气候变化领域集成服务门户(CCPortal): No sedimentary records indicating southerly flow of the paleo-Upper Yangtze River from the First Bend in southeastern Tibet

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DOI	10.1016/j.gr.2015.02.006
	No sedimentary records indicating southerly flow of the paleo-Upper Yangtze River from the First Bend in southeastern Tibet
	Wei, Hong-Hong; Wang, Erchie; Wu, Guo-Li; Meng, Kai
通讯作者	Wei, HH (通讯作者)
发表日期	2016
ISSN	1342-937X
EISSN	1878-0571
起始页码	93
结束页码	104
卷号	32
英文摘要	It is a long-debated issue whether the Upper Yangtze River once flowed southward from its First Bend as a major tributary of the Red River. The Yangbi valley was assumed as a trough carved by the paleo-Upper Yangtze River. This argument, however, has not been substantiated because of the uncertainty of what is beneath the Quaternary sediments of the valley. We conducted a drilling project in an attempt of resolving this outstanding puzzle. We also studied the Upper Eocene-Lower Oligocene Baoxiangsi and Jinsichang Formations distributed widely to the west of the Yangbi valley because sandstone of the Baoxiangsi Formation were previously regarded as remnants of the south-flowing paleo-Upper Yangtze River. Two drilled holes reveal that the Yangbi valley is entirely filled with Quaternary alluvial-fan and bog deposits and contains no typical fluvial sandstone. The base of the valley is the well-consolidated breccia of the Baoxiangsi Formation. The sedimentary analysis shows that the Baoxiangsi and Jinsichang successions are composed mostly of alluvial-fan, lacustrine, fan-delta and braided-stream facies, and interpreted to have formed in an intermontane rift basin. Facies analysis in conjunction with paleocurrent restoration further shows that the bulk of the Baoxiangsi and Jinsichang sediments were shed from local highlands and debouched to the basin mainly from the south and west Collectively, our sedimentary investigations of both boreholes and outcrops lend no support of the long-held view that the paleo-Upper Yangtze River flowed to the south through the region south of the First Bend. It, however, remains an unresolved problem how the ancestral Upper Yangtze River evolved during the Tertiary. (C) 2015 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
关键词	RED-RIVER SHEAR ZONE AILAO SHAN SOUTHWESTERN SICHUAN EASTERN TIBET CHINA YUNNAN DEFORMATION EVOLUTION VIETNAM
英文关键词	Upper Yangtze River; The First Bend; Drillings; Tertiary; Southeastern Tibet
语种	英语
WOS研究方向	Geology
WOS类目	Geosciences, Multidisciplinary
WOS记录号	WOS:000374425100007
来源期刊	GONDWANA RESEARCH
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/258635
推荐引用方式 GB/T 7714	Wei, Hong-Hong,Wang, Erchie,Wu, Guo-Li,et al. No sedimentary records indicating southerly flow of the paleo-Upper Yangtze River from the First Bend in southeastern Tibet[J]. 中国科学院青藏高原研究所,2016,32.
APA	Wei, Hong-Hong,Wang, Erchie,Wu, Guo-Li,&Meng, Kai.(2016).No sedimentary records indicating southerly flow of the paleo-Upper Yangtze River from the First Bend in southeastern Tibet.GONDWANA RESEARCH,32.
MLA	Wei, Hong-Hong,et al."No sedimentary records indicating southerly flow of the paleo-Upper Yangtze River from the First Bend in southeastern Tibet".GONDWANA RESEARCH 32(2016).