%0 Journal Article
%T Provenance of Early Triassic Hongshuichuan Formation in the southern margin of the East Kunlun Mountains: Constrains from detrital framework, heavy mineral analysis and geochemistry<br>东昆仑南缘早三叠世洪水川组的源区特征:来自碎屑组成、重矿物和岩石地球化学的证据
%A Oleg A Korchagin
%A YAN Zhen
%A BIAN QianTao
%A Oleg A Korchagin
%A LI JiLiang
%A WANG ZongQi
%A <br>闫臻
%A 边千韬
%A IgorⅠ. Pospelov
%A 李继亮
%A 王宗起
%A IgorⅠ. Pospelov
%J 岩石学报
%D 2008
%I 
%X Early Triassic Hongshuichuan Formation in the southern margin of the East Kunlun Mountains is composed of shallow- marine and nonmarine conglomerate,sandstone,sihstones,shale and oomicrite,which accumulated in a forearc basin.Sandstone detrital modes,heavy mineral assemblages,geochemistry and paleocurrent data indicate that the source of the Hongshuichuan Formation predominately derived from the island-arc northward,and the A'nyemaqen ophiolite complex also provided some detritus for the Hongshuichuan Forma...
%K Early Triassic
%K Hongshuichuan Formation
%K Tectonic setting of source area
%K East Kunlun Mountains<br>早三叠世
%K 洪水川组
%K 源区背景
%K 东昆仑
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=0E31E640452E8F744B3B0207CC8688C4&yid=67289AFF6305E306&vid=B91E8C6D6FE990DB&iid=94C357A881DFC066&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=32