High‐Pressure Fluid‐Rock Interaction and Mass Transfer During Exhumation of Deeply Subducted Rocks: Insights From an Eclogite‐Vein System in the Ultrahigh‐Pressure Terrane of the Dabie Shan, China-Reference-Cited by-同舟云学术

High‐Pressure Fluid‐Rock Interaction and Mass Transfer During Exhumation of Deeply Subducted Rocks: Insights From an Eclogite‐Vein System in the Ultrahigh‐Pressure Terrane of the Dabie Shan, China

Published:2019-12 Issue:12 Volume:20 Page:5786-5817
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Liu Penglei¹²^ORCID,Massonne Hans‐Joachim¹²,Harlov Daniel E.³⁴⁵,Jin Zhenmin¹^ORCID

Affiliation:

1. School of Earth SciencesChina University of Geosciences Wuhan China

2. Institut für Mineralogie und KristallchemieUniversität Stuttgart Stuttgart Germany

3. Faculty of Earth ResourcesChina University of Geosciences Wuhan China

4. Deutsches GeoForschungsZentrum Potsdam Germany

5. Department of GeologyUniversity of Johannesburg Auckland Park South Africa

Funder

National Basic Research Program of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008521

Reference165 articles.

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5. Fluorapatite solubility in H2O and H2O–NaCl at 700 to 900 °C and 0.7 to 2.0 GPa

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