Early Mesozoic Anatexis‐Induced Strain Partitioning and Gneiss Doming in the Yunkai Massif, South China: A Response to Contrasted Dynamics of Paleo‐Pacific and Paleo‐Tethys Subductions?-Reference-Cited by-同舟云学术

Early Mesozoic Anatexis‐Induced Strain Partitioning and Gneiss Doming in the Yunkai Massif, South China: A Response to Contrasted Dynamics of Paleo‐Pacific and Paleo‐Tethys Subductions?

Published:2022-10 Issue:10 Volume:41 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Cochelin Bryan¹^ORCID,Wang Bo¹^ORCID,Liu Jiashuo¹,Lu Shenghua¹^ORCID,Shu Liangshu¹^ORCID,Gumiaux Charles²^ORCID,Chen Yan²,Song Fang¹

Affiliation:

1. State Key Laboratory for Mineral Deposits Research School of Earth Sciences and Engineering, Nanjing University Nanjing China

2. Université d'Orléans CNRS BRGM ISTO Orléans France

Funder

National Natural Science Foundation of China

State Key Laboratory for Mineral Deposits Research

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022TC007457

Reference121 articles.

1. Late Orogenic doming in the eastern Betic Cordilleras: Final exhumation of the Nevado-Filabride complex and its relation to basin genesis

2. Late Precambrian thrust and wrench zones in northern Brittany (France)

3. The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustally-derived granite connection in thickened orogens

4. Melting of the continental crust during orogenesis: the thermal, rheological, and compositional consequences of melt transport from lower to upper continental crustThis article is one of a selection of papers published in this Special Issue on the the theme Lithoprobe—parameters, processes, and the evolution of a continent.

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