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On the ?late? formation of paragonite and its breakdown in pelitic rocks of the southern Damara Orogen (Namibia)

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What this work says

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

inferredcites →https://doi.org/10.1007/bf00371590openalex-snapshot
Low-temperature compatibility relations of the assemblage quartz-paragonite and the thermodynamic status of the phase rectorite
inferredcites →https://doi.org/10.1007/bf00373483openalex-snapshot
Coexisting phengite, paragonite and margarite in metasediments of the mittlere Hohe Tauern, Austria
inferredcites →https://doi.org/10.1007/bf00373759openalex-snapshot
The upper stability limit of the assemblage paragonite + quartz and its natural occurrences
inferredcites →https://doi.org/10.1007/bf00373785openalex-snapshot
Phase relations of talc and tremolite in metamorphic calcite-dolomite sediments in the southern portion of the Damara Belt (South West Africa)
inferredcites →https://doi.org/10.1007/bf00387954openalex-snapshot
The stability of staurolite and chloritoid and their significance in metamorphism of pelitic rocks
inferredcites →https://doi.org/10.1007/bf00402355openalex-snapshot
A model system for mineral facies in pelitic schists
inferredcites →https://doi.org/10.1007/bf01104160openalex-snapshot
Untersuchungen an Paragoniten und an natriumhaltigen Muskoviten Mit einer Darauenetischen Bemerkung
inferredcites →https://doi.org/10.1017/s0080456800003148openalex-snapshot
XXV.—The Mineralogy and Metamorphism of the Moine Schists of the Morar and Knoydart Districts of Inverness-shire
inferredcites →https://doi.org/10.1086/627237openalex-snapshot
A Computer Program for Processing Microprobe Data
inferredcites →https://doi.org/10.1093/petrology/13.1.147openalex-snapshot
The Two-Phase Region and Excess Mixing Properties of Paragonite-Muscovite Crystalline Solutions
inferredcites →https://doi.org/10.1093/petrology/6.2.246openalex-snapshot
Phase Equilibria in Three Assemblages of Kyanite-Zone Pelitic Schists, Lincoln Mountain Quadrangle, Central Vermont
inferredcites →https://doi.org/10.1111/j.1365-3091.1970.tb02189.xopenalex-snapshot
THE STEP FROM DIAGENESIS TO METAMORPHISM IN PELITIC ROCKS DURING ALPINE OROGENESIS
inferredcites →https://doi.org/10.1130/0016-7606(1956)67[919:goprpi]2.0.co;2openalex-snapshot
GEOCHEMISTRY OF PELITIC ROCKS. PART III: MAJOR ELEMENTS AND GENERAL GEOCHEMISTRY
inferredcites →https://doi.org/10.2113/gsecongeo.53.5.563openalex-snapshot
Rank of coal and metamorphic grade of rocks of the Narragansett Basin of Rhode Island
inferredcites →https://doi.org/10.2475/ajs.263.6.512openalex-snapshot
A petrogenetic grid for the Fe-Mg silicates of pelitic schists
inferredcites →https://doi.org/10.2475/ajs.267.3.259openalex-snapshot
Experimental determination of kyanite-andalusite and andalusite-sillimanite equilibria; the aluminum silicate triple point
inferredcites →https://doi.org/10.3406/bulmi.1964.5774openalex-snapshot
Étude des réactions d'échange d'ions Na — K dans la série muscovite˗paragonite

What points at this work

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

inferred← citeshttps://doi.org/10.1007/978-1-4757-4215-2_14openalex-snapshot
Metamorphism of Pelites
inferred← citeshttps://doi.org/10.1007/978-3-319-68920-3_12openalex-snapshot
The Evolution of the Damara Orogenic System: A Record of West Gondwana Assembly and Crustal Response
inferred← citeshttps://doi.org/10.1007/978-3-642-69124-9_21openalex-snapshot
Overview of the Geosynclinal, Structural and Metamorphic Development of the Intracontinental Branch of the Damara Orogen
inferred← citeshttps://doi.org/10.1007/978-3-642-69124-9_28openalex-snapshot
Structural Development of the Ugab Structural Domain of the Northern Zone of the Damara Orogen
inferred← citeshttps://doi.org/10.1007/978-3-642-69124-9_30openalex-snapshot
Compositional Variations of Minerals in Metapelites Involved in Low- to Medium Grade Isograd Reactions in the Southern Damara Orogen, Namibia, South West Africa
inferred← citeshttps://doi.org/10.1007/bf00324564openalex-snapshot
Genesis and solvus relations of submicroscopically intergrown paragonite and phengite in a blueschist from northern California
inferred← citeshttps://doi.org/10.1007/bf00371702openalex-snapshot
Loss of metals from pelites during regional metamorphism
inferred← citeshttps://doi.org/10.1007/bf00384711openalex-snapshot
Stable isotope evidence for fluid-present and fluid-absent metamorphism in metapelites from the Damara Orogen, Namibia
inferred← citeshttps://doi.org/10.1007/bf01164523openalex-snapshot
Equilibrium relations of prograde metamorphic mineral assemblages
inferred← citeshttps://doi.org/10.1016/0016-7037(94)90009-4openalex-snapshot
The paragonite-muscovite solvus: I. P-T-X limits derived from the Na-K compositions of natural, quasibinary paragonite-muscovite pairs
inferred← citeshttps://doi.org/10.1016/0301-9268(92)90026-kopenalex-snapshot
Microfabrics indicating granulite-facies metamorphism in the low-pressure central Damara Orogen, Namibia
inferred← citeshttps://doi.org/10.1016/j.clay.2020.105960openalex-snapshot
Characteristics and genesis of phyllosilicate hydrothermal assemblages from Neoproterozoic epithermal Au-Ag mineralization of the Avalon Zone of Newfoundland, Canada
inferred← citeshttps://doi.org/10.1016/j.gr.2017.07.006openalex-snapshot
Metamorphic response and crustal architecture in a classic collisional orogen: The Damara Belt, Namibia
inferred← citeshttps://doi.org/10.1016/j.gr.2022.05.003openalex-snapshot
Episodic intra-continental reactivation during collapse of a collisional orogen: The Damara Belt, Namibia
inferred← citeshttps://doi.org/10.1016/s0899-5362(01)90109-5openalex-snapshot
Spinel-bearing assemblages and P-T-t evolution of the Central Zone of the Damara Orogen, Namibia
inferred← citeshttps://doi.org/10.1046/j.1525-1314.2003.00457.xopenalex-snapshot
Metamorphism of pelites in NKFMASH – a new petrogenetic grid with implications for the preservation of high‐pressure mineral assemblages during exhumation
inferred← citeshttps://doi.org/10.1093/petrology/egi050openalex-snapshot
A Quaternary Solution Model for White Micas Based on Natural Coexisting Phengite–Paragonite Pairs
inferred← citeshttps://doi.org/10.1111/j.1525-1314.1994.tb00059.xopenalex-snapshot
The effects of ferromagnesian components on the paragonite‐muscovite solvus: a semiquantitative analysis based on chemical data for natural paragonite‐muscovite pairs
inferred← citeshttps://doi.org/10.1144/gsjgs.140.4.0601openalex-snapshot
Petrogenesis of Dalradian albite porphyroblast schists
inferred← citeshttps://doi.org/10.1180/minmag.2007.071.3.285openalex-snapshot
True and brittle micas: composition and solid-solution series
inferred← citeshttps://doi.org/10.2747/0020-6814.49.4.301openalex-snapshot
Paragonite: Why Is It So Rare in Medium-Temperature High-Pressure Rocks?
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