Are the Chinese Altai “terranes” the result of juxtaposition of different crustal levels during Late Devonian and Permian orogenesis?-Reference-Cited by-同舟云学术

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Are the Chinese Altai “terranes” the result of juxtaposition of different crustal levels during Late Devonian and Permian orogenesis?

Published:2019-02 Issue: Volume:66 Page:183-206
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Broussolle Arnaud,Sun Min,Schulmann Karel,Guy Alexandra,Aguilar Carmen,Štípská Pavla,Jiang Yingde,Yu Yang,Xiao Wenjiao

Funder

National Key Research and Development Program of China

NSFC

Chinese Academy of Sciences

RGC, UGC

HKU

Czech Science Foundation

Publisher

Elsevier BV

Subject

Geology

Reference143 articles.

1. A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia;Badarch;Journal of Asian Earth Sciences,2002

2. Geological Map of the Altai Sheet: Scale1:200,000;BGMRX,1978

3. Neoproterozoic to early Paleozoic tectonic evolution of the Zavkhan terrane of Mongolia: implications for continental growth in the Central Asian belt;Bold;Lithosphere,2016

4. Late Paleozoic tectonic history of the Ertix Fault in the Chinese Altai and its implications for the development of the Central Asian Orogenic System;Briggs;Geological Society of America Bulletin,2007

5. Tectonic development of the southern Chinese Altai Range as determined by structural geology, thermobarometry, 40Ar/39Ar thermochronology, and Th/Pb ion-microprobe monazite geochronology;Briggs;Geological Society of America Bulletin,2009

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