北羌塘拗陷巴贡组致密砂岩储层特征及控制因素

doi:10.11885/j.issn.1674-5086.2019.08.28.02

西南石油大学学报(自然科学版) ›› 2021, Vol. 43 ›› Issue (2): 10-22.DOI: 10.11885/j.issn.1674-5086.2019.08.28.02

北羌塘拗陷巴贡组致密砂岩储层特征及控制因素

程乐利¹, 白林坤², 韦少校², 熊亭^2,3, 印森林¹

1. 长江大学录井技术与工程研究院, 湖北荆州 434023;
2. 中法渤海地质服务有限公司深圳分公司, 广东深圳 518000;
3. 长江大学地球科学学院, 湖北武汉 430100

收稿日期:2019-08-28 出版日期:2021-04-10 发布日期:2021-04-23
通讯作者: 白林坤,E-mail:bailk@cfbgc.com
作者简介:程乐利,1987年生,男,汉族,湖北红安人,讲师,博士,主要从事储层地质和录井地质方面的研究工作。E-mail:chengleli@yangtzeu.edu.cn
白林坤,1978年生,男,汉族,山东济宁人,工程师,主要从事录井地质和储层地质方面的研究工作。E-mail:bailk@cfbgc.com
韦少校,1984年生,男,汉族,广西贵港人,助理工程师,主要从事地质录井方面的研究工作。E-mail:weisx@cfbgc.com
熊亭,1989年生,男,汉族,湖北潜江人,博士研究生,主要从事石油地质与地质录井方面的研究工作。E-mail:xiongting@cfbgc.com
印森林,1983年生,男,汉族,湖北仙桃人,副教授,博士,主要从事油气田开发地质与录井地质方面的研究工作。E-mail:yinxiang_love@qq.com
基金资助:
国家科技重大专项（2017ZX05008-006）；中国地质调查局项目（121201010000161110，DD21160159）；国家青年科学基金（41702119）

Characteristics and Controlling Factors of Tight Sandstone Reservoirs in Bagung Formation in North Qiangtang Depression

CHENG Leli¹, BAI Linkun², WEI Shaoxiao², XIONG Ting^2,3, YIN Senlin¹

1. Institute of Mud Logging Technology and Engineering, Yangtze University, Jingzhou, Hubei 434023, China;
2. Shenzhen Branch, China-Franch Bohai Geological Service Co. Ltd., Shenzhen, Guangdong 518000, China;
3. School of Geosciences, Yangtze University, Wuhan, Hubei 430100, China

Received:2019-08-28 Online:2021-04-10 Published:2021-04-23

摘要/Abstract

摘要： 北羌塘拗陷的上三叠统巴贡组碎屑岩是羌塘盆地的储层重点层系，分析沉积、成岩作用对巴贡组碎屑岩储层物性的影响机制，可以为下步勘探工作提供地质依据。研究表明，巴贡组砂岩总体的成分成熟度和结构成熟度中等偏低，溶蚀孔隙是主要的孔隙类型，孔隙结构表现为分选差、喉道细和连通差。沉积因素是控制优质储层的主要因素，形成于分流河道微相的砂层在形成时的水动力强、搬运远，其厚度更大、原生孔隙更为发育，由于抗压实能力强、保留有更多粒间孔隙，因此，后期酸性溶蚀更为发育。绿泥石衬里抑制了粒间硅质胶结物的形成，裂缝发育改善了储层物性，煤系特有的酸性介质环境亦促进了次生孔隙的形成。

关键词: 北羌塘拗陷, 巴贡组, 致密砂岩, 储层特征, 控制因素

Abstract: The Upper Triassic Bagung Formation clastic rocks in the North Qiangtang Depression are the key strata of reservoirs in the Qiangtang Basin. The study shows that the overall compositional maturity and structural maturity of the sandstone in the Bagung Formation are medium and low, the dissolution pores are the main reservoir space, and the pore structure is characteristic of small pore throat radius, poor sorting and poor connectivity. Dissolved pore space is the main pore type, and the pore structure shows poor sorting, fine roaring channel and poor connectivity. Sedimentary factors are the main factors controlling the quality of the reservoir. The sands formed in the microphase of the diversion channel are formed with strong hydrodynamic force and transported far away, and their thickness is larger and the primary pores are more developed, and the acidic dissolution is more developed in the later stage because of the strong compaction resistance and more intergranular pores are retained. The chlorite lining inhibits the formation of intergranular siliceous cement, the fracture development improves the reservoir properties, and the unique acidic medium environment of the coal system also promotes the formation of secondary pores.

Key words: North Qiangtang Depression, Bagung Formation, tight sandstone, reservoir characteristic, controlling factor

中图分类号:

TE122

程乐利, 白林坤, 韦少校, 熊亭, 印森林. 北羌塘拗陷巴贡组致密砂岩储层特征及控制因素[J]. 西南石油大学学报(自然科学版), 2021, 43(2): 10-22.

CHENG Leli, BAI Linkun, WEI Shaoxiao, XIONG Ting, YIN Senlin. Characteristics and Controlling Factors of Tight Sandstone Reservoirs in Bagung Formation in North Qiangtang Depression[J]. Journal of Southwest Petroleum University(Science & Technology Edition), 2021, 43(2): 10-22.

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参考文献

[1] 王剑,丁俊,王成善,等.青藏高原油气资源战略选区与评价[M].北京:地质出版社,2009. WANG Jian, DING Jun, WANG Chengshan, et al. Strategic selection and evaluation of oil and gas resources on the Qinghai-Tibet Plateau[M]. Beijing:Geological Press, 2009.
[2] 王成善,伊海生,李勇,等.西藏羌塘盆地地质演化与油气远景评价[M].北京:地质出版社,2001. WANG Chengshan, YI Haisheng, LI Yong, et al. Geological evolution and hydrocarbon prospect evaluation of Qiangtang Basin, Tibet[M]. Beijing:Geological Press, 2001.
[3] 丘东洲,乃东专,李晓清,等.羌塘盆地与特提斯域油气盆地类比及其含油气远景[J].沉积与特提斯地质,2007,27(3):1-13. doi:10.3969/j.issn.1009-3850.2007.03.001 QIU Dongzhou, NAI Dongzhuan, LI Xiaoqing, et al. Analog and hydrocarbon potential of the Qiangtang Basin and other petroleum basins in the Asian Tethys[J]. Sedimentary Geology and Tethyan Geology, 2007, 27(3):1-13. doi:10.3969/j.issn.1009-3850.2007.03.001
[4] 胡俊杰,李琦,张慧,等.北羌塘坳陷沃若山剖面上三叠统土门格拉组碎屑岩储集特征与主控因素[J].东华理工大学学报(自然科学版),2014,37(4):403-408. doi:10.3969/j.issn.1474-3504.2014.04.008 HU Junjie, LI Qi, ZHANG Hui, et al. Characteristics and controlling factors of Upper Triassic Tumengela Formation clastic rocks reservoir in Woruo mountains, North Qiangtang Basin[J]. Journal of East China Institute of Technology (Science and Technology Edition), 2014, 37(4):403-408. doi:10.3969/j.issn.1474-3504.2014.04.008
[5] FU Xiugen, WANG Jian, TAN Fuwen, et al. New insights about petroleum geology and exploration of Qiangtang Basin, Northern Tibet, China:A model for low-degree exploration[J]. Marine & Petroleum Geology, 2016, 77:323-340. doi:10.1016/j.marpetgeo.2016.06.015
[6] 孙冬胜,白玉宝,刘池阳,等.羌塘盆地羌南坳陷查郎拉地区储层的基本特征[J].西安石油大学学报(自然科学版),2001,16(5):1-3,10. doi:10.3969/j.issn.1673-064X.2001.05.001 SUN Dongsheng, BAI Yubao, LIU Chiyang, et al. Reservoir characteristics of Chalangla Area in South Depression of Qiangtang Basin[J]. Journal of Xi'an Petroleum Institute (Science and Technology Edition), 2001, 16(5):1-3, 10. doi:10.3969/j.issn.1673-064X.2001.05.001
[7] 侯宇.南羌塘坳陷上三叠统土门格拉组、中侏罗统雀莫错组沉积相分析与储层评价[D].成都:成都理工大学,2016,54-57. HOU Yu. Sedimentary facies analysis and reservoir evaluation of the Upper Triassic Tumengela Formation and the Middle Jurassic Quemocuo Formation in the South Qiangtang Depression, Tibet[D]. Chengdu:Chengdu University of Technology, 2016, 54-57.
[8] 赵靖舟,付金华,姚泾利,等.鄂尔多斯盆地准连续型致密砂岩大气田成藏模式[J].石油学报,2012,33(S1):37-52. doi:10.7623/syxb2012S1006 ZHAO Jingzhou, FU Jinhua, YAO Jingli, et al. Quasi-continuous accumulation model of large tight sandstone gas field in Ordos Basin[J]. Acta Petrolei Sinica, 2012, 33(S1):37-52. doi:10.7623/syxb2012S1006
[9] 王国亭,孙建伟,黄锦袖,等.神木气田低渗致密储层特征与水平井开发评价[J].西南石油大学学报(自然科学版),2019,41(5):1-9. doi:10.11885/j.issn.1674-5086.2018.07.20.01 WANG Guoting, SUN Jianwei, HUANG Jinxiu, et al. The characteristics of low permeability tight reservoir in the Shenmu Gas Field and the Evaluation of horizontal well development[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2019, 41(5):1-9. doi:10.11885/j.issn.1674-5086.2018.07.20.01
[10] 王雪柯,李伟,张本健,等.四川盆地西北部上三叠统须三段储层超致密与气藏超压成因[J]. 天然气工业,2019,39(11):25-35. doi:10.3787/j.issn.1000-0976.2019.11.004 WANG Xueke, LI Wei, ZHANG Benjian, et al. The formation mechanisms of ultra-tight and overpressured gas reservoir in the third Member of Upper Triassic Xujiahe Formation in the northwestern Sichuan Basin[J]. Natural Gas Industry, 2019, 39(11):25-35. doi:10.3787/j.issn.1000-0976.2019.11.004
[11] 斯尚华,任翔,赵玉涛,等.齐家地区高台子油层致密化与油气充注的关系[J].西南石油大学学报(自然科学版),2019,41(5):56-66. doi:10.11885/j.issn.1674-5086.2018.12.10.01 SI Shanghua, REN Xiang, ZHAO Yutao, et al. Relationship between densification and hydrocarbon filling of the Gaotaizi Oil Layer in the Qijia Area[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2019, 41(5):56-66. doi:10.11885/j.issn.1674-5086.2018.12.10.01
[12] 吕雪莹,蒋有录,刘景东,等.渤海湾盆地杜寨气田深层致密砂岩气成藏机理[J].天然气工业,2018,38(7):34-43. doi:10.3787/j.issn.1000-0976.2018.07.005 LÜ Xueying, JIANG Youlu, LIU Jingdong, et al. Accumulation mechanism of deep-seated tight sandstone gas reservoirs in the Duzhai Gas Field, Bohai Bay Basin[J]. Natural Gas Industry, 2018, 38(7):34-43. doi:10.3787/j.issn.1000-0976.2018.07.005
[13] 邹才能,朱如凯,吴松涛,等.常规与非常规油气聚集类型、特征、机理及展望——以中国致密油和致密气为例[J].石油学报,2012,33(2):173-187. doi:10.7623/syxb201202001 ZOU Caineng, ZHU Rukai, WU Songtao, et al. Types, characteristics, genesis and prospects of conventional and unconventional hydrocarbon accumulations:Taking tight oil and tight gas in China as an instance[J]. Acta Petrolei Sinica, 2012, 33(2):173-187. doi:10.7623/syxb201202001
[14] 孟万斌,吕正祥,冯明石,等.致密砂岩自生伊利石的成因及其对相对优质储层发育的影响——以川西地区须四段储层为例[J].石油学报,2011,32(5):783-790. doi:10.7623/syxb201105007 MENG Wanbin, LÜ Zhengxiang, FENG Mingshi, et al. The origin authigenic illite in tight sandstones and its effect on the formation of relatively high-quality reservoirs:A case study on sandstones in the 4th member of Xujiahe Formation, western Sichuan Basin[J]. Acta Petrolei Sinica, 2011, 32(5):783-790. doi:10.7623/syxb201105007
[15] 邵淑骁,曾溅辉,张善文,等.东营凹陷沙河街组砂岩储层高岭石类型、特征及其成因[J].沉积学报,2015,33(6):1204-1216. doi:10.14027/j.cnki.cjxb.2015.06.013 SHAO Shuxiao, ZENG Jianhui, ZHANG Shanwen, et al. Types, characteristics and origin of kaolinite in sandstone reservoir of Shahejie Formation, Dongying Sag[J]. Acta Sedimentology Sinica, 2015, 33(6):1204-1216. doi:10.14027/j.cnki.cjxb.2015.06.013
[16] 黄思静,黄可可,冯文立,等.成岩过程中长石、高岭石、伊利石之间的物质交换与次生孔隙的形成:来自鄂尔多斯盆地上古生界和川西凹陷三叠系须家河组的研究[J].地球化学,2009,38(5):498-506. doi:10.3321/j.issn:0379-1726.2009.05.009 HUANG Sijing, HUANG Keke, FENG Wenli, et al. Mass exchanges among feldspar, kaolinite and illite and their influences on secondary porosity formation in clastic diagenesis:A case study on the Upper Paleozoic, Ordos Basin and Xujiahe Formation, western Sichuan Depression[J]. Geochimica, 2009, 38(5):498-506. doi:10.3321/j.issn:0379-1726.2009.05.009
[17] 张哨楠,丁晓琪,万友利,等.致密碎屑岩中粘土矿物的形成机理与分布规律[J].西南石油大学学报(自然科学版),2012,34(3):174-182. doi:10.3863/j.issn.1674-5086.2012.03.027 ZHANG Shaonan, DING Xiaoqi, WAN Youli, et al. Formation mechanism and distribution of clay minerals of deeply tight siliciclastic reservoirs[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2012, 34(3):174-182. doi:10.3863/j.issn.1674-5086.2012.03.027
[18] 田建锋,喻建,张庆洲.孔隙衬里绿泥石的成因及对储层性能的影响[J].吉林大学学报(地球科学版),2014,44(3):741-748. doi:10.13278/j.cnki.jjuese.201403103 TIAN Jianfeng, YU Jian, ZHANG Qingzhou. The pore-lining chlorite formation mechanism and its contribution to reservoir quality[J]. Journal of Jilin University (Earth Science Edition), 2014, 44(3):741-748. doi:10.13278/j.cnki.jjuese.201403103
[19] 马鹏杰,林承焰,张世奇,等.碎屑岩储集层中绿泥石包膜的研究现状[J].古地理学报,2017,19(1):147-159. doi:10.7605/gdlxb.2017.01.012 MA Pengjie, LIN Chengyan, ZHANG Shiqi, et al. An overview on study of chlorite films in clastic reservoirs[J]. Journal of Palaeogeography, 2017, 19(1):147-159. doi:10.7605/gdlxb.2017.01.012
[20] 王琪,郝乐伟,陈国俊,等.白云凹陷珠海组砂岩中碳酸盐胶结物的形成机理[J].石油学报,2010,31(4):553-558,565. doi:10.1016/S1876-3804(11)60008-6 WANG Qi, HAO Lewei, CHEN Guojun, et al. Forming mechanism of carbonate cements in siliciclastic sandstone of Zhuhai Formation in Baiyun Sag[J]. Acta Petrolei Sinica, 2010, 31(4):553-558, 565. doi:10.1016/S1876-3804(11)60008-6
[21] 郑浚茂,应凤祥.煤系地层(酸性水介质)的砂岩储层特征及成岩模式[J].石油学报,1997,18(4):19-24. doi:10.7623/syxb199704004 ZHENG Junmao, YING Fengxiang. Reservoir characteristics and diagenetic model of sandstone intercalated in coal-bearing strata (acid water medium)[J]. Acta Petrolei Sinica, 1997, 18(4):19-24. doi:10.7623/syxb199704004
[22] 杨晓萍,赵文智,邹才能,等.低渗透储层成因机理及优质储层形成与分布[J].石油学报,2007,28(4):57-61. YANG Xiaoping, ZHAO Wenzhi, ZOU Caineng, et al. Origin of low-permeability reservoir and distribution of favorable reservoir[J]. Acta Petrolei Sinica, 2007, 28(4):57-61.
[23] 纪友亮,周勇,刘玉瑞,等.高邮凹陷古近系阜宁组一段沉积特征对储层成岩作用及物性的影响[J].地质学报,2014,88(7):1299-1310. doi:10.3969/j.issn.0001-5717.2014.07.007 JI Youliang, ZHOU Yong, LIU Yurui, et al. The impact of sedimentary characteristics on the diagenesis and reservoir quality of the 1^st Member of Paleogene Funing Formation in the Gaoyou Subbasin[J]. Acta Geologica Sinica, 2014, 88(7):1299-1310. doi:10.3969/j.issn.0001-5717.2014.07.007
[24] 吴胜和,马晓芬.煤系地层低渗透岩屑砂岩储层成因机理及储集特征[J]. 低渗透油气田,1996,1(1):13-17. WU Shenghe, MA Xiaofen. Formation mechanism and reservoir characteristics of low permeability lithic sandstone reservoirs in coal measure formation[J]. Low Permeability Oil and Gas Field, 1996, 1(1):13-17.
[25] 远光辉,操应长,贾珍臻,等.含油气盆地中深层碎屑岩储层异常高孔带研究进展[J].天然气地球科学,2015,26(1):28-42. doi:10.11764/j.issn.1672-1926.2014.01.0028 YUAN Guanghui, CAO Yingchang, JIA Zhenzhen, et al. Research progress on anomalously high porosity zones in deeply buried clastic reservoirs in petroliferous basin[J]. Natural Gas Geoscience, 2015, 26(1):28-42. doi:10.11764/j.issn.1672-1926.2014.01.0028
[26] 付金华,邓秀芹,张晓磊,等.鄂尔多斯盆地三叠系延长组深水砂岩与致密油的关系[J].古地理学报,2013,15(5):624-634. doi:10.7605/gdlxb.2013.05.050 FU Jinhua, DENG Xiuqin, ZHANG Xiaolei, et al. Relationship between deepwater sandstone and tight oil of the Triassic Yanchang Formation in Ordos Basin[J]. Journal of Palaeogeography, 2013, 15(5):624-634. doi:10.7605/gdlxb.2013.05.050
[27] BERGER A, GIER S, KROIS P. Porosity-preserving chlorite cements in shallow-marine volcaniclastic sandstones:Evidence from Cretaceous sandstones of the Sawan Gas Field, Pakistan[J]. AAPG Bulletin, 2009, 93(5):595-615. doi:10.1306/01300908096
[28] GOULD K, PEPIPER G, PIPER D J W. Relationship of diagenetic chlorite rims to depositional facies in Lower Cretaceous reservoir sandstones of the Scotian Basin[J]. Sedimentology, 2010, 57(2):587-610. doi:10.1111/j.1365-3091.2009.01106.x
[29] 黄思静,谢连文,张萌,等.中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储层孔隙保存的关系[J].成都理工大学学报(自然科学版),2004,31(3):273-281. doi:10.3969/j.issn.1671-9727.2004.03.009 HUANG Sijing, XIE Lianwen, ZHANG Meng, et al. Formation mechanism of authigenic chlorite and relation to preservation of porosity in nonmarine Triassic reservoir sandstones, Ordos Basin and Sichuan Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2004, 31(3):273-281. doi:10.3969/j.issn.1671-9727.2004.03.009
[30] 田建锋,陈振林,凡元芳,等.砂岩中自生绿泥石的产状、形成机制及其分布规律[J].矿物岩石地球化学通报,2008,27(2):200-205. doi:10.3969/j.issn.1007-2802.2008.02.015 TIAN Jianfeng, CHEN Zhenlin, FAN Yuanfang, et al. The occurrence, growth mechanism and distribution of authigenic chlorite in sandstone[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2008, 27(2):200-205. doi:10.3969/j.issn.1007-2802.2008.02.015
[31] 仙麦龙,王辉,马君龙,等.羌塘盆地晚三叠世含煤岩系沉积体系与层序地层学特征[J].中国煤炭地质,2012,24(4):1-5. doi:10.3969/j.issn.1674-1803.2012.04.01 XIAN Mailong, WANG Hui, MA Junlong, et al. Late Triassic coal-bearing rock series depositional system and sequence stratigraphic features in Qiangtang Basin[J]. Coal Geology of China, 2012, 24(4):1-5. doi:10.3969/j.issn.1674-1803.2012.04.01
[32] 柯丹丹,毛晓冬,廖云君,等.浅议西藏区域地层区划及其含煤地层[J].华南地质与矿产,2014,30(1):50-57. doi:10.3969/j.issn.1007-3701.2014.01.007 KE Dandan, MAO Xiaodong, LIAO Yunjun, et al. Brief study on the regional stratigraphic division and coal-bearing strata in Tibet[J]. Geology and Minaeral Resources of South China, 2014, 30(1):50-57. doi:10.3969/j.issn.1007-3701.2014.01.007

北羌塘拗陷巴贡组致密砂岩储层特征及控制因素

Characteristics and Controlling Factors of Tight Sandstone Reservoirs in Bagung Formation in North Qiangtang Depression

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