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| 草湖地区侏罗系层序地层及沉积体系特征 | |
| 引用本文： | 陆金波,王英民,张雷,王改云,顾秀梅.草湖地区侏罗系层序地层及沉积体系特征[J].沉积与特提斯地质,2011,31(1):1-5. |
| 作者姓名： | 陆金波 王英民 张雷 王改云 顾秀梅 |
| 作者单位： | 1. 中国石油大学,资源与信息学院,北京,102249;中国石油大学,油气资源与探测国家重点实验室,北京,102249 2. 中石油煤层气有限责任公司,北京,100028 3. 大港油田电力公司港中变电分公司,天津,300280 |
| 基金项目： | 国家十一五重大科技专项 |
| 摘 要： | 基于测录井资料对比,结合区域构造演化特征,将草湖凹陷侏罗系划分为两个三级层序J-SQ1与J-SQ2。J-SQ1时期气候温暖潮湿,层序发育完整的上升半旋回和下降半旋回沉积,发育辫状河体系和湖泊体系;J-SQ2时期气候逐渐转为炎热半干旱,层序发育不完整,只发育上升半旋回沉积,主要由氧化型湖泊体系构成,发育滨浅湖砂滩、泥滩互层沉积。其中,J-SQ1早期辫状河河道砂体叠置厚度大,储层物性好,上覆中厚层湖相泥岩沉积,是本区有利的储集层段。 |
| 关 键 词： | 草湖凹陷 侏罗系 沉积体系 层序地层 |
| 收稿时间： | 2010/5/28 0:00:00 |
| 修稿时间： | 2010/8/30 0:00:00 |
Sequence stratigraphy and depositional systems in the Caohu depression, Tarim Basin, Xinjiang |
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| LU Jin-bo,WANG Ying-min,ZHANG Lei,WANG Gai-yun,GU Xiu-mei.Sequence stratigraphy and depositional systems in the Caohu depression, Tarim Basin, Xinjiang[J].Sedimentary Geology and Tethyan Geology,2011,31(1):1-5. | |
| Authors: | LU Jin-bo WANG Ying-min ZHANG Lei WANG Gai-yun GU Xiu-mei |
| Institution: | LU Jin-bo1,2,WANG Ying-min1,ZHANG Lei3,WANG Gai-yun1,GU Xiu-mei4 (1.School of Resources and Information Technology,China University of Petroleum,Beijing 102249,China,2.State Key Laboratory of Petroleum Resources and Exploration,3.PetroChina Coalbed Methane Co.ltd.,Beijing 100028,4.Dagang Oil Field Power Company,Tianjin 300280,China) |
| Abstract: | The Jurassic strata in the Caohu depression,Tarim Basin,Xinjiang are divided,on the basis of well logs and regional tectonic evolution,into two third-order sequences J-SQ1 and J-SQ2.During the deposition of J-SQ1 sequences,the climates were warm and humid.The sequence displays the complete rising-falling semicyclic deposits.Till the deposition of J-SQ2 sequences,the climates turned into hot and semiarid ones.The sequences display only the rising semicyclic deposits,and consists of oxidized lacustrine deposi... |
| Keywords: | Caohu depression Jurassic depositional system sequence stratigraphy |
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