Oceanic Island Basalts from the Darbut and Karamay Ophiolitic Mé1ange in West Junggar （NW China）： Product of a Middle Devonian Mantle Plume

The Central Asian Orogenic Belt （CAOB） is an immense accretionary orogen and is an important site of Phanerozoic crustal growth （Fig. la; Sengor et al., 1993; Jahn, 2004; Windley et al., 2007; Xiao et al., 2008;Safonova and Santosh, 2014）.

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Bibliographic Details
Published in地质学报：英文版 Vol. 89; no. 2; pp. 105 - 106
Main Author YANG Gaoxue LI Yongjun TONG Lili YANG Baokai
Format Journal Article
LanguageEnglish
Published 2015
Subjects
中亚造山带
中国
产品
克拉玛依
地壳生长
洋岛玄武岩
蛇绿混杂岩
西准噶尔
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Summary:The Central Asian Orogenic Belt （CAOB） is an immense accretionary orogen and is an important site of Phanerozoic crustal growth （Fig. la; Sengor et al., 1993; Jahn, 2004; Windley et al., 2007; Xiao et al., 2008;Safonova and Santosh, 2014）.
Bibliography:The Central Asian Orogenic Belt （CAOB） is an immense accretionary orogen and is an important site of Phanerozoic crustal growth （Fig. la; Sengor et al., 1993; Jahn, 2004; Windley et al., 2007; Xiao et al., 2008;Safonova and Santosh, 2014）.
11-2001/P
ISSN:1000-9515
1755-6724