老黑山盆地下白垩统穆棱组油页岩与煤含油率控制因素

doi:10.13278/j.cnki.jjuese.20190247

吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 378-391.doi: 10.13278/j.cnki.jjuese.20190247

• 油页岩成矿与资源评价 • 上一篇下一篇

老黑山盆地下白垩统穆棱组油页岩与煤含油率控制因素

宋宇^1,2, 刘招君^2,3, Achim Bechtel⁴, 徐银波⁵, 孟庆涛^2,3, 孙平昌^2,3, 朱凯¹

1. 构造与油气资源教育部重点实验室(中国地质大学(武汉)), 武汉 430074;
2. 吉林省油页岩与共生能源矿产重点实验室, 长春 130061;
3. 吉林大学地球科学学院, 长春 130061;
4. 莱奥本矿业大学应用地球科学与地球物理系, 奥地利莱奥本A-8700;
5. 中国地质调查局油气资源调查中心, 北京 100083

收稿日期:2019-11-23 出版日期:2020-03-26 发布日期:2020-03-31
作者简介:宋宇(1989-),男,副教授,博士,主要从事非常规油气地球化学研究,E-mail:songyu@cug.edu.cn
基金资助:
国家自然科学基金项目（41902139）；吉林省油页岩与共生能源矿产重点实验室开放基金（DBY-ZZ-18-04）

Controlling Factors of Oil Shale and Coal Oil Yield in Lower Cretaceous Muling Formation in Laoheishan Basin

Song Yu^1,2, Liu Zhaojun^2,3, Achim Bechtel⁴, Xu Yinbo⁵, Meng Qingtao^2,3, Sun Pingchang^2,3, Zhu Kai¹

1. Key Laboratory of Tectonics and Petroleum Resources(China University of Geosciences), Ministry of Education, Wuhan 430074, China;
2. Key Laboratory of Oil Shale and Coexistent Energy Minerals of Jilin Province, Changchun 130061, China;
3. College of Earth Sciences, Jilin Universiry, Changchun 130061, China;
4. Department of Applied Geosciences and Geophysics, Montanuniversitaet Leoben, Leoben A-8700, Austria;
5. Oil&Gas Survey Center, China Geological Survey, Beijing 100083, China

Received:2019-11-23 Online:2020-03-26 Published:2020-03-31
Supported by:
Supported by National Natural Science Foundation of China (41902139) and Open Fund of Key Laboratory of Oil Shale and Coexistent Energy Minerals of Jilin Province (DBY-ZZ-18-04)

摘要/Abstract

摘要： 我国陆相盆地内普遍存在油页岩与煤共生的地质现象。本文以老黑山盆地下白垩统穆棱组油页岩与煤为研究对象，基于工业分析（含油率、灰分、挥发分、全硫和发热量）和有机地球化学分析（有机碳、岩石热解、显微组分和生物标志化合物），对油页岩与煤含油率的控制因素开展研究。根据含油率等工业品质特征，将研究区油页岩与煤进一步划分为高含油率油页岩（HOS）、低含油率油页岩（LOS）、高含油率煤（HC）和低含油率煤（LC）4种亚类。其中HC的总有机碳质量分数和生烃潜力最高，其次为LC、HOS和LOS，4种亚类的有机质类型以Ⅱ型干酪根为主，均处于未成熟的热演化阶段。沉积环境与有机质来源是控制油页岩与煤含油率的关键因素，HOS主要形成于陆源有机质供给中等的湖沼环境，而HC主要形成于陆源有机质供给丰富的泥炭沼泽环境。油页岩与煤形成时期的高等植物以松科、柏科/杉科、南洋杉科、罗汉松科和蕨类植物为主，这些植物可以提供充足的树脂和蜡质有机质，从而使油页岩与煤具有相对较高的含油率。

关键词: 老黑山盆地, 下白垩统, 油页岩与煤, 含油率, 有机地球化学

Abstract: The paragenetic oil shale and coal are widely developed in continental basins of China. The authors took the oil shale and coal of the lower Cretaceous Muling Formation in Laoheishan basin as a study object, and studied the controlling factors of oil yield of oil shale and coal, combined with both industrial parameters (oil yield, ash content, volatile matter, total sulfur, and gross calorific value) and organic geochemical analyses (total organic carbon, Rock-Eval, maceral, and biomarker analyses). The oil shale and coal are classified into four types, including high oil yield oil shale (HOS), low oil yield oil shale (LOS), high oil yield coal (HC), and low oil yield coal (LC). The highest TOC and S₁+S₂ values are observed in HC, followed by LC, HOS, and LOS, all types are of type Ⅱ kerogen and in immature stage. The source of organic matter and depositional environment are the key controlling factors of oil yield in oil shale and coal. HC was deposited in mire with abundant input of terrestrial organic matter; in contrast, HOS was formed in limnology environment with moderate input of terrestrial organic matter. The floral assemblage is characterized by the presence of Pinaceae, Cupressaceae/Taxodiaceae, Araucariaceae, Podocarpaceae and ferns during the formation of oil shale and coal. These plants could provide abundant resinous and waxy organic matter, which lead to relatively high oil yield of oil shale and coal.

Key words: Laoheishan basin, Lower Cretaceous, oil shale and coal, oil yield, ornigac geochemistry

中图分类号:

P618.12

宋宇, 刘招君, Achim Bechtel, 徐银波, 孟庆涛, 孙平昌, 朱凯. 老黑山盆地下白垩统穆棱组油页岩与煤含油率控制因素[J]. 吉林大学学报(地球科学版), 2020, 50(2): 378-391.

Song Yu, Liu Zhaojun, Achim Bechtel, Xu Yinbo, Meng Qingtao, Sun Pingchang, Zhu Kai. Controlling Factors of Oil Shale and Coal Oil Yield in Lower Cretaceous Muling Formation in Laoheishan Basin[J]. Journal of Jilin University(Earth Science Edition), 2020, 50(2): 378-391.

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老黑山盆地下白垩统穆棱组油页岩与煤含油率控制因素

Controlling Factors of Oil Shale and Coal Oil Yield in Lower Cretaceous Muling Formation in Laoheishan Basin

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