Was the Enclosed Qaidam Basin in the Tibetan Plateau Accumulative or Erosive during the Late Quatern

来源 :The 12th International Conference on Salt Lake Research(第十二届 | 被引量 : 0次 | 上传用户：lalalan

【摘要】

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【作者】

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LAI Zhongping

【机构】

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Key Laboratory of Salt Lake Resources and Chemistry,Qinghai Institute of Salt Lakes,Chinese Academy

【出处】

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The 12th International Conference on Salt Lake Research(第十二届

【发表日期】

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2014年2期

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A geological feature in the Qaidam Basin known as the "Shell Bar" contains millions of freshwater articulated clam shells buried in-situ.Since the 1980s this feature in the now hyper-arid basin has been interpreted to be lake deposits that provide evidence for a warmer and more humid climate than present during late Marine Isotope Stage 3(MIS 3)(Bowler et al.,1986).

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Was the Enclosed Qaidam Basin in the Tibetan Plateau Accumulative or Erosive during the Late Quatern

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