Peritectic Melting of Mica in Fault‐Related Pseudotachylite Melts and Potassium Mass Balance as an Indicator of Fluid‐Absent Source Conditions.-Reference-Cited by-同舟云学术

Peritectic Melting of Mica in Fault‐Related Pseudotachylite Melts and Potassium Mass Balance as an Indicator of Fluid‐Absent Source Conditions.

Published:2021-02 Issue:2 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Dobson David P.¹^ORCID,Montheil Leny²,Paine Joseph J.¹,Thomson Andrew R.¹^ORCID

Affiliation:

1. Department of Earth Sciences University College London London UK

2. Géosciences Montpellier (UMR 5243) Université de Montpellier Montpellier France

Funder

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009217

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4. Fossil earthquakes recorded by pseudotachylytes in mantle peridotite from the Alpine subduction complex of Corsica

5. Petrology of pseudotachylytes from the Alpine Fault of New Zealand

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2. Selective clast survival in an experimentally-produced pseudotachylyte;Journal of Structural Geology;2021-06