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The relationship between websterite and peridotite in the Balmuccia peridotite massif (NW Italy) as revealed by trace element variations in clinopyroxene

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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

inferredcites →https://doi.org/10.1002/sca.4950140306openalex-snapshot

SIMS analyses of rare earth elements in natural minerals and glasses: An investigation of structural matrix effects on ion yields

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Pyroxene thermometry in simple and complex systems

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Crystal chemistry and evolution of the clinopyroxene in a suite of high pressure ultramafic nodules from the Newer Volcanics of Victoria, Australia

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The origin and significance of large, tabular dunite bodies in the Trinity peridotite, northern California

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Isotopic constraints on the origin of ultramafic and mafic dikes in the Balmuccia peridotite (Ivrea Zone)

inferredcites →https://doi.org/10.1007/bf00399712openalex-snapshot

Differentiation of partial melts in the mantle: Evidence from the Balmuccia peridotite, Italy

inferredcites →https://doi.org/10.1007/bf00698314openalex-snapshot

Distribution of trace elements during breakdown of mantle garnet: an example from Zabargad

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Multi-element analysis by isotope dilution-spark source mass spectrometry (ID-SSMS)

inferredcites →https://doi.org/10.1016/0012-821x(78)90125-5openalex-snapshot

An assessment of local and regional isotopic equilibrium in the mantle

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Extreme isotopic variations in the upper mantle: evidence from Ronda

inferredcites →https://doi.org/10.1016/0012-821x(88)90132-xopenalex-snapshot

Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust

inferredcites →https://doi.org/10.1016/0012-821x(89)90130-1openalex-snapshot

Further Sr and Nd isotopic results from peridotites of the Ronda Ultramafic Complex

inferredcites →https://doi.org/10.1016/0012-821x(91)90110-4openalex-snapshot

Partitioning of trace elements between olivine and aqueous fluids at highP-T conditions: implications for the effect of fluid composition on trace-element transport

inferredcites →https://doi.org/10.1016/0016-7037(73)90086-0openalex-snapshot

Experimental studies of the distribution of rare earths as trace elements among silicate minerals and liquids and water

inferredcites →https://doi.org/10.1016/0016-7037(84)90329-6openalex-snapshot

Strontium and samarium diffusion in diopside

inferredcites →https://doi.org/10.1016/0016-7037(88)90198-6openalex-snapshot

World-wide occurrence of HFSE-depleted mantle

inferredcites →https://doi.org/10.1016/0016-7037(92)90195-oopenalex-snapshot

Trace element distribution between clinopyroxene and garnet in gabbroic rocks of the deep crust: An ion microprobe study

inferredcites →https://doi.org/10.1016/b978-0-444-42148-7.50010-1openalex-snapshot

Rare Earth Element Abundances in Upper Mantle Rocks

inferredcites →https://doi.org/10.1029/jb095ib03p02661openalex-snapshot

Melting in the oceanic upper mantle: An ion microprobe study of diopsides in abyssal peridotites

inferredcites →https://doi.org/10.1038/323123a0openalex-snapshot

Implications of a two-component marble-cake mantle

inferredcites →https://doi.org/10.1038/345521a0openalex-snapshot

High-field-strength element depletions in arc basalts due to mantle–magma interaction

inferredcites →https://doi.org/10.1093/petrology/22.1.127openalex-snapshot

Existence of Different Peridotite Types and of a Layered Igneous Complex in the Ivrea Zone of the Western Alps

inferredcites →https://doi.org/10.1093/petrology/25.2.343openalex-snapshot

Rare Earth and 3d Transition Element Geochemistry of Peridotitic Rocks: I. Peridotites from the Western Alps

inferredcites →https://doi.org/10.1093/petrology/30.1.199openalex-snapshot

Evidence for Modal Metasomatism in the Orogenic Spinel Lherzolite Body from Caussou (Northeastern Pyrenees, France)

inferredcites →https://doi.org/10.1093/petrology/31.3.597openalex-snapshot

Mechanisms of Mantle Metasomatism: Geochemical Evidence from the Lherz Orogenic Peridotite

inferredcites →https://doi.org/10.1093/petrology/32.4.671openalex-snapshot

Melting of the Shallow Upper Mantle: A New Perspective

inferredcites →https://doi.org/10.1093/petrology/special_volume.2.155openalex-snapshot

The Balmuccia Orogenic Lherzolite Massif, Italy

inferredcites →https://doi.org/10.1093/petrology/special_volume.2.191openalex-snapshot

Continental to Oceanic Mantle Transition--REE and Sr-Nd Isotopic Geochemistry of the Lanzo Lherzolite Massif

inferredcites →https://doi.org/10.1093/petrology/special_volume.2.255openalex-snapshot

Rare Earth and Trace Element Geochemistry of Clinopyroxenes from the Zabargad Peridotite--Pyroxenite Association

inferredcites →https://doi.org/10.1180/minmag.1994.58a.2.254openalex-snapshot

Crystal-Chemical Variations in Amphiboles Close to a Hornblendite Vein: Implications for Models of Mantle Metasomatism

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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Melt-Induced Modification of Zircon: Implications for Dating the External Gabbro of the Finero Mafic Complex, Ivrea-Verbano Zone

inferred← citeshttps://doi.org/10.1002/2017jb015287openalex-snapshot

Effects of Melt Percolation on Zn Isotope Heterogeneity in the Mantle: Constraints From Peridotite Massifs in Ivrea‐Verbano Zone, Italian Alps

inferred← citeshttps://doi.org/10.1007/978-94-015-8979-6_29openalex-snapshot

Shallow Continental Lithospheric Mantle Heterogeneity — Petrological Constraints

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/s00410-017-1387-4openalex-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/s00410-019-1640-0openalex-snapshot

Origin of pyroxenites in the oceanic mantle and their implications on the reactive percolation of depleted melts

inferred← citeshttps://doi.org/10.1007/s004100050280openalex-snapshot

Subcalcic clinopyroxenites and associated ultramafic xenoliths in alkali basalt near Glen Innes, northeastern New South Wales, Australia

inferred← citeshttps://doi.org/10.1007/s004100050472openalex-snapshot

The Finero phlogopite-peridotite massif: an example of subduction-related metasomatism

inferred← citeshttps://doi.org/10.1007/s00604-007-0850-8openalex-snapshot

SIMS analysis of chlorine in metasomatised upper-mantle rocks

inferred← citeshttps://doi.org/10.1007/s11430-006-0926-zopenalex-snapshot

Element diffusion ability in metasomatic agents and its effect on chemical characteristics of metasomatized peridotites

inferred← citeshttps://doi.org/10.1016/0012-821x(96)00019-2openalex-snapshot

Peridotite clinopyroxene chemistry reflects mantle processes rather than continental versus oceanic settings

inferred← citeshttps://doi.org/10.1016/0016-7037(95)00080-jopenalex-snapshot

Origin of LREE-depleted amphiboles in the subcontinental mantle

inferred← citeshttps://doi.org/10.1016/b0-08-043751-6/02004-1openalex-snapshot

Orogenic, Ophiolitic, and Abyssal Peridotites

inferred← citeshttps://doi.org/10.1016/b0-08-043751-6/02008-9openalex-snapshot

Melt Extraction and Compositional Variability in Mantle Lithosphere

inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.00204-7openalex-snapshot

Orogenic, Ophiolitic, and Abyssal Peridotites

inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.00208-4openalex-snapshot

Melt Extraction and Compositional Variability in Mantle Lithosphere

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2017.12.006openalex-snapshot

Zinc isotope composition of the Earth and its behaviour during planetary accretion

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2018.09.023openalex-snapshot

Molybdenum partitioning behavior and content in the depleted mantle: Insights from Balmuccia and Baldissero mantle tectonites (Ivrea Zone, Italian Alps)

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.2023.121315openalex-snapshot

The peridotite-pyroxenite sequence of Rocca d'Argimonia (Ivrea-Verbano Zone, Italy): Evidence for reactive melt flow and slow cooling in the lowermost continental crust

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.122405openalex-snapshot

Heavy halogen compositions of peridotite massifs in the Ivrea-Verbano Zone and implications for strong modification of mantle rocks

inferred← citeshttps://doi.org/10.1016/j.dib.2025.111362openalex-snapshot

Geochemical data of Al-rich diopside pyroxenites from the Premosello mantle peridotite massif, Ivrea-Verbano Zone, Southern Alps

inferred← citeshttps://doi.org/10.1016/j.earscirev.2023.104318openalex-snapshot

The Ivrea-Verbano tectonic evolution: The role of the crust-mantle interactions in rifting localization

inferred← citeshttps://doi.org/10.1016/j.epsl.2004.09.027openalex-snapshot

Direct assessment of mantle boron and lithium contents and distribution by SIMS analyses of peridotite minerals

inferred← citeshttps://doi.org/10.1016/j.epsl.2011.08.034openalex-snapshot

Chlorine isotope evidence for multicomponent mantle metasomatism in the Ivrea Zone

inferred← citeshttps://doi.org/10.1016/j.epsl.2016.08.036openalex-snapshot

Dating layered websterite formation in the lithospheric mantle

inferred← citeshttps://doi.org/10.1016/j.epsl.2017.07.017openalex-snapshot

Sources and timing of pyroxenite formation in the sub-arc mantle: Case study of the Cabo Ortegal Complex, Spain

inferred← citeshttps://doi.org/10.1016/j.epsl.2017.10.018openalex-snapshot

Chromium isotopic homogeneity between the Moon, the Earth, and enstatite chondrites

inferred← citeshttps://doi.org/10.1016/j.epsl.2018.04.008openalex-snapshot

Constant Cu/Ag in upper mantle and oceanic crust: Implications for the role of cumulates during the formation of continental crust

inferred← citeshttps://doi.org/10.1016/j.gca.2013.01.021openalex-snapshot

Partial re-equilibration of highly siderophile elements and the chalcogens in the mantle: A case study on the Baldissero and Balmuccia peridotite massifs (Ivrea Zone, Italian Alps)

inferred← citeshttps://doi.org/10.1016/j.gca.2015.03.036openalex-snapshot

Fractionation of highly siderophile and chalcogen elements during magma transport in the mantle: Constraints from pyroxenites of the Balmuccia peridotite massif

inferred← citeshttps://doi.org/10.1016/j.gca.2017.05.007openalex-snapshot

Copper isotope fractionation during partial melting and melt percolation in the upper mantle: Evidence from massif peridotites in Ivrea-Verbano Zone, Italian Alps

inferred← citeshttps://doi.org/10.1016/j.gca.2019.01.031openalex-snapshot

Calcium isotope fractionation during magmatic processes in the upper mantle

inferred← citeshttps://doi.org/10.1016/j.gca.2019.07.008openalex-snapshot

Calcium isotopic compositions of oceanic crust at various spreading rates

inferred← citeshttps://doi.org/10.1016/j.gca.2025.02.032openalex-snapshot

Mineral-melt calcium isotope fractionation factors constrained using ab initio molecular dynamics simulations and their implications to calcium isotope effects during partial melting in the upper mantle

inferred← citeshttps://doi.org/10.1016/j.gca.2025.02.035openalex-snapshot

Vanadium isotope fractionation in mantle rocks: Constraints from peridotites and pyroxenites

inferred← citeshttps://doi.org/10.1016/j.gca.2025.03.007openalex-snapshot

Metallogeny of subcontinental lithospheric mantle driven by sulfide-saturated pyroxenite-forming melts: evidence from the Balmuccia peridotite massif

inferred← citeshttps://doi.org/10.1016/j.gca.2025.12.018openalex-snapshot

Underplating of H2O-rich magmas in post-collisional tectonic settings

inferred← citeshttps://doi.org/10.1016/j.gsf.2018.11.001openalex-snapshot

Melt migration and melt-rock reaction in the Alpine-Apennine peridotites: Insights on mantle dynamics in extending lithosphere

inferred← citeshttps://doi.org/10.1016/j.gsf.2025.102049openalex-snapshot

Stable chromium isotope fractionation during melt percolation: Implications for chromium isotopic heterogeneity in the mantle

inferred← citeshttps://doi.org/10.1016/j.jrmge.2024.03.012openalex-snapshot

Fracture network characterisation of the Balmuccia peridotite using drone-based photogrammetry, implications for active-seismic site survey for scientific drilling

inferred← citeshttps://doi.org/10.1016/j.jseaes.2019.104146openalex-snapshot

Sapphirine-bearing pyroxenite xenoliths in Cenozoic alkali basalt from Jabel El Arab (Syria): Insights into the nature and composition of the lithosphere beneath the southern Syrian Rift, northern part of the Arabian Plate

inferred← citeshttps://doi.org/10.1016/j.lithos.2004.04.020openalex-snapshot

Genesis and evolution of the lithospheric mantle beneath the Buffalo Head Terrane, Alberta (Canada)☆

inferred← citeshttps://doi.org/10.1016/j.lithos.2007.05.006openalex-snapshot

Origin and significance of spinel and garnet pyroxenites in the shallow lithospheric mantle: Ultramafic massifs in orogenic belts in Western Europe and NW Africa

inferred← citeshttps://doi.org/10.1016/j.lithos.2008.09.011openalex-snapshot

Mantle peridotites from the Dinaridic ophiolite belt and the Vardar zone western belt, central Balkan: A petrological comparison

inferred← citeshttps://doi.org/10.1016/j.lithos.2010.08.002openalex-snapshot

Age and geochemistry of mantle peridotites and diorite dykes from the Baldissero body: Insights into the Paleozoic–Mesozoic evolution of the Southern Alps

inferred← citeshttps://doi.org/10.1016/j.lithos.2016.06.015openalex-snapshot

Origin and age of zircon-bearing chromitite layers from the Finero phlogopite peridotite (Ivrea–Verbano Zone, Western Alps) and geodynamic consequences

inferred← citeshttps://doi.org/10.1016/s0012-821x(02)01059-2openalex-snapshot

Nb/Ta, Zr/Hf and REE in the depleted mantle: implications for the differentiation history of the crust–mantle system

inferred← citeshttps://doi.org/10.1016/s0012-821x(04)00073-1openalex-snapshot

Refertilization of mantle peridotite in embryonic ocean basins: trace element and Nd isotopic evidence and implications for crust–mantle relationships

inferred← citeshttps://doi.org/10.1016/s0016-7037(96)00280-3openalex-snapshot

The neodymium isotopic compositions and rare earth patterns in highly depleted ultramafic rocks

inferred← citeshttps://doi.org/10.1016/s0024-4937(00)00016-5openalex-snapshot

Magmatic modification and metasomatism of the subcontinental mantle beneath the Vitim volcanic field (East Siberia): evidence from trace element data on pyroxenite and peridotite xenoliths from Miocene picrobasalt

inferred← citeshttps://doi.org/10.1016/s0024-4937(99)00033-xopenalex-snapshot

Growth of subcontinental lithosphere: evidence from repeated dike injections in the Balmuccia lherzolite massif, Italian Alps

inferred← citeshttps://doi.org/10.1016/s0264-3707(99)00031-9openalex-snapshot

New Sm–Nd ages for the Ivrea–Verbano Zone, Sesia and Sessera valleys (Northern-Italy)

inferred← citeshttps://doi.org/10.1016/s0419-0254(99)80016-0openalex-snapshot

Growth of subcontinental lithosphere: evidence from repeated dike injections in the balmuccia lherzolite massif, Italian Alps

inferred← citeshttps://doi.org/10.1029/2019jb017385openalex-snapshot

The Ductile‐to‐Brittle Transition Recorded in the Balmuccia Peridotite Body, Italy: Ambient Temperature for the Onset of Seismic Rupture in Mantle Rocks

inferred← citeshttps://doi.org/10.1029/2019jb017990openalex-snapshot

Copper Isotope Variations During Magmatic Migration in the Mantle: Insights From Mantle Pyroxenites in Balmuccia Peridotite Massif

inferred← citeshttps://doi.org/10.1029/2020gc009397openalex-snapshot

Joint Geophysical‐Petrological Modeling on the Ivrea Geophysical Body Beneath Valsesia, Italy: Constraints on the Continental Lower Crust

inferred← citeshttps://doi.org/10.1029/2021jb022584openalex-snapshot

Reaction‐Induced Mantle Weakening at High‐Pressure Conditions: An Example From Garnet Pyroxenites of Ulten Zone (Eastern Alps, N Italy)

inferred← citeshttps://doi.org/10.1038/s41598-024-61763-3openalex-snapshot

Accretion of “young” Phanerozoic subcontinental lithospheric mantle triggered by back-arc extension—the case of the Ivrea-Verbano Zone

inferred← citeshttps://doi.org/10.1093/gji/ggaa263openalex-snapshot

New gravity data and 3-D density model constraints on the Ivrea Geophysical Body (Western Alps)

inferred← citeshttps://doi.org/10.1093/petrology/42.1.233openalex-snapshot

Formation and Modification of the Shallow Sub-continental Lithospheric Mantle: a Review of Geochemical Evidence from Ultramafic Xenolith Suites and Tectonically Emplaced Ultramafic Massifs of Western and Central Europe

inferred← citeshttps://doi.org/10.1093/petrology/egae094openalex-snapshot

Composite Melt–Rock Interactions in the Lowermost Continental Crust: Insights from a Dunite–Pyroxenite–Gabbronorite Association of the Mafic Complex from the Ivrea–Verbano Zone (Italian Alps)

inferred← citeshttps://doi.org/10.1093/petrology/egag061openalex-snapshot

Melt Infiltration and Olivine Accumulation in Upwelling Mantle Recorded in Interlayered Spinel Peridotite, Plagioclase Lherzolite, and Mafic Rocks in the Horoman Peridotite Complex, Japan

inferred← citeshttps://doi.org/10.1093/petrology/egl019openalex-snapshot

Supra-subduction Zone Pyroxenites from San Jorge and Santa Isabel (Solomon Islands)

inferred← citeshttps://doi.org/10.1093/petrology/egn053openalex-snapshot

Formation of Highly Refractory Dunite by Focused Percolation of Pyroxenite-Derived Melt in the Balmuccia Peridotite Massif (Italy)

inferred← citeshttps://doi.org/10.1093/petrology/egt046openalex-snapshot

SHRIMP U–Pb Zircon Triassic Intrusion Age of the Finero Mafic Complex (Ivrea–Verbano Zone, Western Alps) and its Geodynamic Implications

inferred← citeshttps://doi.org/10.1093/petrology/egv074openalex-snapshot

Pyroxenite Layers in the Northern Apennines’ Upper Mantle (Italy)—Generation by Pyroxenite Melting and Melt Infiltration

inferred← citeshttps://doi.org/10.1130/g34438.1openalex-snapshot

Meter-scale Nd isotopic heterogeneity in pyroxenite-bearing Ligurian peridotites encompasses global-scale upper mantle variability

inferred← citeshttps://doi.org/10.1144/gsl.sp.2003.218.01.29openalex-snapshot

Mineral chemistry of ultramafic massifs in the Southern Uralides orogenic belt (Russia) and the petrogenesis of the Lower Palaeozoic ophiolites of the Uralian Ocean

inferred← citeshttps://doi.org/10.1201/b10092-9openalex-snapshot

Rare earth elements in hypabyssal and subvolcanic rocks with high in magnesium composition

inferred← citeshttps://doi.org/10.1201/b11831-13openalex-snapshot

Geochemical relationship between REE and PGE in mafic and ultramafic rocks and their petrogenetic significance

inferred← citeshttps://doi.org/10.17169/refubium-7356openalex-snapshot

Melt-Rock interaction and refertilization of oceanic lithosphere – a highly siderophile element and Os isotope study, Totalp Massif, Switzerland

inferred← citeshttps://doi.org/10.2138/am-2018-6423openalex-snapshot

The distribution of lead and thallium in mantle rocks: Insights from the Balmuccia peridotite massif (Italian Alps)

inferred← citeshttps://doi.org/10.2138/rmg.2016.81.7openalex-snapshot

Re–Pt–Os Isotopic and Highly Siderophile Element Behavior in Oceanic and Continental Mantle Tectonites

inferred← citeshttps://doi.org/10.2139/ssrn.6597973openalex-snapshot

Dual tectonomagmatic origin of the Ivrea-Verbano Zone: Ediacaran–Cambrian arc roots and Late Paleozoic extension

inferred← citeshttps://doi.org/10.2973/odp.proc.sr.153.022.1997openalex-snapshot

Petrology and geochemistry of nodular websterite inclusions in harzburgite, Hole 920D

inferred← citeshttps://doi.org/10.5194/ejm-32-587-2020openalex-snapshot

Contaminating melt flow in magmatic peridotites from the lower continental crust (Rocca d'Argimonia sequence, Ivrea–Verbano Zone)

inferred← citeshttps://doi.org/10.5194/ejm-34-109-2022openalex-snapshot

Melt–rock interactions in a veined mantle: pyroxenite–peridotite reaction experiments at 2 GPa

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