10.1016/j.epsl.2015.06.013openalex-snapshot
Combined petrological, geochemical and isotopic modeling of a plume source: Example of Gambier Island, Pitcairn chain
inferred← citeshttps://doi.org/10.1016/j.epsl.2015.12.005openalex-snapshot
Major and trace element and Sr and Nd isotopic results from mantle diapirs in the Oman ophiolite: Implications for off-axis magmatic processes
inferred← citeshttps://doi.org/10.1016/j.epsl.2020.116365openalex-snapshot
Lithospheric memory of subduction in mantle pyroxenite xenoliths from rift-related basalts
inferred← citeshttps://doi.org/10.1016/j.epsl.2021.117330openalex-snapshot
Geophysical and cosmochemical evidence for a volatile-rich Mars
inferred← citeshttps://doi.org/10.1016/j.epsl.2024.118952openalex-snapshot
Partial melting of arclogite and petrogenesis of alkaline-silicate complexes
inferred← citeshttps://doi.org/10.1016/j.gca.2005.11.008openalex-snapshot
A catalytic delamination-driven model for coupled genesis of Archaean crust and sub-continental lithospheric mantle
inferred← citeshttps://doi.org/10.1016/j.gca.2008.02.018openalex-snapshot
Recycled crust controls contrasting source compositions of Mesozoic and Cenozoic basalts in the North China Craton
inferred← citeshttps://doi.org/10.1016/j.gca.2008.10.015openalex-snapshot
The importance of melt extraction for tracing mantle heterogeneity
inferred← citeshttps://doi.org/10.1016/j.gca.2009.01.001openalex-snapshot
Determining melt productivity of mantle sources from 238U–230Th and 235U–231Pa disequilibria; an example from Pico Island, Azores
inferred← citeshttps://doi.org/10.1016/j.gca.2009.10.007openalex-snapshot
Formation of pyroxenite layers in the Totalp ultramafic massif (Swiss Alps) – Insights from highly siderophile elements and Os isotopes
inferred← citeshttps://doi.org/10.1016/j.gca.2011.08.020openalex-snapshot
Understanding melt generation beneath the slow-spreading Kolbeinsey Ridge using 238U, 230Th, and 231Pa excesses
inferred← citeshttps://doi.org/10.1016/j.gca.2012.03.041openalex-snapshot
The influence of source heterogeneity on the U–Th–Pa–Ra disequilibria in post-glacial tholeiites from Iceland
inferred← citeshttps://doi.org/10.1016/j.gca.2012.07.025openalex-snapshot
Inherited Pb isotopic records in olivine antecryst-hosted melt inclusions from Hawaiian lavas
inferred← citeshttps://doi.org/10.1016/j.gca.2013.03.042openalex-snapshot
The geochemical consequences of mixing melts from a heterogeneous mantle
inferred← citeshttps://doi.org/10.1016/j.gca.2013.09.039openalex-snapshot
Partitioning of copper between olivine, orthopyroxene, clinopyroxene, spinel, garnet and silicate melts at upper mantle conditions
inferred← citeshttps://doi.org/10.1016/j.gca.2013.11.031openalex-snapshot
Melt generation beneath Arctic Ridges: Implications from U decay series disequilibria in the Mohns, Knipovich, and Gakkel Ridges
inferred← citeshttps://doi.org/10.1016/j.gca.2014.12.023openalex-snapshot
Petrogenesis of Late Cenozoic basalts from North Hainan Island: Constraints from melt inclusions and their host olivines
inferred← citeshttps://doi.org/10.1016/j.gca.2015.07.036openalex-snapshot
Mid-ocean ridge basalt generation along the slow-spreading, South Mid-Atlantic Ridge (5–11°S): Inferences from 238U–230Th–226Ra disequilibria
inferred← citeshttps://doi.org/10.1016/j.gca.2015.10.006openalex-snapshot
Melt evolution beneath a rifted craton edge: 40 Ar/ 39 Ar geochronology and Sr–Nd–Hf–Pb isotope systematics of primitive alkaline basalts and lamprophyres from the SW Baltic Shield
inferred← citeshttps://doi.org/10.1016/j.gca.2015.12.011openalex-snapshot
231Pa systematics in postglacial volcanic rocks from Iceland
inferred← citeshttps://doi.org/10.1016/j.gca.2016.09.017openalex-snapshot
The effect of bonding environment on iron isotope fractionation between minerals at high temperature
inferred← citeshttps://doi.org/10.1016/j.gca.2017.01.054openalex-snapshot
Primary magmas and mantle sources of Emeishan basalts constrained from major element, trace element and Pb isotope compositions of olivine-hosted melt inclusions
inferred← citeshttps://doi.org/10.1016/j.gca.2018.04.033openalex-snapshot
Genesis of ultra-high pressure garnet pyroxenites in orogenic peridotites and its bearing on the compositional heterogeneity of the Earth’s mantle
inferred← citeshttps://doi.org/10.1016/j.gca.2020.09.033openalex-snapshot
Heavy δ 57Fe in ocean island basalts: A non-unique signature of processes and source lithologies in the mantle
inferred← citeshttps://doi.org/10.1016/j.gca.2022.02.022openalex-snapshot
Origin of low-MgO primitive intraplate alkaline basalts from partial melting of carbonate-bearing eclogite sources
inferred← citeshttps://doi.org/10.1016/j.gca.2022.11.013openalex-snapshot
Barium isotope composition of depleted MORB mantle constrained by basalts from the South Mid-Atlantic Ridge (5–11°S) with implication for recycled components in the convecting upper mantle
inferred← citeshttps://doi.org/10.1016/j.gca.2023.05.003openalex-snapshot
Transcrustal and source processes affecting the chemical characteristics of magmas in a hyperactive volcanic zone
inferred← citeshttps://doi.org/10.1016/j.gca.2025.05.034openalex-snapshot
From crustal protoliths to mantle garnet pyroxenites: insights from Os isotopes and highly siderophile elements
inferred← citeshttps://doi.org/10.1016/j.geogeo.2022.100033openalex-snapshot
Petrogenesis of phlogopite-pyroxenite from Southern India: Implications for the link between Proterozoic subduction- to rift-related arc magmatism
inferred← citeshttps://doi.org/10.1016/j.gr.2009.05.006openalex-snapshot
Magma genesis beneath Northeast Japan arc: A new perspective on subduction zone magmatism
inferred← citeshttps://doi.org/10.1016/j.gr.2013.12.005openalex-snapshot
Tectonic development from oceanic subduction to continental collision: Geochemical evidence from postcollisional mafic rocks in the Hong'an–Dabie orogens
inferred← citeshttps://doi.org/10.1016/j.gr.2016.05.014openalex-snapshot
Origin of Late Cenozoic Abaga–Dalinuoer basalts, eastern China: Implications for a mixed pyroxenite–peridotite source related with deep subduction of the Pacific slab
inferred← citeshttps://doi.org/10.1016/j.gr.2021.08.004openalex-snapshot
Magmatic controls on the mineralization potential of a porphyry Cu system: The case of Jurassic Tongshan skarn Cu deposit in the Qin–Hang Belt, South China
inferred← citeshttps://doi.org/10.1016/j.gsf.2019.02.003openalex-snapshot
Subduction zone geochemistry
inferred← citeshttps://doi.org/10.1016/j.gsf.2020.01.012openalex-snapshot
Constructing the latest Neoproterozoic to Early Paleozoic multiple crust-mantle interactions in western Bainaimiao arc terrane, southeastern Central Asian Orogenic Belt
inferred← citeshttps://doi.org/10.1016/j.gsf.2022.101380openalex-snapshot
Melting of hydrous pyroxenites with alkali amphiboles in the continental mantle: 1. Melting relations and major element compositions of melts
inferred← citeshttps://doi.org/10.1016/j.jsames.2012.07.005openalex-snapshot
Trace element composition of parental magmas from mafic–ultramafic cumulates determined by in situ mineral analyses: The Juquiá mafic–ultramafic alkaline–carbonatite massif, SE Brazil
inferred← citeshttps://doi.org/10.1016/j.jsames.2024.104903openalex-snapshot
Geochronology and geochemistry of the Camacan and itaju do Colônia mafic dykes swarms, Eastern Brazil: Insights into their mantle source and geodynamic implications
inferred← citeshttps://doi.org/10.1016/j.jseaes.2016.12.033openalex-snapshot
Tectonic implications of Early Miocene OIB magmatism in a near-trench setting: The Outer Zone of SW Japan and the northernmost Ryukyu Islands
inferred← citeshttps://doi.org/10.1016/j.jseaes.2019.104185openalex-snapshot
Chemical geodynamics of mafic magmatism above subduction zones
inferred← citeshttps://doi.org/10.1016/j.lithos.2007.06.015openalex-snapshot
Formation of continental flood volcanism — The perspective of setting of melting
inferred← citeshttps://doi.org/10.1016/j.lithos.2007.09.007openalex-snapshot
Petrogenesis of basalts and gabbros from an ancient continent–ocean transition (External Liguride ophiolites, Northern Italy)
inferred← citeshttps://doi.org/10.1016/j.lithos.2009.03.016openalex-snapshot
The basalt-high magnesium andesite association formed by multi-stage partial melting of a heterogeneous source mantle: Evidence from Hirado-Seto, Northwest Kyushu, Southwest Japan
inferred← citeshttps://doi.org/10.1016/j.lithos.2009.07.001openalex-snapshot
Contrasting geochemistry of the Cretaceous volcanic suites in Shandong province and its implications for the Mesozoic lower crust delamination in the eastern North China craton
inferred← citeshttps://doi.org/10.1016/j.lithos.2009.08.002openalex-snapshot
Enriched crustal and mantle components and the role of the lithosphere in generating Paleoproterozoic dyke swarms of the Ungava Peninsula, Canada
inferred← citeshttps://doi.org/10.1016/j.lithos.2011.06.006openalex-snapshot
Zircon Hf–O isotope and whole-rock geochemical constraints on origin of postcollisional mafic to felsic dykes in the Sulu orogen
inferred← citeshttps://doi.org/10.1016/j.lithos.2011.06.010openalex-snapshot
Origin of postcollisional magmatic rocks in the Dabie orogen: Implications for crust–mantle interaction and crustal architecture
inferred← citeshttps://doi.org/10.1016/j.lithos.2011.10.012openalex-snapshot
Comment on “Coupling of basaltic magma evolution and lithospheric seismic structure in the Emeishan Large Igneous Province: MELTS modeling constraints”. by J.Y. Chen, X.S. Yang, L. Xiao, Q. He [Lithos 119 (2010): 61–74]
inferred← citeshttps://doi.org/10.1016/j.lithos.2012.01.010openalex-snapshot
Formation of cratonic lithosphere: An integrated thermal and petrological model
inferred← citeshttps://doi.org/10.1016/j.lithos.2012.06.030openalex-snapshot
Early Cretaceous intermediate-mafic dykes in the Dabie orogen, eastern China: Petrogenesis and implications for crust–mantle interaction
inferred← citeshttps://doi.org/10.1016/j.lithos.2012.11.018openalex-snapshot
Markers of the pyroxenite contribution in the major-element compositions of oceanic basalts: Review of the experimental constraints
inferred← citeshttps://doi.org/10.1016/j.lithos.2013.06.018openalex-snapshot
Multiple exsolutions in a rare clinopyroxene megacryst from the Hannuoba basalt, North China: Implications for subducted slab-related crustal thickening and recycling
inferred← citeshttps://doi.org/10.1016/j.lithos.2013.07.001openalex-snapshot
Metamorphism and melting of picritic crust in the early Earth
inferred← citeshttps://doi.org/10.1016/j.lithos.2014.09.023openalex-snapshot
The role of external fluid in the Shanggusi dynamic granitic magma system, East Qinling, China: Quantitative integration of textural and chemical data
inferred← citeshttps://doi.org/10.1016/j.lithos.2015.05.017openalex-snapshot
Mantle refertilization and magmatism in old orogenic regions: The role of late-orogenic pyroxenites
inferred← citeshttps://doi.org/10.1016/j.lithos.2015.05.021openalex-snapshot
Recycling of oceanic crust from a stagnant slab in the mantle transition zone: Evidence from Cenozoic continental basalts in Zhejiang Province, SE China
inferred← citeshttps://doi.org/10.1016/j.lithos.2016.06.012openalex-snapshot
Petrology and geochemistry of Cenozoic intra-plate basalts in east-central China: Constraints on recycling of an oceanic slab in the source region
inferred← citeshttps://doi.org/10.1016/j.lithos.2016.10.027openalex-snapshot
Cumulate xenoliths from Mt. Overlord, northern Victoria Land, Antarctica: A window into high pressure storage and differentiation of mantle-derived basalts
inferred← citeshttps://doi.org/10.1016/j.lithos.2016.12.024openalex-snapshot
Crust recycling induced compositional-temporal-spatial variations of Cenozoic basalts in the Trans-North China Orogen
inferred← citeshttps://doi.org/10.1016/j.lithos.2017.01.022openalex-snapshot
Petrogenesis of Cenozoic basalts in central-eastern China: Constraints from Re–Os and PGE geochemistry
inferred← citeshttps://doi.org/10.1016/j.lithos.2018.05.025openalex-snapshot
Phase relations and melting of nominally ‘dry’ residual eclogites with variable CaO/Na2O from 3 to 5 GPa and 1250 to 1500 °C; implications for refertilisation of upwelling heterogeneous mantle
inferred← citeshttps://doi.org/10.1016/j.lithos.2018.12.020openalex-snapshot
Formation of Siberian cratonic mantle websterites from high-Mg magmas
inferred← citeshttps://doi.org/10.1016/j.lithos.2019.02.011openalex-snapshot
Testing pyroxenite versus peridotite sources for marine basalts using U-series isotopes
inferred← citeshttps://doi.org/10.1016/j.lithos.2019.105217openalex-snapshot
Pyroxene exsolution microstructures in garnet from the Almklovdalen peridotite, SW Norway
inferred← citeshttps://doi.org/10.1016/j.lithos.2019.105253openalex-snapshot
Influence of the subduction of the Pacific plate on the mantle characteristics of South China: Constraints from the temporal geochemical evolution of the Mesozoic basalts in the Jitai Basin
inferred← citeshttps://doi.org/10.1016/j.lithos.2020.105444openalex-snapshot
Source lithology and crustal assimilation recorded in low δ18O olivine from Okinawa Trough, back-arc basin
inferred← citeshttps://doi.org/10.1016/j.lithos.2020.105855openalex-snapshot
Interplay between melt infiltration and deformation in the deep lithospheric mantle (External Liguride ophiolite, North Italy)
inferred← citeshttps://doi.org/10.1016/j.lithos.2021.106564openalex-snapshot
Slab tear as a cause of coeval arc-intraplate volcanism in the Alexandra Volcanic Group, New Zealand
inferred← citeshttps://doi.org/10.1016/j.lithos.2022.106776openalex-snapshot
Petrological evidence of an anhydrous carbonatitic peridotite source for the Xiaogulihe ultrapotassic volcanic rocks, northeastern China
inferred← citeshttps://doi.org/10.1016/j.lithos.2024.107626openalex-snapshot
Eocene mafic alkaline volcanism in north Central Iran; Signatures of development and subsequent melting of a pyroxenite mantle source
inferred← citeshttps://doi.org/10.1016/j.lithos.2025.107976openalex-snapshot
Melting of amphibole-apatite-rich metasomes in the continental mantle and comparison of melt compositions with natural igneous rocks
inferred← citeshttps://doi.org/10.1016/j.lithos.2025.108036openalex-snapshot
Possible lateral flow in the Big Mantle Wedge of Northeast China revealed by the geochemistry of Cenozoic basalts
inferred← citeshttps://doi.org/10.1016/j.lithos.2025.108378openalex-snapshot
Ambient pyroxenite mantle melting in the origin of Panjal-Qiangtang continental flood basalts: Implications for Early Permian Gondwana rifting and the birth of the Neo-Tethys
inferred← citeshttps://doi.org/10.1016/j.oregeorev.2021.104534openalex-snapshot
Isotopic fingerprints of recycled eclogite facies sediments in the generation of the Huanglongpu carbonatite, central China
inferred← citeshttps://doi.org/10.1016/j.precamres.2013.11.008openalex-snapshot
Genesis of the 1.21 Ga Marnda Moorn large igneous province by plume–lithosphere interaction
inferred← citeshttps://doi.org/10.1016/j.precamres.2017.12.021openalex-snapshot
The petrogenesis of the Neoarchean Kukuluma Intrusive Complex, NW Tanzania
inferred← citeshttps://doi.org/10.1016/j.precamres.2022.106658openalex-snapshot
Geochemical evidence for a widespread Paleoproterozoic continental arc-back-arc magmatism in the Lesser Himalaya during the Columbia supercontinent assembly
inferred← citeshttps://doi.org/10.1016/j.tecto.2009.11.013openalex-snapshot
Structure and evolution of the lithospheric mantle beneath Siberian craton, thermobarometric study
inferred← citeshttps://doi.org/10.1016/j.tecto.2025.230928openalex-snapshot
Does mantle melting due to lithospheric flexural deformation explain the rejuvenated volcanism at the Juan Fernández Ridge?
inferred← citeshttps://doi.org/10.1029/2005gc000927openalex-snapshot
Melting in the Hawaiian plume at 1–2 Ma as recorded at Maui Nui: The role of eclogite, peridotite, and source mixing
inferred← citeshttps://doi.org/10.1029/2005jb003931openalex-snapshot
Origin and geochemical evolution of the Madeira‐Tore Rise (eastern North Atlantic)
inferred← citeshttps://doi.org/10.1029/2006gc001390openalex-snapshot
Temperatures in ambient mantle and plumes: Constraints from basalts, picrites, and komatiites
inferred← citeshttps://doi.org/10.1029/2007gc001583openalex-snapshot
Evidence from high‐Ni olivines for a hybridized peridotite/pyroxenite source for orogenic andesites from the central Mexican Volcanic Belt
inferred← citeshttps://doi.org/10.1029/2008gc001959openalex-snapshot
MORB generation beneath the ultraslow spreading Southwest Indian Ridge (9–25°E): Major element chemistry and the importance of process versus source
inferred← citeshttps://doi.org/10.1029/2008gc002173openalex-snapshot
Petrogenesis of arc lavas from the Rucu Pichincha and Pan de Azucar volcanoes (Ecuadorian arc): Major, trace element, and boron isotope evidences from olivine‐hosted melt inclusions
inferred← citeshttps://doi.org/10.1029/2010gc003233openalex-snapshot
Low‐productivity Hawaiian volcanism between Kaua‘i and O‘ahu
inferred← citeshttps://doi.org/10.1029/2012gc004060openalex-snapshot
Lithosphere versus asthenosphere mantle sources at the Big Pine Volcanic Field, California
inferred← citeshttps://doi.org/10.1029/2018jb016145openalex-snapshot
Using Major Element Logratios to Recognize Compositional Patterns of Basalt: Implications for Source Lithological and Compositional Heterogeneities
inferred← citeshttps://doi.org/10.1029/2019jb017552openalex-snapshot
Ancient Refertilization Process Preserved in the Plagioclase Peridotites: An Example From the Shuanggou Ophiolite, Southwest China
inferred← citeshttps://doi.org/10.1029/2020gc009157openalex-snapshot
Do Olivine Crystallization Temperatures Faithfully Record Mantle Temperature Variability?
inferred← citeshttps://doi.org/10.1029/2020jb020673openalex-snapshot
Partial Melting of the Lower Oceanic Crust: Implications for Tracing the Slab Component in the Source of Mid‐Ocean Ridge Basalts
inferred← citeshttps://doi.org/10.1029/2022gc010657openalex-snapshot
The Meaning of Pressure for Primary Magmas: New Insights From PRIMELT3‐P
inferred← citeshttps://doi.org/10.1029/2023gc011166openalex-snapshot
Origin of Late Cenozoic Basaltic Magmatism in Inner Mongolia, NE China: Constraints From Sr–Nd–Hf–Pb–Mo–He Isotopes
inferred← citeshttps://doi.org/10.1029/2024gc012028openalex-snapshot
Mantle Dynamics of the Long‐Lived Middle Yangtze Basaltic Field: Insight From a Combined Geochemical and Numerical Modeling Approach
inferred← citeshttps://doi.org/10.1029/2025gc012556openalex-snapshot
Evolution of the Source Mineralogy and Lithospheric Controls on Magmatism During the Northeast Atlantic Continental Breakup
inferred← citeshttps://doi.org/10.1029/2026jb034659openalex-snapshot
BaSIC: A Bayesian Inversion Model for Basalt Source Investigation and Characterization
inferred← citeshttps://doi.org/10.1038/nature05254openalex-snapshot
Petrology and thermal structure of the Hawaiian plume from Mauna Kea volcano
inferred← citeshttps://doi.org/10.1038/s41467-025-60619-2openalex-snapshot
Deep evolution of carbonated magmas controls ocean island basalt chemistry
inferred← citeshttps://doi.org/10.1038/s41598-017-10276-3openalex-snapshot
Genesis of ultra-high-Ni olivine in high-Mg andesite lava triggered by seamount subduction
inferred← citeshttps://doi.org/10.1038/s43017-020-0095-1openalex-snapshot
Subduction erosion and arc volcanism
inferred← citeshttps://doi.org/10.1038/srep01856openalex-snapshot
Can we identify source lithology of basalt?
inferred← citeshttps://doi.org/10.1038/srep06099openalex-snapshot
Continuous eclogite melting and variable refertilisation in upwelling heterogeneous mantle
inferred← citeshttps://doi.org/10.1073/pnas.2414632122openalex-snapshot
The return of stagnant slab recorded by intraplate volcanism
inferred← citeshttps://doi.org/10.1080/00206814.2012.663645openalex-snapshot
Review of melting experiments on carbonated eclogite and peridotite: insights into mantle metasomatism
inferred← citeshttps://doi.org/10.1080/00206814.2019.1630859openalex-snapshot
Appinite suites and their genetic relationship with coeval voluminous granitoid batholiths
inferred← citeshttps://doi.org/10.1080/00206814.2019.1686660openalex-snapshot
Geochemical constraints on the origin of late Cenozoic basalts in the Mt. Changbai volcanic field, NE China: evidence for crustal recycling
inferred← citeshttps://doi.org/10.1080/00206814.2020.1756002openalex-snapshot
Alkalic to tholeiitic magmatism near a mid-ocean ridge: petrogenesis of the KR1 Seamount Trail adjacent to the Australian-Antarctic Ridge
inferred← citeshttps://doi.org/10.1080/00206814.2024.2335516openalex-snapshot
Heterogeneity of the late Mesozoic lithospheric mantle beneath the Jiaodong Peninsula, eastern North China Craton: a synthesis from geochemistry and Sr-Nd-Pb isotopes of mafic dykes
inferred← citeshttps://doi.org/10.1093/petrology/egac082openalex-snapshot
Recycled Crustal Components of the Iceland Plume Centre: Ultra-Dehydrated Crust and Oxidised Water-Bearing Fertile Mantle
inferred← citeshttps://doi.org/10.1093/petrology/egac092openalex-snapshot
Mixing Loops, Mixing Envelopes, and Scattered Correlations among Trace Elements and Isotope Ratios Produced by Mixing of Melts Derived from a Spatially and Lithologically Heterogenous Mantle
inferred← citeshttps://doi.org/10.1093/petrology/egad011openalex-snapshot
Multiple Episodes of Rock-Melt Reaction at the Slab-Mantle Interface: Formation of High Silica Primary Magmas in Intermediate to Hot Subduction Zones
inferred← citeshttps://doi.org/10.1093/petrology/egae030openalex-snapshot
Experimental Melting of Phlogopite Websterite in the Upper Mantle between 1.5 and 4.5 GPa
inferred← citeshttps://doi.org/10.1093/petrology/egae095openalex-snapshot
Crystals and Melt Inclusions Record Deep Storage of Superhydrous Magma Prior to the Largest Known Eruption of Cerro Machín Volcano, Colombia
showing the first 200 of 280 · page through all 280
Editorial review for independent work. ICSAC — the Institute for Complexity
Science and Advanced Computing — runs a structured editorial panel for researchers
publishing outside journals, and publishes on CiteStamp rails. Submission is free
and goes through ORCID: icsacinstitute.org/submit.