Paleocave as a Proxy for Calculating Uplift Amplitude of the Late Ordovician in Central Tarim, Xinjiang, Northwest China
- 责任者：Shen Yinmin (School of Earth and Space Sciences ; Peking University ; Beijing 100871 ; China) ; Li Yue
- 刊名：Chinese Journal of Geology
- 出版年：2010
- 卷期：45(2)
- 关键词：隆起 ; uplifts ; 古岩溶 ; paleokarst ; 晚奥陶世 ; Upper Ordovician ; 塔里木盆地 ; Tarim Basin
- 页码：p.349-360
- 图表：5 illus., 2 tables, 34 refs.
- 分类号：1200
- issnNo：ISSN0563-5020
- isbnNo：CN11-1937/P
Unconformably contact between the sandstone-siltstone of the Sangtamu Formation and limestone of the Lianglitag Formation in Ordovician, Kaitian, exists in the Tazhong High, central Tarim Platform.spacerun: yes"> It distinctively indicates a regional tectonic uplift event happened with duration of about 1 Ma.spacerun: yes"> A suite of coalesced, collapsed-paleocave sediment occurred from the 4 125.6～4 133.space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />