Topographic architecture and drainage reorganization in Southeast China: Zircon U-Pb chronology and Hf isotope evidence from Taiwan
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- 作者：Qing Lana ; b ; Yi Yana ; yanyi@gig.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Chi-Yue Huanga ; c ; M. Santoshd ; Ye-Hua Shana ; Wenhuang Chena ; e ; Mengming Yua ; e ; Kun Qiana ; e
- 关键词：East Tibet ; Provenance ; Topography ; Drainage system ; Zircon geochronology
- 刊名：Gondwana Research
- 出版年：2016
- 出版时间：August 2016
- 年：2016
- 卷：36
- 期：Complete
- 页码：376-389
- 全文大小：2600 K
文摘
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The same sedimentary source for the Paleogene stratigraphy in Western Foothills and Hsuehshan Range.
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The provenance for the Tertiary strata in Taiwan has greatly migrated inland during Late Oligocene and Early Miocene.
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The headwaters of Minjiang River could have reached up to the boundary of the Yangtze and Cathaysia Blocks in Early Miocene
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The evolution of topography and drainage systems in SE China seems to be mainly controlled by the opening of marginal sea