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藏北龙木错东部三岔口地区下奥陶统与泥盆系的不整合界面

Unconformity between the Lower Ordovician and Devonian in the Sanchakou area in the eastern part of the Lungmu Co, northern Tibet, China.

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【作者】 夏军钟华明童劲松鲁如魁

【Author】 XIA Jun1, ZHONG Hua-ming1, TONG Jin-song1,2, LU Ru-kui1,31. Anhui Institute of Geological Survey, Hefei 230001, Anhui, China;2. China University of Geosciences, Beijing 100083, China;3. Northwest University, Xi′an 710069, Shaanxi, China

【机构】 安徽省地质调查院安徽省地质调查院 安徽合肥230001安徽合肥230001安徽合肥230001中国地质大学北京100083安徽合肥230001西北大学陕西西安710069

【摘要】 在北羌塘三岔口一带采获丰富的腕足类:汉伯矮正形贝及比较种Nanorthiscf.hamburgensis(Walcott)。建立了早奥陶世岩石地层单位——三岔口组,是羌塘地区目前有化石控制的最低层位。中、晚泥盆世拉竹龙组与下伏志留系、奥陶系不整合接触关系的进一步确定,证明了羌北-昌都板块与扬子板块的亲缘性,为羌北-昌都板块属性的确定提供了重要证据。

【Abstract】 Abundant brachiopods (Nanorthis cf. hamburgensis (Walcott)) have been collected from the Sanchakou area, northern Qiangtang, and according to the fossils the authors erect a new Early Ordovician lithostratigraphic unit-Sanchakou Formation, which is the lowest horizon controlled by fossils in the Qiangtang region at present. The further determination of the unconformable contact relationships between the Middle-Late Devonian Lazhulong Formation and its underlying Silurian and Ordovician has prove the affinity between the northern Qiangtang-Qamdo plate and the Yangtze plate. This provides important evidence for the determination of the nature of the Qiangtang-Qamdo plate.

【基金】 中国地质调查局《西藏1∶25万松西幅、温泉幅区域地质调查》项目(200213000007)成果。
  • 【文献出处】 地质通报 ,Geological Bulletin of China , 编辑部邮箱 ,2006年Z1期
  • 【分类号】P534.42;P534.44;P542.34
  • 【被引频次】49
  • 【下载频次】194
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