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5. The Late Cretaceous source-to-sink system at the eastern margin of the Tibetan Plateau:Insights from

The Late Cretaceous source-to-sink system at the eastern margin of the Tibetan Plateau:Insights from

来源 :地学前缘:英文版 | 被引量 : 0次 | 上传用户：wq123sd

【摘 要】

：

The surface uplift of the Tibetan Plateau(TP)and its geomorphology evolution has triggered aridification of Asias interior and drainage development at the easte

【作 者】

：

Licheng Wang Lijian Shen Chenglin Liu Ke Chen Lin Ding Chengshan Wang 

【机 构】

：

CASCenterforExcellenceinTibetanPlateauEarthSciences,MNRKeyLaboratoryofMetallogenyandMineralAssessmen

【出 处】

：

地学前缘:英文版

【发表日期】

：

2021年3期

【关键词】

：

Detrital Zircons Drainage Late Cretaceous Source-to-sink Lacustrine Basin Tibeta 

【基金项目】

：

financially supported by the National Natural Science Foundation of China(Grant Nos.41572067,91855104,41802111),the Strategic Priority Research Program of Chinese Academy of Sciences(Grant No.XDA 2017

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The surface uplift of the Tibetan Plateau(TP)and its geomorphology evolution has triggered aridification of Asias interior and drainage development at the eastern margin of the plateau.However,how the pre-Cenozoic early growth histories of the TP impact

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