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塔里木盆地库鲁克塔格地区新元古代冰碛岩锆石SHRIMP U—Pb年龄新证据
引用本文:高林志,王宗起,许志琴,杨经绥,张维. 塔里木盆地库鲁克塔格地区新元古代冰碛岩锆石SHRIMP U—Pb年龄新证据[J]. 中国区域地质, 2010, 0(2): 205-213
作者姓名:高林志  王宗起  许志琴  杨经绥  张维
作者单位:[1]中国地质科学院地质研究所,北京100037 [2]国土资源部北京离子探针中心,北京100037
基金项目:中国石化勘探项目《塔里木盆地及周边南华-白垩纪古环境图编制》和中国地质调查局项目(编号:1212010811033)资助
摘    要:塔里木盆地库鲁克塔格地区新元古代冰碛岩剖面是目前世界各大陆中唯一发育有4套新元古代冰碛岩和多期火成岩事件的剖面。近年来。“雪球事件”的提出为全球新元古代冰碛岩的研究注入了新的活力,各国地质学家根据新元古代冰碛岩在全球各大洲发育的特点、同位素年龄扣C/O、Sr同位素在新元古界划分出4个冰期。因此,新疆库鲁克塔格地区新元古界发育的4套冰碛岩的沉积特征、沉积环境和年代地层学研究的进展始终为各国地质学家所注目。本次获得的库鲁克塔格地区特瑞爱肯组的锆石SHKIMPU-Pb新年龄.为完善库鲁克塔格地区新元古代冰碛岩的年代地层学提供了新的证据。

关 键 词:塔里木盆地  库鲁克塔格地区  新元古代  冰碛岩  锆石SHRIMP  U-Pb年龄

A new evidence from zircon SHRIMP U-Pb dating of the Neoproterozoic diamictite in Quruqtagh area, Tarim besin, Xinjiang, China
GAO Lin-zhi,WANG Zong-qi,XU Zhi-qin,YANG Jing-sui,ZHANG Wei. A new evidence from zircon SHRIMP U-Pb dating of the Neoproterozoic diamictite in Quruqtagh area, Tarim besin, Xinjiang, China[J]. Regional Geology of China, 2010, 0(2): 205-213
Authors:GAO Lin-zhi  WANG Zong-qi  XU Zhi-qin  YANG Jing-sui  ZHANG Wei
Affiliation:1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China; 2. Beijing SHRIMP Centre, Ministry of Land and Resources of China, Beijing 100037, China)
Abstract:Neoproterozoic glaciations of Quruqtagh area in Tarim basin are recognized, four of which appear to be global and with different volcanic rocks. In recent years, "Snow earth" hypothesis put forwards to the study of glaciation, any advancement of sedimentary, depositional environment and glaciation chronostratigraphic dating for the four glaciations in Quruqtagh area in Tarim basin, which will put more attention to global. This paper gives a new zircon SHRIMP U-Pb dating to be showing an evidence for the Neoproterozoic glaciations of Quruqtagh area in Tarim basin.
Keywords:Tarim basin  Quruqtagh area  Neoproterozoic  diamictite  zircon SHRIMP U-Pb dating
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