| 盆地内大面积砂体分布的一种成因机理--干旱气候下季节性河流沉积 |
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| 引用本文： | 高志勇,周川闽,冯佳睿,崔京钢,郭美丽,吴昊.盆地内大面积砂体分布的一种成因机理--干旱气候下季节性河流沉积[J].沉积学报,2015,33(3):427-438. |
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| 作者姓名： | 高志勇 周川闽 冯佳睿 崔京钢 郭美丽 吴昊 |
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| 作者单位： | 1.中国石油勘探开发研究院实验研究中心 北京 100083; |
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| 基金项目： | 国家科技重大专项课题，中国石油股份公司科技项目 |
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| 摘 要： | 我国西部新疆地区侏罗系-下白垩统大面积、厚层状砂岩油气勘探获得了重大发现, 大面积厚层状砂体及泥岩红层沉积的成因机理受到长期关注。结合现今准噶尔南缘多条季节性河流的沉积体系、砂体展布特征分析, 并对比郝家沟-头屯河剖面、玛纳斯河剖面上侏罗统齐古组、喀拉扎组的岩相组合、岩石颜色、砂泥岩沉积构造、沉积序列与古环境分析, 认为干旱气候下头屯河组上部-喀拉扎组的季节性曲流河-季节性辫状河沉积是上侏罗统大面积厚层状砂砾岩体及厚层状泥岩红层沉积的重要成因机理, 进而建立了季节性河流的砂体构型和成因模式。准噶尔盆地南缘季节性河流沉积砂体构型和成因模式的建立, 对进一步认识我国古代季节性河流沉积提供了有益参考。
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| 关 键 词： | 大面积砂体 干旱气候 季节性河流 砂体构型 准噶尔南缘 中上侏罗统 |
| 收稿时间： | 2014-06-18 |
Distribution of a Large Area of Sand Body Formation Mechanism:Ephemeral Streams in Arid Climate |
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| GAO ZhiYong
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ZHOU ChuanMin
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FENG JiaRui
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CUI JingGang
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GUO MeiLi
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WU Hao.Distribution of a Large Area of Sand Body Formation Mechanism:Ephemeral Streams in Arid Climate[J].Acta Sedimentologica Sinica,2015,33(3):427-438. |
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| Authors: | GAO ZhiYong ZHOU ChuanMin FENG JiaRui CUI JingGang GUO MeiLi WU Hao |
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| Institution: | 1.Petroleum Geology Research and Laboratory Center RIPED, Beijing 100083;2.State Key Laboratory of Enhanced Oil Recovery (Research Institute of Petroleum Exploration and Development), Beijing 100083;3.China University of Geosciences, Beijing 100083 |
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| Abstract: | A major breakthrough of thick bedded sandstone oil and gas exploration is in China's western Xinjiang region of Jurassic and Cretaceous. Large areas of thick layer of sand body and red mudstone layer deposition formation mechanism have been a research focus by attention for a long time. Combined with much more information including southern margin of Junggar Basin sedimentary system of seasonal rivers, sand body distribution characteristics of analysis, and analysis of the lithofacies assemblages and rock color, sedimentary structure and formation mechanism of sandstone and mudstone of the Haojiagou-Toutun River section and Manasi River section of Toutun River formation of Middle Jurassic in upper part of Middle Jurassic Qigu and Kalazha Formation in the southern margin of the Junggar Basin, We think arid climate background ephemeral streams are the main sediment types of the period. An ephemeral streams sand body configuration and the genetic model have been established, and further understanding of ancient ephemeral streams sedimentary will provide the beneficial reference in China. |
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| Keywords: | large area of sand body arid climate ephemeral streams sand body configuration the southern margin of the Junggar Basin Middle and Upper Jurassic |
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