| 上扬子地区下寒武统海相富有机质页岩形成环境与主控因素分析 |
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| 引用本文： | 久凯,丁文龙,黄文辉,张金川,曾维特.上扬子地区下寒武统海相富有机质页岩形成环境与主控因素分析[J].现代地质,2012,26(3):547-554. |
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| 作者姓名： | 久凯 丁文龙 黄文辉 张金川 曾维特 |
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| 作者单位： | 1. 中国地质大学能源学院,北京100083;中国地质大学海相储层演化与油气富集机理教育部重点实验室,北京100083
2. 中国地质大学能源学院,北京,100083 |
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| 基金项目： | 国家自然科学基金，国家科技重大专项项目，全国油气资源战略选区调查与评价国家专项项目 |
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| 摘 要： | 对上扬子地区下寒武统富有机质页岩发育主控因素的研究是进行该区页岩气勘探有利区预测的基础问题之一。通过对上扬子地区下寒武统黑色页岩典型露头剖面样品特征的分析,运用岩石、矿物、有机质特点、特征元素等指标对该区海相富有机质页岩在早寒武世时的古环境进行恢复,建立上扬子地区下寒武统海相富有机质页岩沉积环境判别综合表,认为该套黑色页岩在早寒武世是典型的缺氧环境。上扬子地区下寒武统富有机质页岩的发育是古构造、古气候和古海平面变化、古洋流及海底热液活动等因素综合作用的结果。建立了上扬子地区古海平面上升―上升洋流―热液活动―水体分层―缺氧环境的页岩发育模式,指出海底热液活动和上升洋流促进生物体的勃发,为富有机质页岩形成提供物质基础;海平面上升和上升洋流不仅造成水体分层,而且共同影响富有机质页岩的分布范围。
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| 关 键 词： | 上扬子地区 富有机质页岩 古环境恢复 主控因素 发育模式 |
Formation Environment and Controlling Factors of Organic-rich Shale of Lower Cambrian in Upper Yangtze Region |
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| JIU Kai
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DING Wen-long
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HUANG Wen-hui
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ZHANG Jin-chuan
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ZENG Wei-te.Formation Environment and Controlling Factors of Organic-rich Shale of Lower Cambrian in Upper Yangtze Region[J].Geoscience——Journal of Graduate School,China University of Geosciences,2012,26(3):547-554. |
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| Authors: | JIU Kai DING Wen-long HUANG Wen-hui ZHANG Jin-chuan ZENG Wei-te |
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| Institution: | 1(1.School of Energy Resources,China University of Geosciences,Beijing 100083,China;2.Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism,Ministry of Education,China University of Geosciences,Beijing 100083,China) |
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| Abstract: | The research of controlling factors on organic-rich shale of Lower Cambrian in Upper Yangtze region is one of the basic questions for forecasting favorable shale gas exploration area.Through analyzing samples of typical organic-rich black shale outcrop profile in Upper Yangtze region,the Early Cambrian paleo-environment of marine organic-rich in Upper Yangtze region is restored and the depositional environment comprehensive distinguished table is established using information from rocks,minerals,organic matter charactersics,feature elements.In Early Cambrian,the black shale is formed in a typical hypoxia.The Lower Cambrian black shale of Upper Yangtze region is a combined result of paleostructure,paleoclimate,sea level changes,paleoocean currents and hydrothermal activity,and so on.The shale development model of sea level-ascending current-hydrothermal activity-stratified water bodies-hypoxia is built.Hydrothermal activity and ascending current promote the organisms to thrive and provide the material basis for the formation of organic-rich shale.Rising sea level and ascending current not only lead to stratified water bodies,but also affect the distribution range of organic-rich shale. |
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| Keywords: | Upper Yangtze region organic-rich shale paleoenvironment reconstruction controlling factor development model |
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