松辽盆地青山口乡青山口组细粒沉积岩分类及其成因

doi:10.7657/XJPG20210404

新疆石油地质 ›› 2021, Vol. 42 ›› Issue (4): 418-427.doi: 10.7657/XJPG20210404

松辽盆地青山口乡青山口组细粒沉积岩分类及其成因

丁聪¹(), 孙平昌¹^,²(), 热西提·亚力坤¹, 王畅³, 张瀛¹, 张晴⁴

1.吉林大学地球科学学院,长春 130061
2.吉林省油页岩及共生能源矿产重点实验室,长春 130061
3.北京师范大学珠海分校统计学院,广东珠海 519087
4.吉林大学经济学院,长春 130012

收稿日期:2020-11-09 修回日期:2021-04-24 出版日期:2021-08-01 发布日期:2022-09-27
通讯作者: 孙平昌 E-mail:1140114133@qq.com;sunpc@jlu.edu.cn
作者简介:丁聪（1997-）,男,山东济宁人,硕士研究生,沉积学,（Tel）15764331685（E-mail） 1140114133@qq.com
基金资助:
国家自然科学基金(41772092);国家自然科学基金(41402088);中国地质调查局地质调查项目(CDD2106-2);中国地质调查局地质调查项目(DD20211341)

Classification and Genesis of Fine-Grained Sedimentary Rocks of Qingshankou Formation in Songliao Basin

DING Cong¹(), SUN Pingchang¹^,²(), WANG Chang³, ZHANG Ying¹, ZHANG Qing⁴

1. School of Earth Sciences, Jilin University, Changchun, Jilin 130061, China
2. Jilin Key Laboratory of Oil Shale and Coexisting Minerals, Changchun, Jilin 130061, China
3. School of Statistics, Beijing Normal University, Zhuhai, Guangdong 519087, China
4. School of Economics, Jilin University, Changchun, Jilin 130012, China

Received:2020-11-09 Revised:2021-04-24 Online:2021-08-01 Published:2022-09-27
Contact: SUN Pingchang E-mail:1140114133@qq.com;sunpc@jlu.edu.cn

摘要/Abstract

摘要：

松辽盆地青山口组为厚层细粒沉积岩,是页岩油气成藏的重要层位,细粒沉积岩的分类是开展非常规油气勘探的前提。通过松辽盆地青山口乡剖面实测和系统样品分析,开展了青山口组细粒沉积岩类型、沉积环境和地球化学特征研究。根据总有机碳、碳酸盐矿物和陆源碎屑矿物含量,研究区细粒沉积岩可分为贫有机质陆源碎屑细粒岩、中有机质陆源碎屑细粒岩、富有机质陆源碎屑细粒岩、极贫有机质陆源碎屑细粒岩、贫有机质碳酸盐细粒岩和极贫有机质碳酸盐细粒岩。其中富有机质陆源碎屑细粒岩、中有机质陆源碎屑细粒岩和贫有机质碳酸盐细粒岩沉积于相对静水的半深湖,贫有机质陆源碎屑细粒岩、极贫有机质陆源碎屑细粒岩和极贫有机质碳酸盐细粒岩沉积于浅湖,碳酸盐岩主要沉积于温带—亚热带开放性咸水湖盆。细粒沉积岩有机质类型主要为Ⅱ₁型,为中等—好烃源岩,深埋藏区中—富有机质陆源碎屑细粒岩是进行页岩油气勘探的优质对象。

关键词: 松辽盆地, 青山口乡, 青山口组, 细粒沉积岩, 岩石分类, 沉积环境, 地球化学特征

Abstract:

The Qingshankou formation in the Songliao basin belongs to thick fine-grained sedimentary rock, and it is an important interval for shale oil and gas accumulation. The classification of the fine-grained sedimentary rocks is the key premise for exploring unconventional oil and gas. Based on field survey and systematic sampling analysis, we studied the types, sedimentary environment and geochemical characteristics of the fine-grained sedimentary rock of the Qingshankou formation in the Songliao basin. According to TOC and the contents of carbonate and terrigenous clastic minerals, the fine-grained sedimentary rocks in the study area can be classified into fine-grained terrigenous clastic rocks with extremely poor, poor, moderate and rich organic matters, and fine-grained terrigenous carbonate rocks with poor and extremely poor organic matters. The fine-grained terrigenous clastic rocks with rich and moderate organic matters and the fine-grained terrigenous carbonate rocks with poor organic matter were deposited in a semi-deep lake environment with stiller water; the fine-grained terrigenous clastic rock with poor and extremely poor organic matters and the fine-grained terrigenous carbonate rock with extremely poor organic matters were deposited in a shallow lake environment; and carbonate rock was mainly deposited in an open saline lake basin in temperate to subtropical zones. The primary type of organic matters in the fine-grained sedimentary rocks is Type Ⅱ₁. The fine-grained sedimentary rocks are medium-good quality source rocks. The fine-grained terrigenous clastic rocks with rich and poor organic matters in deep formations are primary targets for shale oil and gas exploration.

Key words: Songliao basin, Qingshankou township, Qingshankou formation, fine-grained sedimentary rock, rock classification, sedimentary environment, geochemical characteristic

中图分类号:

TE122.113

丁聪, 孙平昌, 热西提·亚力坤, 王畅, 张瀛, 张晴. 松辽盆地青山口乡青山口组细粒沉积岩分类及其成因[J]. 新疆石油地质, 2021, 42(4): 418-427.

DING Cong, SUN Pingchang, WANG Chang, ZHANG Ying, ZHANG Qing. Classification and Genesis of Fine-Grained Sedimentary Rocks of Qingshankou Formation in Songliao Basin[J]. Xinjiang Petroleum Geology, 2021, 42(4): 418-427.

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参考文献 43

[1]	郝运轻, 谢忠怀, 周自立, 等. 非常规油气勘探领域泥页岩综合分类命名方案探讨[J]. 油气地质与采收率, 2012, 19(6):16-19.
	HAO Yunqing, XIE Zhonghuai, ZHOU Zili, et al. Discussion on multi-factors indentification of mudstone and shale[J]. Petroleum Geology and Recovery Efficiency, 2012, 19(6):16-19.
[2]	支东明, 宋永, 何文军, 等. 准噶尔盆地中—下二叠统页岩油地质特征、资源潜力及勘探方向[J]. 新疆石油地质, 2019, 40(4):389-401.
	ZHI Dongming, SONG Yong, HE Wenjun, et al. Geological characteristics,resource potential and exploration direction of shale oil in Middle-Lower Permian,Junggar basin[J]. Xinjiang Petroleum Geology, 2019, 40(4):389-401.
[3]	邹才能, 杨智, 崔景伟, 等. 页岩油形成机制、地质特征及发展对策[J]. 石油勘探与开发, 2013, 40(1):14-26.
	ZOU Caineng, YANG Zhi, CUI Jingwei, et al. Formation mechanism,geological characteristics and development strategy of nonmarine shale oil in China[J]. Petroleum Exploration and Development, 2013, 40(1):14-26.
[4]	KRUMBEIN W C. Shales and their environmental significance[J]. Journal of Sedimentary Petrology, 1947, 17(3):101-108.
[5]	TUCKER M E. Sedimentary petrology[M]. New Jersey:Wiley-Blackwell, 2001.
[6]	APLIN A C, MACQUAKER J H S. Mudstone diversity:origin and implications for source,seal,and reservoir properties in petroleum systems[J]. American Association of Petroleum Geologists Bulletin, 2011, 95(12):2 031-2 059. doi: 10.1306/03281110162
[7]	JIANG Zaixing, GUO Ling, LIANG Chao. Lithofacies and sedimentary characteristics of the Silurian Longmaxi shale in southeastern Sichuan basin,China[J]. Journal of Palaeogeography, 2013, 2(3):238-251.
[8]	朱德顺. 陆相湖盆页岩油富集影响因素及综合评价方法:以东营凹陷和沾化凹陷为例[J]. 新疆石油地质, 2019, 40(3):269-275.
	ZHU Deshun. Influencing factor analysis and comprehensive evaluation method of lacustrine shale oil:cases from Dongying and Zhanhua sags[J]. Xinjiang Petroleum Geology, 2019, 40(3):269-275.
[9]	SCHIEBER J, SOUTHARD J B, SCHIMMELMANN A. Lenticular shale fabrics resulting from intermittent erosion of water-rich muds-interpreting the rock record in the light of recent flume experiments[J]. Journal of Sedimentary Research, 2010, 80(1):119-128. doi: 10.2110/jsr.2010.005
[10]	JOE,MACQUAKER. Mud and mudstones：introduction and overview[J]. Clays and Clay Minerals, 2005, 53(5)548-552. doi: 10.1346/000986005774539241
[11]	YANG Wanli. Daqing oil field,People’s Republic of China:a giant field with oil of nonmarine origin[J]. AAPG Bulletin, 1985, 69(7):1 101-1 111.
[12]	WATSON W P, HAYWARD A B, PARKINSON D N, et al. Plate tectonic history,basin development and petroleum source rock deposition on shore China[J]. Marine & Petroleum Geology, 1987, 4(3):205-225.
[13]	FENG Zhiqiang, JIA Chengzao, XIE Xinong, et al. Tectonostratigraphic units and stratigraphic sequences of the nonmarine Songliao basin,Northeast China[J]. Basin Research, 2010, 22(1):79-95. doi: 10.1111/bre.2010.22.issue-1
[14]	闫晶晶. 吉林农安地区青山口组和嫩江组生物地层及古气候变化[D]. 北京:中国地质大学(北京), 2007.
	YAN Jingjing. Mid-Cretaceous biostratigraphy and palaeoclimate change from the Qingshankou and Nenjiang formations in Nong’an area,Jilin province[D]. Beijing:China University of Geosciences (Beijing), 2007.
[15]	刘群, 袁选俊, 林森虎, 等. 鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨[J]. 沉积学报, 2014, 32(6):1 016-1 025.
	LIU Qun, YUAN Xuanjun, LIN Senhu, et al. The classification of lacustrine mudrock and research on its’ depositional environment[J]. Acta Sedimentologica Sinica, 2014, 32(6):1 016-1 025.
[16]	TRABUCHO-ALEXANDRE J, DIRKX R, VELD H, et al. Toarcian black shales in the Dutch Central Graben:record of energetic,variable depositional conditions during an ocean anoxic event[J]. Journal of Sedimentary Research, 2012, 82(2):104-120. doi: 10.2110/jsr.2012.5
[17]	HICKEY J J, HENK B. Lithofacies summary of the Mississippian barnett shale[J]. AAPG Bulletin, 2007, 91(4):437-443. doi: 10.1306/12040606053
[18]	BOWKER K A. Barnett shale gas production,Fort Worth basin:issues and discussion[J]. AAPG Bulletin, 2007, 91(4):523-533. doi: 10.1306/06190606018
[19]	徐希旺, 陈世悦, 王越, 等. 吐哈盆地大河沿地区塔尔朗组细粒沉积岩特征[J]. 沉积学报, 2017, 35(4):705-713.
	XU Xiwang, CHEN Shiyue, WANG Yue, et al. Characteristics of fine-grained sedimentary rocks in Taerlang formation,Daheyan area,Turpan-Hami basin[J]. Acta Sedimentologica Sinica, 2017, 35(4):705-713.
[20]	王冠民. 济阳坳陷古近系页岩的纹层组合及成因分类[J]. 吉林大学学报(地球科学版), 2012, 42(3):666-671.
	WANG Guanmin. Laminae combination and genetic classification of Eogene shale in Jiyang depression[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(3):666-671.
[21]	付金华, 邓秀芹, 楚美娟, 等. 鄂尔多斯盆地延长组深水岩相发育特征及其石油地质意义[J]. 沉积学报, 2013, 31(5):928-938.
	FU Jinhua, DENG Xiuqin, CHU Meijuan, et al. Features of deepwater lithofacies,Yanchang formation in Ordos basin and its petroleum significance[J]. Acta Sedimentologica Sinica, 2013, 31(5):928-938.
[22]	张顺, 陈世悦, 谭明友, 等. 东营凹陷西部沙河街组三段下亚段泥页岩沉积微相[J]. 石油学报, 2014, 35(4):633-645.
	ZHANG Shun, CHEN Shiyue, TAN Mingyou, et al. Characterization of sedimentary microfacies of shale in the lower third sub-menber of Shahejie formation,western Dongying sag[J]. Acta Petrolei Sinica, 2014, 35(4):633-645.
[23]	王岚, 曾雯婷, 夏晓敏, 等. 松辽盆地齐家—古龙凹陷青山口组黑色页岩岩相类型与沉积环境[J]. 天然气地球科学, 2019, 30(8):1 125-1 133.
	WANG Lan, ZENG Wenting, XIA Xiaomin, et al. Study on lithofacies types and sedimentary environment of black shale of Qingshankou formation in Qijia-Gulong depression,Songliao basin[J]. Natural Gas Geoscience, 2019, 30(8):1 125-1 133.
[24]	柳波, 石佳欣, 付晓飞, 等. 陆相泥页岩层系岩相特征与页岩油富集条件:以松辽盆地古龙凹陷白垩系青山口组一段富有机质泥页岩为例[J]. 石油勘探与开发, 2018, 45(5):828-838.
	LIU Bo, SHI Jiaxin, FU Xiaofei, et al. Petrological characteristics and shale oil enrichment of lacustrine fine-grained sedimentary system:a case study of organic-rich shale in first member of Cretaceous Qingshankou formation in Gulong sag,Songliao basin,NE China[J]. Petroleum Exploration and Development, 2018, 45(5):828-838.
[25]	彭军, 许天宇, 于乐丹. 东营凹陷沙河街组四段湖相细粒沉积特征及其控制因素[J]. 岩性油气藏, 2020, 32(5):1-12.
	PENG Jun, XU Tianyu, YU Ledan. Characteristics and controlling factors of lacustrine fine-grained sediments of the fourth member of Shahejie formation in Dongying depression[J]. Lithologic Reservoirs, 2020, 32(5):1-12.
[26]	姜在兴, 梁超, 吴靖, 等. 含油气细粒沉积岩研究的几个问题[J]. 石油学报, 2013, 34(6):1 031-1 039.
	JIANG Zaixing, LIANG Chao, WU Jing, et al. Several issues in sedimentological studies on hydrocarbon-bearing fine-grained sedimentary rocks[J]. Acta Petrolei Sinica, 2013, 34(6):1 031-1 039.
[27]	周立宏, 韩国猛, 马建英, 等. 歧口凹陷西南缘沙河街组一段下亚段古环境特征与沉积模式[J]. 石油学报, 2020, 41(8):903-917.
	ZHOU Lihong, HAN Guomeng, MA Jianying, et al. Palaeoenvironment characteristics and sedimentary model of the lower submember of member 1 of Shahejie formation in the southwestern margin of Qikou sag[J]. Acta Petrolei Sinica, 2020, 41(8):903-917.
[28]	李圯, 刘可禹, 蒲秀刚, 等. 沧东凹陷孔二段混合细粒沉积岩相特征及形成环境[J]. 地球科学, 2020, 45(10):3 779-3 796.
	LI Yi, LIU Keyu, PU Xiugang, et al. Lithofacies characteristics and formation environments of mixed fine-grained sedimentary rocks in second member of Kongdian formation in Cangdong depression,Bohai Bay basin[J]. Earth Science, 2020, 45(10):3 779-3 796.
[29]	李维, 朱筱敏, 段宏亮, 等. 苏北盆地高邮—金湖凹陷古近系阜宁组细粒沉积岩纹层特征与成因[J]. 古地理学报, 2020, 22(3):469-482.
	LI Wei, ZHU Xiaomin, DUAN Hongliang, et al. Characteristics and forming mechanism of laminae fine-grained sedimentary rock of the Paleogene Funing formation in Gaoyou and Jinhu sags,Subei basin[J]. Journal of Palaeogeography, 2020, 22(3):469-482.
[30]	ANGELA L, LAMB, MELANIE J, et al. Climatic and non-climatic effects on the δ¹⁸O and δ¹³C compositions of Lake Awassa,Ethiopia,during the last 6.5ka[J]. Quaternary Science Review, 2002, 21:2 199-2 211. doi: 10.1016/S0277-3791(02)00087-2
[31]	TALBOT M R. A review of the palaeohydrological interpretation of carbon and oxygen Isotopic ratios in primary lacustrine carbonates[J]. Chemical Geology Isotope Geoence, 1990, 80(4):261-279.
[32]	孙平昌. 松辽盆地东南部上白垩统含油页岩系有机质富集环境动力学[D]. 长春:吉林大学, 2013.
	SUN Pingchang. Environmental dynamics of organic accumulation in the oil shale bearing layers in the Upper Cretaceous,Southeast Songliao basin (NE China)[D]. Changchun: Jilin University, 2013.
[33]	HORACEK M, BRANDNER R, ABART R. Carbon isotope record of the P/T boundary and the Lower Triassic in the Southern Alps:evidence for rapid changes in storage of organic carbon[J]. Palaeogeography,Palaeoclimatology,Palaeoecology, 2007, 252(1/2):347-354. doi: 10.1016/j.palaeo.2006.11.049
[34]	马中良, 申宝剑, 潘安阳, 等. 四川盆地五峰组—龙马溪组页岩气成因与碳同位素倒转机制——来自热模拟实验的认识[J]. 石油实验地质, 2020, 42(3):428-433.
	MA Zhongliang, SHEN Baojian, PAN Anyang, et al. Origin and carbon isotope reversal of shale gas in Wufeng-Longmaxi formations, Sichuan basin: implication from pyrolysis experiments[J]. Petroleum Geology & Experiment, 2020, 42(3):428-433.
[35]	孔玉华, 沈新安, 李桂秋, 等. 陆西地区火山岩中碳酸盐矿物氧碳稳定同位素特征[J]. 新疆石油地质, 2009, 30(5):557-559.
	KONG Yuhua, SHEN Xin’an, LI Guiqiu, et al. Characteristic of carbonate oxygen-carbon stable isotopes in volcanic rocks in Luxi area,Junggar basin[J]. Xinjiang Petroleum Geology, 2009, 30(5):557-559.
[36]	KEITH M L, WEBER J N. Carbon and oxygen isotopic composition of selected limestones and fossils[J]. Geochimica Cosmochimica Acta, 1964, 28:1787-1816. doi: 10.1016/0016-7037(64)90022-5
[37]	EPSTEIN S, MAYEDA T K. Recised carbonate-water isotopic tempetrature scale[J]. Geological Society of America Bulletin, 1953, 64:1 315-1 326. doi: 10.1130/0016-7606(1953)64[1315:RCITS]2.0.CO;2
[38]	申家年, 王庆红, 何江林, 等. 松辽盆地白垩纪湖泊水体温度与古气候温度估算[J]. 吉林大学学报(地球科学版), 2008, 38(6):946-952.
	SHEN Jianian, WANG Qinghong, HE Jianglin, et al. Estimation of the ancient lake temperature and paleo-climate of the Cretaceous period in the Songliao basin[J]. Journal of Jilin University(Earth Science Edition), 2008, 38(6):946-952.
[39]	靳军, 张朝军, 刘洛夫, 等. 准噶尔盆地石炭系构造沉积环境与生烃潜力[J]. 新疆石油地质, 2009, 30(2):211-214.
	JIN Jun, ZHANG Chaojun, LIU Luofu, et al. Structural/sedimentary environment and hydrocarbon-generating potentials of carboniferous in Junggar basin[J]. Xinjiang Petroleum Geology, 2009, 30(2):211-214.
[40]	苑坤, 陈榕, 林拓, 等. 贵州南部晚石炭世沉积环境与古地理特征[J]. 石油实验地质, 2019, 41(1):38-44.
	YUAN Kun, CHEN Rong, LIN Tuo, et al. Petrological characteristics and sedimentary environment in the southern Guizhou during the Late Carboniferous[J]. Petroleum Geology & Experiment, 2019, 41(1):38-44.
[41]	刘忠宝, 刘光祥, 胡宗全, 等. 陆相页岩层系岩相类型、组合特征及其油气勘探意义——以四川盆地中下侏罗统为例[J]. 天然气工业, 2019, 39(12):10-21.
	LIU Zhongbao, LIU Guangxiang, HU Zongquan, et al. Lithofacies types and assemblage features of continental shale strata and their significance for shale gas exploration: A case study of the Middle and Lower Jurassic strata in the Sichuan Basin[J]. Natural Gas Industry, 2019, 39(12):10-21.
[42]	曹剑, 边立曾, 刘云田, 等. 柴达木盆地北缘中、下侏罗统烃源岩生烃潜力[J]. 新疆石油地质, 2009, 30(1):21-24.
	CAO Jian, BIAN Liceng, LIU Yuntian, et al. Hydrocarbon generative potentials of Middle and Lower Jurassic source rocks in northern margin of Qaidam basin[J]. Xinjiang Petroleum Geology, 2009, 30(1):21-24.
[43]	LANGFORD F F, BLANC-VALLERON M M. Interpreting rock-eval pyrolysis data using graphs of pyrolizable hydrocarbons vs. total organic carbon[J]. AAPG Bulletin, 1990, 74(6):799-804.

分类方式	参数	典型实例
定性	沉积层理构造	鄂尔多斯盆地延长组黏土岩^[15]
	颜色、结构、沉积构造、生物化石、矿物成分	荷兰下侏罗统Toarcian黑色页岩^[16]
		密西西比Barnett页岩^[17]
		Fort Worth盆地Barnett页岩^[18]
		吐哈盆地大河沿地区塔尔朗组细粒岩^[19]
	纹层组分	济阳坳陷古近系泥页岩^[20]
	粒度、沉积构造、有机地球化学	鄂尔多斯盆地延长组深水沉积岩^[21]
半定量	总有机碳、沉积构造、矿物成分	东营凹陷沙三下亚段—沙四上亚段细粒岩^[22]
		松辽盆地齐家—古龙凹陷青山口组黑色页岩^[23,24]
		东营凹陷沙河街组四段细粒岩^[25]
定量	总有机碳、碳酸盐矿物、黏土矿物	中国东部湖相含油气细粒岩^[26]
	长英质矿物、碳酸盐矿物、黏土矿物	歧口凹陷西南缘沙一下亚段细粒岩^[27]
	长英质矿物、碳酸盐矿物、黏土矿物	沧东凹陷孔二段细粒岩^[28]
	碳酸盐矿物、长石+石英、黏土矿物、纹层厚度	苏北盆地高邮—金湖凹陷阜宁组细粒岩^[29]

岩石分类	岩石名称	厚度/m	所占厚度比/%	岩石类型所占厚度比/%
富有机质陆源碎屑细粒岩	富有机质粉砂质泥岩	1.37	3.06	4.24
富有机质陆源碎屑细粒岩	富有机质泥质粉砂岩	0.55	1.18	4.24
中有机质陆源碎屑细粒岩	中有机质泥岩	6.35	13.80	13.80
贫有机质陆源碎屑细粒岩	贫有机质粉砂质细砂岩	1.93	4.50	59.35
	贫有机质粉砂岩	3.85	8.53
	贫有机质泥岩	21.93	46.32
贫有机质碳酸盐细粒岩	贫有机质白云质石灰岩	2.36	5.07	5.07
极贫有机质陆源碎屑细粒岩	极贫有机质细砂岩	0.83	1.73	15.27
	极贫有机质粉砂岩	2.81	6.02
	极贫有机质泥岩	3.50	7.52
极贫有机质碳酸盐细粒岩	极贫有机质鲕粒石灰岩	0.08	0.17	2.27
	极贫有机质叠层石石灰岩	0.62	1.31
	极贫有机质白云质石灰岩	0.37	0.79

松辽盆地青山口乡青山口组细粒沉积岩分类及其成因

Classification and Genesis of Fine-Grained Sedimentary Rocks of Qingshankou Formation in Songliao Basin

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