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准噶尔盆地北三台地区侏罗系头屯河组沉积物源分析
引用本文:商琳,戴俊生,刘旭,卞保力. 准噶尔盆地北三台地区侏罗系头屯河组沉积物源分析[J]. 世界地质, 2011, 30(4): 579-584
作者姓名:商琳  戴俊生  刘旭  卞保力
作者单位:1. 中国石油大学地球资源与信息学院,山东青岛266555; 2. 新疆油田勘探开发研究院,新疆克拉玛依834000
基金项目:国家重大科技专项专题“深煤层地应力预测及高渗富集规律研究”(2011ZX05042-001-001)
摘    要:为明确准噶尔盆地北三台地区头屯河期物源体系,应用砂砾岩含量分析法、重矿物组合分析法,在计算头屯河组剥蚀厚度基础上,恢复头屯河期原始地貌,综合判断研究区的主要物源方向; 认为北三台地区侏罗系头屯河组沉积物有两个物源体系,分别是北部沙奇凸起方向和南部博格达山。北三台凸起在头屯河期为水下低凸起,并不提供物源。

关 键 词:物源分析  古地貌  准噶尔盆地  新疆  侏罗系

Sedimentary source analysis of Jurassic Toutunhe Formation in Beisantai area in Junggar Basin
SHANG Lin , DAI Jun-sheng , LIU Xu , BIAN Bao-li. Sedimentary source analysis of Jurassic Toutunhe Formation in Beisantai area in Junggar Basin[J]. Global Geology, 2011, 30(4): 579-584
Authors:SHANG Lin    DAI Jun-sheng    LIU Xu    BIAN Bao-li
Affiliation:1. College of Geo-resources and Information,China University of Petroleum,Qingdao 266555,Shandong,China; 2. Research Institute of Exploration and Development,CNPC Xinjiang Oilfield Company,Karamay 834000,Xinjiang,China
Abstract:For definition of the source system of Jurassic Toutunhe Formation in Beisantai area of Junggar Ba- sin, the authors calculate the erosion thickness of the Formation, restore the palaeogeomorphology during this For- mation, and judge the source direction in the studied area, using sandstone content and heavy mineral combination analysis methods. The deposits of the Toutunhe Formation have two source systems in Beisantai area, including Shaqi uplift in the north and Bogurda mountain in the south. The Beisantai uplift was underwater low uplift during the Toutunhe Formation, and did not provide source.
Keywords:source analysis  palaeogeomorphology  Junggar Basin  Xinjiang  Jurassic
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