Newly Discovered Jurassic and Cretaceous Strata in the Yidun Area, SW China and their Constraints on the Mesozoic Tectonic Evolution of the Eastern Tethys

The Yushu-Yidun arc magmatic belt has attracted much attention among geologists due to its complete record of the evolutionary process of the Sanjiang tectonic belt in eastern Tethys and its favorable metallogenic conditions. This belt is composed of the sedimentary rock series, and Late Triassic vo...

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Published inActa geologica Sinica (Beijing) Vol. 89; no. 3; pp. 1045 - 1046
Main Authors Awei, MABI, ZARI, Muhetaer, Mingchun, ZHANG, Dengkui, WEN
Format Journal Article
LanguageEnglish
Published Richmond Blackwell Publishing Ltd 01.06.2015
Wiley Subscription Services, Inc
School of Geology and Mining Engineering, Xinjiang University, Urumqi 830002, Xinjiang, China%Institute of Geological Survey of Sichuan Province, Chengdu 610000, Sichuan, China
EditionEnglish ed.
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Summary:The Yushu-Yidun arc magmatic belt has attracted much attention among geologists due to its complete record of the evolutionary process of the Sanjiang tectonic belt in eastern Tethys and its favorable metallogenic conditions. This belt is composed of the sedimentary rock series, and Late Triassic volcanic- the Indosinian and Yanshanian granite intrusions. It has long been believed that there are no Jurassic or Cretaceous strata in this area.
Bibliography:11-2001/P
The Yushu-Yidun arc magmatic belt has attracted much attention among geologists due to its complete record of the evolutionary process of the Sanjiang tectonic belt in eastern Tethys and its favorable metallogenic conditions. This belt is composed of the sedimentary rock series, and Late Triassic volcanic- the Indosinian and Yanshanian granite intrusions. It has long been believed that there are no Jurassic or Cretaceous strata in this area.
ark:/67375/WNG-QQJVZS97-Q
istex:0B8CFB58B77474E0730C3304B3C2F4EBF472505C
ArticleID:ACGS12500
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.12500