黄骅坳陷大港探区下古生界碳酸盐岩潜山差异演化及优质储层成因

doi:10.11743/ogg20210313

石油与天然气地质 ›› 2021, Vol. 42 ›› Issue (3): 673-689.doi: 10.11743/ogg20210313

黄骅坳陷大港探区下古生界碳酸盐岩潜山差异演化及优质储层成因

程鑫^1,²(), 周立宏³, 操应长^1,^4,*(), 金凤鸣³, 付立新³, 李宏军³, 楼达³, 远光辉^1,⁴

1. 中国石油大学(华东) 深层油气重点实验室, 山东青岛 266580
2. 中海石油(中国)有限公司天津分公司, 天津 300459
3. 中国石油大港油田分公司, 天津 300280
4. 海洋矿产资源评价与探测技术国家功能实验室, 山东青岛 266071

收稿日期:2019-03-04 出版日期:2021-06-28 发布日期:2021-06-23
通讯作者: 操应长 E-mail:645719710@qq.com;cyc8391680@163.com
第一作者简介:程鑫(1990—)，男，博士研究生，油气储层。E-mail: 645719710@qq.com
基金项目:
国家科技重大专项(2016ZX05006-007);研究生自主创新项目(16CX06042A);大港油田公司与中国石油大学（华东）校企合作项目(DGYI-2016-JS-586)

Differential evolution and origin of high-quality reservoirs in the Lower Paleozoic carbonate buried hills in Dagang prospecting area, Huanghua Depression

Xin Cheng^1,²(), Lihong Zhou³, Yingchang Cao^1,^4,*(), Fengming Jin³, Lixin Fu³, Hongjun Li³, Da Lou³, Guanghui Yuan^1,⁴

1. Key Laboratory of Deep Oil and Gas, China University of Petroleum (East China), Qingdao, Shandong 266580, China
2. Tianjin Branch of CNOOC Ltd., Tianjin 300459, China
3. Dagang Oilfield Branch, PetroChina, Tianjin 300280, China
4. Laboratory for Marine Mineral Resources, Qingdao, Shandong 266071, China

Received:2019-03-04 Online:2021-06-28 Published:2021-06-23
Contact: Yingchang Cao E-mail:645719710@qq.com;cyc8391680@163.com

摘要/Abstract

摘要：

碳酸盐岩潜山储层成因及分布的复杂性制约了该类油藏的勘探。综合利用地震资料、岩心-薄片观察、测-录井分析、地化分析以及埋藏史分析等技术方法，从构造演化差异性角度对大港探区下古生界碳酸盐岩潜山进行分类，并开展了储集差异性和优质储层成因研究。大港探区下古生界碳酸盐岩潜山可以划分为残丘山、间断侵蚀断块山、断块山、挤压褶皱山和重力滑动褶皱山5种类型。残丘山为晚期大气水淋滤型储层，储集空间以岩溶孔、洞为主，发育少量裂缝；间断侵蚀断块山为中期大气水淋滤-深部溶蚀共控型储层，溶孔和裂缝均较发育；断块山、挤压褶皱山和重力滑动褶皱山未经历中、晚期表生淋滤，储层成因与断裂和埋深密切相关，可分为断裂破碎-深部溶蚀共控和断裂沟通-TSR溶蚀共控2种成因类型。前者在靠近基底断裂部分发育孔、洞、缝复合型储层，随着距基底断层距离增加，逐渐变为裂缝主导型储层，溶孔含量降低；后者主要发育在地温较高（>140 ℃）的深埋区，储集空间以裂缝为主，发育部分溶蚀孔、洞。上古生界缺失区、基底断层发育区和发育上古生界的深埋高温区（>140 ℃）可作为优质储层预测的有利指向。

关键词: 潜山分类, 储集特征, 储层成因, 碳酸盐岩, 下古生界, 大港探区, 黄骅坳陷

Abstract:

The exploration for carbonate reservoirs in buried hills has been hampered by a poor understanding of their distribution and genesis.With a combination of seismic profile interpretation, core and thin section observation, logging analysis as well as geochemical and burial history analysis, the types of the Lower Paleozoic buried hills, reservoir characteristics and genesis of high-quality reservoirs in Dagang prospecting area were studied from the perspective of evolutional difference.The buried-hills in the area can be classified into five categories: monadnock, intermittently eroded fault-block buriedhill, fault-block buried hill, compressional folded buried hill and gravitational sliding folded buried hill.The monadnock resulted from a late-stage meteoric water leaching is dominated by dissolution pores and cavities, followed by some fissures.The intermittently eroded fault-block, a result of middle-stage meteoric water leaching and deep burial dissolution, is full of dissolution pores and tectonic fissures.The last three buried hills that shunned the middle- or late-stage meteoric water leaching contain reservoirs linked to faulting and deep burial and formed either by fault-related shattering-deep burial dissolution or by fault connection-TSR related dissolution.The former forms mostly composite reservoirs with dissolution pores, cavities and fissures in areas close to basement faults and would gradually turn into tectonic fissure-dominated reservoirs as they migrate away from the basement faults.The latter forms reservoirs commonly seen in deep buried formations with very high temperatures (higher than 140 ℃).These reservoirs are mainly composed of fissures, followed by some dissolution pores and cavities.It is therefore suggested that high-quality reservoirs are most probably developed in areas with the Upper Paleozoic strata heavily eroded or basement faults well developed or with the Upper Paleozoic strata developed against a high temperature setting (higher than 140 ℃).

Key words: buried hill classification, reservoir characteristics, origin of high-quality reservoirs, carbonate rock, Lower Paleozoic, Dagang prospecting area, Huanghua Depression

中图分类号:

TE122.2

程鑫,周立宏,操应长,等. 黄骅坳陷大港探区下古生界碳酸盐岩潜山差异演化及优质储层成因[J]. 石油与天然气地质, 2021, 42(3): 673-689. doi: 10.11743/ogg20210313 Xin Cheng,Lihong Zhou,Yingchang Cao,et al. Differential evolution and origin of high-quality reservoirs in the Lower Paleozoic carbonate buried hills in Dagang prospecting area, Huanghua Depression[J]. Oil & Gas Geology, 2021, 42(3): 673-689. doi: 10.11743/ogg20210313

图/表 11

图1

图2

图3

图4

图5

图6

表1

图7

图8

图9

图10

参考文献 55

1	赵文龙, 韩春元, 严梦颖, 等. 冀中坳陷北部奥陶系储层形成机理与分布模式[J]. 特种油气藏, 2019, 27 (5): 61- 67.
	Zhao Wenlong , Han Chunyuan , Yan Mengying , et al. Formation mechanism and distribution models of Ordovician reservoirs in northern Jizhong depression[J]. Special oil & Gas Reservoirs, 2019, 27 (5): 61- 67.
2	吴永平, 付立新, 杨池银, 等. 黄骅坳陷中生代构造演化对潜山油气成藏的影响[J]. 石油学报, 2002, 23 (2): 16- 21.
	Wu Yongping , Fu Lixin , Yang Chiyin , et al. Effect of Mesozoic tectonic evolution on hydrocarbon accumulation in buried hills in Huanghua depression[J]. Acta Petrolei Sinica, 2002, 23 (2): 16- 21.
3	杨明慧. 渤海湾盆地潜山多样性及其成藏要素比较分析[J]. 石油与天然气地质, 2008, 29 (5): 623- 630. doi: 10.3321/j.issn:0253-9985.2008.05.011
	Yang Minghui . Diversity of buried-hills and comparison of their hydrocarbon-pooling factors in the Bohai Bay Basin[J]. Oil&Gas Geology, 2008, 29 (5): 623- 630. doi: 10.3321/j.issn:0253-9985.2008.05.011
4	韩志宁. 广饶碳酸盐岩古潜山油藏储层特征研究[D]. 青岛: 中国石油大学(华东), 2011.
	Han Zhining. Study on the Reservoir characteristics of Carbonate Buried Hill in GuangraoOilfield[D]. Qingdao: China University of Petroleum(East China), 2011.
5	李欣, 闫伟鹏, 崔周旗, 等. 渤海湾盆地潜山油气藏勘探潜力与方向[J]. 石油实验地质, 2012, 34 (2): 140- 152. doi: 10.3969/j.issn.1001-6112.2012.02.007
	Li Xin , Yan Weipeng , Cui Zhouqi , et al. Prospecting potential and targets of buried- hill oil and gas reservoirs in Bohai Bay Basin[J]. Petroleum Geology and Experiment, 2012, 34 (2): 140- 152. doi: 10.3969/j.issn.1001-6112.2012.02.007
6	李欣, 李建忠, 杨涛, 等. 渤海湾盆地油气勘探现状与勘探方向[J]. 新疆石油地质, 2013, 34 (2): 140- 144.
	Li Xin , Li Jianzhong , Yang Tao , et al. Oil-gas exploration status and future targets in Bohai Bay Basin[J]. Xinjiang Petroleum Geology, 2013, 34 (2): 140- 144.
7	蒋有录, 叶涛, 张善文, 等. 渤海湾盆地潜山油气富集特征与主控因素[J]. 中国石油大学学报, 2015, 39 (9): 20- 29.
	Jiang Youlu , Ye Tao , Zhang Shanwen , et al. Enrichment characteristics and main controlling factors of hydrocarbon in buried hill of Bohai Bay Basin[J]. Journal of China University of Petroleum, 2015, 39 (9): 20- 29.
8	赵贤正, 金凤鸣, 王权, 等. 渤海湾盆地牛东1超深潜山高温油气藏的发现及其意义[J]. 石油学报, 2011, 32 (6): 915- 925.
	Zhao Xianzheng , Jin Fengming , Wang Quan , et al. Niudong 1 ultra-deep and ultra-temperature subtle buried hill field in Bohai Bay basin: discovery and significance[J]. Acta Petrolei Sinica, 2011, 32 (6): 915- 925.
9	赵贤正, 金凤鸣, 王权, 等. 冀中坳陷隐蔽深潜山及潜山内幕油气藏的勘探发现与认识[J]. 中国石油勘探, 2014, 19 (1): 10- 21. doi: 10.3969/j.issn.1672-7703.2014.01.002
	Zhao Xianzheng , Jin Fengming , Wang Quan , et al. Exploration and discovery of subtle deep buried hill and buried hill inner-curtain hydrocarbon reservoir in Jizhong sag[J]. China Petroleum Exploration, 2014, 19 (1): 10- 21. doi: 10.3969/j.issn.1672-7703.2014.01.002
10	赵贤正, 王权, 金凤鸣, 等. 渤海湾盆地富油凹陷二次勘探工程及其意义[J]. 石油勘探与开发, 2015, 42 (6): 723- 733.
	Zhao Xianzheng , Wang Quan , Jin Fengming , et al. Re-exploration program for petroleum-rich sags and its significance in Bohai Bay Basin, EastChina[J]. Petroleum Exploration and Development, 2015, 42 (6): 723- 733.
11	高长海, 张新征, 查明, 等. 冀中坳陷潜山油气藏特征[J]. 岩性油气藏, 2011, 23 (6): 6- 12. doi: 10.3969/j.issn.1673-8926.2011.06.004
	Gao Changhai , Zhang Xinzheng , Zha Ming , et al. Characteristics of buried hill reservoir in Jizhong depression[J]. Lithologic Reservoirs, 2011, 23 (6): 6- 12. doi: 10.3969/j.issn.1673-8926.2011.06.004
12	方杰, 吴小洲, 王居峰. 黄骅坳陷下古生界深潜山油气聚集条件及成藏因素分析[J]. 中国石油勘探, 2013, 18 (4): 11- 18. doi: 10.3969/j.issn.1672-7703.2013.04.002
	Fang Jie , Wu Xiaozhou , Wang Jufeng . Accumulation conditions and reservoiring factors of deep buried hills of lower Paleozoic in Huanghua depression[J]. China Petroleum Exploration, 2013, 18 (4): 11- 18. doi: 10.3969/j.issn.1672-7703.2013.04.002
13	Palmer A N . Origin and morphology of limestone caves[J]. Geological Society of America Bulletin, 1991, 1- 21+25.
14	Palmer A N. Geochemical models for the origin of macroscopic solution porosity in carbonate rocks[G]//Budd D A, Harris P M, 1Saller A, Unconformities in carbonate strata: their recognition and the significance of associated porosity, American Association of Petroleum Geologists, Memoir 63, 1995, 77-101.
15	Loucks R G . Paleocave carbonate reservoirs: origins, burial-depth modifications, spatial complexity, and reservoir implications[J]. AAPG Bulletin, 1999, 83 (11): 1795- 1834.
16	孙福宁, 胡文瑄, 胡忠亚, 等. 断裂-层序双控机制下的热液活动及成储效应——以塔里木盆地塔河、玉北地区下奥陶统为例[J]. 石油与天然气地质, 2020, 41 (3): 558- 575.
	Sun Funing , Hu Wenxuan , Hu Zhongya , et al. Impact of hydrothermal activities on reservoir formation controlled by both faults and sequences boundaries: A case study from the Lower Ordovician in Tahe and Yubeiareas, Tarim Basin[J]. Oil & Gas Geology, 2020, 41 (3): 558- 575.
17	丁茜, 何治亮, 王静彬, 等. 生烃伴生酸性流体对碳酸盐岩储层改造效应的模拟实验[J]. 石油与天然气地质, 2020, 41 (1): 223- 234.
	Ding Qian , He Zhiliang , Wang Jingbin , et al. Simulation experiment of carbonate reservoir modification by source rock-derived acidic fluids[J]. Oil & Gas Geology, 2020, 41 (1): 223- 234.
18	付立新, 胡见义. 黄骅盆地奥陶系古岩溶特征、演化及其对潜山油气聚集的控制作用[J]. 海相油气地质, 2001, 6 (2): 21- 27. doi: 10.3969/j.issn.1672-9854.2001.02.004
	Fu Lixin , Hu Jianyi . Characteristics and evolution Ordovician palaeo-karst in Huanghua Basin and its control on oil and gas accumulation[J]. Marine Origin Petroleum Geology, 2001, 6 (2): 21- 27. doi: 10.3969/j.issn.1672-9854.2001.02.004
19	夏日元, 唐健生. 黄骅坳陷奥陶系古岩溶发育演化模式[J]. 石油勘探与开发, 2004, 31 (1): 51- 53. doi: 10.3321/j.issn:1000-0747.2004.01.015
	Xia Riyuan , Tang Jiansheng . The developed and evaluated patterns of Ordovician palaeokarst in the Huanghua depression[J]. Petroleum Exploration and Development, 2004, 31 (1): 51- 53. doi: 10.3321/j.issn:1000-0747.2004.01.015
20	朱光有, 张水昌, 梁英波. 四川盆地深部海相优质储集层的形成机理及其分布预测[J]. 石油勘探与开发, 2006, 33 (2): 161- 166. doi: 10.3321/j.issn:1000-0747.2006.02.008
	Zhu Guangyou , Zhang Shuichang , Liang Yingbo . Formation mechanism and distribution predictionofhigh-quality marine reservoir in deeper Sichuan Basin[J]. Petroleum Exploration and Development, 2006, 33 (2): 161- 166. doi: 10.3321/j.issn:1000-0747.2006.02.008
21	李开开, 蔡春芳, 蔡镠璐, 等. 塔河地区下古生界热液流体及储层发育主控因素探讨—以S88和TS1井为例[J]. 石油实验地质, 2010, 32 (1): 46- 51. doi: 10.3969/j.issn.1001-6112.2010.01.009
	Li Kaikai , Cai Chunfang , Cai Liulu , et al. Hydrothermal fluid activities and main controlling factor of deep reservoir development in the lower Paleozoic of the Tahe oilfield—taking wells S88 and TS1 as examples[J]. Petroleum Geology and Experiment, 2010, 32 (1): 46- 51. doi: 10.3969/j.issn.1001-6112.2010.01.009
22	Dravis J J , Muir I D . Deep-burial dissolution and brecciation in dolostone reservoirs: Striking similarities between the Devonian Keg River Formation of western Canada and the Ordovician Ellenburger group of west Texas[J]. Interpretation, 2014, 2 (4): T221- T241. doi: 10.1190/INT-2014-0167.1
23	Ennes-Silva R A , Bezerra F H R , Nogueira F C C , et al. Superposed folding and associated fracturing influence hypogene karst development in Neoproterozoic carbonates, São Francisco Craton, Brazil[J]. Tectonophysics, 2016, 666, 244- 259. doi: 10.1016/j.tecto.2015.11.006
24	李继岩, 王永诗, 刘传虎, 等. 热液流体活动及其对碳酸盐岩储集层改造定量评价——以渤海湾盆地东营凹陷西部下古生界为例[J]. 石油勘探与开发, 2016, 43 (3): 359- 366.
	Li Jiyan , Wang Yongshi , Liu Chuanhu , et al. Hydrothermal fluid activity and the quantitative evaluation of its impact on carbonate reservoirs: A case study of the Lower Paleozoic in the west of Dongying sag, Bohai Bay Basin, East China[J]. Petroleum Exploration and Development, 2016, 43 (3): 359- 366.
25	刘子豪, 朱东亚, 吴胜和, 等. 中国南方地区奥陶系热液-岩溶改造型白云岩储层发育机理——以黔中地区下奥陶统为例[J]. 海相油气地质, 2017, 22 (2): 51- 58. doi: 10.3969/j.issn.1672-9854.2017.02.007
	Liu Zihao , Zhu Dongya , Wu Shenghe , et al. Developmental mechanism of Ordovician dolostone reservoir altered by hydrothermal karstification in southern China: An example from Qianzhong uplift, Guizhou province[J]. Marine Origin Petroleum Geology, 2017, 22 (2): 51- 58. doi: 10.3969/j.issn.1672-9854.2017.02.007
26	昝念民, 王艳忠, 操应长, 等. 东营凹陷下古生界碳酸盐岩古潜山储层储集空间特征及发育模式[J]. 石油与天然气地质, 2018, 39 (2): 355- 365.
	Zan Nianmin , Wang Yanzhong , Cao Yingchang , et al. Characteristics and development patterns of reservoir space of the lower Paleozoic buried hills in Dongying Sag, Bohai Bay Basin[J]. Oil & Gas Geology, 2018, 39 (2): 355- 365.
27	Hans G Machel , Mary Luz Borrero , Eugene Dembicki . The Grosmont: a complex dolomitized, fractured and karstified heavy oil reservoir in a Devonian carbonate-evaporite platform[J]. GeoConvention, 2012, Vision.
28	金振奎, 邹元荣, 蒋春雷, 等. 大港探区奥陶系岩溶储层发育分布控制因素[J]. 沉积学报, 2001, 19 (4): 530- 535. doi: 10.3969/j.issn.1000-0550.2001.04.009
	Jin Zhenkui , Zou Yuanrong , Jiang Chunlei , et al. Distribution and controlling factors of Ordovician karst reservoirs in Dagang Region[J]. Acta Sedimentologica Sinica, 2001, 19 (4): 530- 535. doi: 10.3969/j.issn.1000-0550.2001.04.009
29	徐学纯, 邹海峰, 刘立, 等. 大港探区古流体特征及其地质意义[J]. 地学前缘, 2001, 8 (4): 363- 371. doi: 10.3321/j.issn:1005-2321.2001.04.016
	Xu Xuechun , Zou Haifeng , Liu Li , et al. The features and geological significance of the paleo-fluid in Dagang exploration area[J]. Earth Science Frontiers, 2001, 8 (4): 363- 371. doi: 10.3321/j.issn:1005-2321.2001.04.016
30	付立新, 楼达, 李宏军, 等. 印支-燕山运动对大港探区古潜山形成的控制作用[J]. 石油学报, 2016, 37 (增刊2): 19- 30.
	Fu Lixin , Lou Da , Li Hongjun , et al. Indosinian-Yanshan movement on the formation of buried hill in Dagang exploration area[J]. Acta Petrolei Sinica, 2016, 37 (S2): 19- 30.
31	侯中帅, 陈世悦, 鄢继华, 等. 大港探区上古生界沉积特征与控制因素[J]. 地球科学, 2017, 42(11): 2055-2068, 2104.
	Hou Zhongshuai, Chen Shiyue, Yan Jihua, et al. Sedimentary characteristics and control factors of Upper Palaeozoic in Dagang exploration Area[J]. Journal of Earth Science, 2017, 42(11): 2055-2068, 2104.
32	杨明慧, 王嗣敏, 陈善勇, 等. 渤海湾盆地黄骅坳陷奥陶系碳酸盐岩潜山成因分类与分布[J]. 石油与天然气地质, 2005, 26 (3): 310- 315. doi: 10.3321/j.issn:0253-9985.2005.03.008
	Yang Minghui , Wang Simin , Chen Shanyong , et al. Genetic classification and distribution of Ordovician carbonate buried hill in Huanghua depresssion, Bohai Bay Basin[J]. Oil & Gas Geology, 2005, 26 (3): 310- 315. doi: 10.3321/j.issn:0253-9985.2005.03.008
33	李建东, 苏立萍, 赵腊腊, 等. 大港探区千米桥奥陶系潜山裂缝分布预测[J]. 中国石油勘探, 2010, 15 (5): 48- 53.
	Li Dongjian , Su Liping , Zhao Lala , et al. Distribution and prediction of fissures in Qianmiqiao Buried Hill of Ordovician[J]. China Petroleum Exploration, 2010, 15 (5): 48- 53.
34	楼达, 李三忠, 金宠, 等. 黄哗坳陷中区中生代构造演化[J]. 海洋地质与第四纪地质, 2008, 28 (3): 43- 53.
	Lou Da , Li Sanzhong , Jin Pang , et al. Evolution of the Mesozoic Strata in the middle range of the Huanghua depression[J]. Marine Geology & Quaternary Geology, 2008, 28 (3): 43- 53.
35	杨池银, 张一伟. 黄骅地区叠合盆地演化与潜山油气聚集[J]. 石油勘探与开发, 2003, 30 (6): 8- 12. doi: 10.3321/j.issn:1000-0747.2003.06.003
	Yang Chiyin , Zhang Yiwei . Huanghua superimposed basin evolution and oil & gas accumulation in buried hill[J]. Petroleum Exploration and Development, 2003, 30 (6): 8- 12. doi: 10.3321/j.issn:1000-0747.2003.06.003
36	梁书义. 车西地区古潜山储层特征与形成机制[D]. 中国青岛: 中国石油大学(华东), 2006.
	Liang Shuyi. Geoburried-hills Reservoir characteristics and forming- mechanism In Chexi Area[D]. Qingdao: China University of Petroleum(East China).
37	李三忠, 索艳慧, 周立宏, 等. 华北克拉通内部的拉分盆地: 渤海湾盆地黄骅坳陷结构构造与演化[J]. 吉林大学学报(地球科学版), 2011, 41 (5): 1362- 1379.
	Li Sanzhong , Suo Yanhui , Zhou Lihong , et al. Pull-apart basins within the north China craton: structral pattern and evolution of Huanghua depression in Bohai Bay Basin[J]. Journal of Jilin University(Earth Science Edition), 2011, 41 (5): 1362- 1379.
38	卢刚臣. 渤海湾盆地黄骅坳陷潜山演化历程及展布规律研究[D]. 中国武汉: 中国地质大学(武汉), 2013.
	Lu Chengang. The Evolutionary history and distributional regularities of Huanghua depression buried hillsin Bohai Bay Basin[D]. Wuhan: China Universityof Geosciences, 2013.
39	王文庆, 李岳桐, 卢刚臣, 等. 黄骅坳陷中部潜山地质特征及油气勘探方向[J]. 断块油气田, 2017, 24 (5): 19- 23.
	Wang Qingwen , Li Yuetong , Lu Chengang , et al. Geological characteristics and hydrocarbon exploration direction in buried-hill, central Huanghua depression[J]. Fault-Block Oil & GasField, 2017, 24 (5): 19- 23.
40	杜旭东, 漆家福, 陆克政, 付立新. 大港探区中生代盆地构造特征及演化[J]. 石油实验地质, 2000, 22 (2): 125- 130. doi: 10.3969/j.issn.1001-6112.2000.02.006
	Du Xudong , Qi Jiafu , Lu Kezheng , Fu Lixin . Evolution and tectonic characteristics of the Mesozoic basin in Dagang prospect area[J]. Experimental Petroleum Geology, 2000, 22 (2): 125- 130. doi: 10.3969/j.issn.1001-6112.2000.02.006
41	于炳松. 阴极发光显微镜在碳酸盐岩研究中的应用及其进展[J]. 地质科技情报, 1992, 11 (4): 92- 96.
	Yu Bingsong . The application and development of cathodoluminescence microscope in the study of carbonate rocks[J]. Geological Science and Technology Information, 1992, 11 (4): 92- 96.
42	赖勇. 阴极发光技术在成岩成矿作用研究中的应用[J]. 北京大学学报(自然科学版), 1995, 31 (5): 631- 638.
	Lai Yong . Application of cathodoluminescence tomineraliztion and lithogenesis studying[J]. Acta Scientiarum Naturalium, 1995, 31 (5): 631- 638.
43	肖晖, 赵靖舟. 鄂尔多斯盆地靖边气田奥陶系马家沟组的阴极发光特征及白云岩化[J]. 西安石油大学学报(自然科学版), 2013, 28 (4): 1- 7. doi: 10.3969/j.issn.1673-064X.2013.04.001
	Xiao Hui , Zhao Jingzhou . Cathodoluminescence characteristics and dolomitization of Ordovician Majiagou formation in Jinbian gasfield, Ordos basin[J]. Journal of Xi'an Shiyou University(Natrual Science Edition), 2013, 28 (4): 1- 7. doi: 10.3969/j.issn.1673-064X.2013.04.001
44	李北康, 胡作维, 李云, 等. 川中下寒武统龙王庙组白云岩阴极发光特征与成岩流体[J]. 石油地质与工程, 2016, 30 (2): 28- 31. doi: 10.3969/j.issn.1673-8217.2016.02.008
	Li Beikang , Hu Zuowei , Li Yun , et al. Cathodoluminescence characteristics and diagenetic fluids of dolomites in lower Cambrian Longwangmiao formation of central Sichuan basin[J]. Petroleum Geology and Engineering, 2016, 30 (2): 28- 31. doi: 10.3969/j.issn.1673-8217.2016.02.008
45	James R F , Aleden B C , Thomas W O . Cathodoluminescence and composition of calcite cement in the Taum Sauk limestone (upper Cambrian), Southeast Missouri[J]. Journal of Sedimentary Petrology, 1982, 52 (2): 0631- 0638.
46	Hiatt E E, Pufahl P K. Cathodoluminescence petrography of carbonate rocks: A review of application for understanding diagenesis, reservoir quality, and pore system evolution[R]. Mineralogical Association of Canada Short Course 45, Fredericton NB, May 2014, 75-96.
47	Friedman I, O'NeilJ R. Compilation of stable isotope fractionation factors of geological interest. In: Fleischer, M. (Ed. )[M]. Data of Geochemistry, 6thed. United States Geological Survey Professional Paper, 1977.
48	陈昭年. 黄骅坳陷千米桥潜山形成演化与油气成藏史[D]. 北京: 中国地质大学(北京), 2002.
	Chen Zhaonian. The formation and evolution of Qianmiqiao buried hills and their oil & gas accumulation history in Huanghua sub-basin[D]. Beijing: China University of Geosciences(Beijing), 2002.
49	蒋有录, 刘学嘉, 赵贤正, 等. 根据储层沥青和流体包裹体综合判识油气成藏期—以黄骅坳陷北大港古生界潜山为例[J]. 地球科学, 2020, 45 (3): 980- 988.
	Jiang Youlu , Liu Xujia , Zhao Xianzheng , et al. Comprehensive identification of oil and gas accumulation period by fluid inclusion technique and reservoirbitumen characteristics—A case study of the Paleozoic buried hill in Beidagang, Huanghua Depression[J]. Earth Science, 2020, 45 (3): 980- 988.
50	付立新, 陈善勇, 王丹丽, 等. 乌马营奥陶系潜山天然气藏特点及成藏过程[J]. 石油勘探与开发, 2002, 29 (5): 25- 27. doi: 10.3321/j.issn:1000-0747.2002.05.008
	Fu Lixin , Chen Shanyong , Wang Danli , et al. Natural gas pool in Ordovician reservoir in Wumaying buried –hill and its formation history[J]. Petroleum Exploration and Development, 2002, 29 (5): 25- 27. doi: 10.3321/j.issn:1000-0747.2002.05.008
51	朱光有, 张水昌, 梁英波, 等. TSR对深部碳酸盐岩储层的溶蚀改-四川盆地深部碳酸盐岩优质储层形成的重要方式[J]. 岩石学报, 2006, 22 (8): 2182- 2194.
	Zhu Guangyou , Zhang Shuichang , Liang Yingbo , et al. Dissolution and alteration of the deep carbonate reservoirs by TSR: an important type of deep-buried high-quality carbonate reservoirs in Sichuan basin[J]. Acta Petrologica Sinica, 2006, 22 (8): 2182- 2194.
52	朱光有, 张水昌, 梁英波, 等. 川东北地区飞仙关组高含H₂S天然气TSR成因的同位素证据[J]. 中国科学D辑: 地球科学, 2005, 35 (11): 1037.
	Zhu Guangyou , Zhang Shuichang , LiangYingbo , et al. Isotope evidence of TSR origin for nature gas bearing high H₂S content within Feixianguan formatiopn in northeastern Sichuan area[J]. Science in China Series D: Earth Sciences, 2005, 35 (11): 1037.
53	胡永嘉, 陆元庆, 梁学东, 等. 华南震旦、寒武系海相沉积成因重晶石的硫同位素组成及其在地质学上的意义[J]. 湖南地质, 1986, 5 (1): 51- 56.
	Hu Yongjia , Lu Yuanqing , Liang Xuedong , et al. Sulphur isotope composition of the marine sedimentary barite of Cambrian-Sinian system in south China and its signficance in geology[J]. Hunan Geology, 1986, 5 (1): 51- 56.
54	蔡春芳, 邬光辉, 李开开, 等. 塔中地区古生界热化学硫酸盐还原作用与原油中硫的成因[J]. 矿物岩石地球化学通报, 2007, 26 (1): 44- 48. doi: 10.3969/j.issn.1007-2802.2007.01.005
	Cai Chunfang , Wu Guanghui , Li Kaikai , et al. Thermochemical sulfate reduction and origin of sulfur in crude oils in Palaeozoic carbonates[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2007, 26 (1): 44- 48. doi: 10.3969/j.issn.1007-2802.2007.01.005
55	付立新, 吴雪松, 赵敏, 等. 歧口凹陷埕海潜山地质构造及奥陶系天然气成藏特点[J]. 东北石油大学学报, 2013, 37 (5): 63- 72. doi: 10.3969/j.issn.2095-4107.2013.05.009
	Fu Lixin , Wu Xuesong , Zhao Min , et al. Structural geology and gas accumulation in Ordovician reservoir in Chenghai buried-hill in Qikou sag[J]. Journal of Northeast Petroleum, 2013, 37 (5): 63- 72. doi: 10.3969/j.issn.2095-4107.2013.05.009

编号	井号	深度/m	潜山类型	产状	发光特征	δ¹⁸O(PDB)/‰	δ¹⁸O(W-SMOW)/‰	计算温度/℃
1	扣24	2 094.09	断块山	粒间	不发光	-6.04	0	46.03
2	歧古1	4 012.41	断块山	粒间	不发光	0.29	0	14.34
3	歧古1	4 195.70	断块山	粒间	不发光	-7.97	0	58.01
4	港古1-1	2 220.20	断块山	角砾间	不发光	-18.32	-12.00	48.12
5	港古1-1	2 220.20	断块山	角砾间	不发光	-17.64	-12.00	44.06
6	港古1-1	2 220.20	断块山	角砾间	不发光	-15.70	-12.00	33.35
7	港古1-1	2 220.20	断块山	角砾间	不发光	-16.64	-12.00	38.37
8	板深701	4 617.78	间断侵蚀断块山	脉体	不发光	-12.82	-8.00	39.32
9	板深701	4 617.78	间断侵蚀断块山	脉体	不发光	-13.01	-8.00	40.36
10	板深701	4 617.78	间断侵蚀断块山	脉体	不发光	-12.11	-8.00	35.43
11	板深701	4 617.78	间断侵蚀断块山	脉体	不发光	-11.75	-8.00	33.51
12	板深701	4 617.78	间断侵蚀断块山	脉体	不发光	-11.34	-8.00	31.40
13	板深701	4 622.80	间断侵蚀断块山	角砾间	不发光	-12.84	-8.00	39.37
14	板深701	4 622.80	间断侵蚀断块山	角砾间	不发光	-11.03	-8.00	29.78
15	板深701	4 648.00	间断侵蚀断块山	角砾间	不发光	-11.97	-8.00	34.69
16	板深701	4 648.00	间断侵蚀断块山	角砾间	不发光	-13.16	-8.00	41.21
17	板深701	4 648.40	间断侵蚀断块山	脉体	不发光	-13.56	-8.00	43.46
18	板深701	4 648.40	间断侵蚀断块山	脉体	不发光	-12.95	-8.00	40.01

[1]	丁文龙, 李云涛, 韩俊, 黄诚, 王来源, 孟庆修. 碳酸盐岩储层高精度构造应力场模拟与裂缝多参数分布预测方法及其应用[J]. 石油与天然气地质, 2024, 45(3): 827-851.
[2]	杨德彬, 鲁新便, 鲍典, 曹飞, 汪彦, 王明, 谢润成. 塔里木盆地北部奥陶系海相碳酸盐岩断溶体油藏成因类型及特征再认识[J]. 石油与天然气地质, 2024, 45(2): 357-366.
[3]	张赫驿, 杨帅, 张玺华, 彭瀚霖, 李乾, 陈聪, 高兆龙, 陈安清. 川东地区中二叠统茅口组沉积微相与环境演变[J]. 石油与天然气地质, 2024, 45(2): 457-470.
[4]	江同文, 邓兴梁, 曹鹏, 常少英. 塔里木盆地富满断控破碎体油藏储集类型特征与注水替油效果[J]. 石油与天然气地质, 2024, 45(2): 542-552.
[5]	屈海洲, 郭新宇, 徐伟, 李文皓, 唐松, 邓雅霓, 何仕鹏, 张云峰, 张兴宇. 碳酸盐岩微孔隙的分类、成因及对岩石物理性质的影响[J]. 石油与天然气地质, 2023, 44(5): 1102-1117.
[6]	周雁, 付斯一, 张涛, 陈洪德, 苏中堂, 张军涛, 张成弓, 刘子铭, 韩骁宇. 鄂尔多斯盆地下古生界构造-沉积演化、古地理重建及有利成藏区带划分[J]. 石油与天然气地质, 2023, 44(2): 264-275.
[7]	史今雄, 赵向原, 潘仁芳, 曾联波, 朱正平. 川中地区震旦系灯影组碳酸盐岩天然裂缝特征及其对气井产能影响[J]. 石油与天然气地质, 2023, 44(2): 393-405.
[8]	邹才能, 谢增业, 李剑, 张璐, 杨春龙, 崔会英, 王晓波, 郭泽清, 潘松圻. 典型碳酸盐岩大气田规模聚集差异性及其主控因素[J]. 石油与天然气地质, 2023, 44(1): 1-15.
[9]	张涛, 张亚雄, 金晓辉, 周雁, 张军涛, 谷宁, 张威, 王濡岳, 鲁锴. 鄂尔多斯盆地奥陶系马家沟组碳酸盐岩-蒸发岩层系层序地层模式及其对源-储的控制作用[J]. 石油与天然气地质, 2023, 44(1): 110-124.
[10]	刘建章, 蔡忠贤, 滕长宇, 张恒, 陈诚. 塔里木盆地顺北地区克拉通内走滑断裂带中-下奥陶统储集体方解石脉形成及其与油气充注耦合关系[J]. 石油与天然气地质, 2023, 44(1): 125-137.
[11]	何治亮, 赵向原, 张文彪, 吕心瑞, 朱东亚, 赵峦啸, 胡松, 郑文波, 刘彦锋, 丁茜, 段太忠, 胡向阳, 孙建芳, 耿建华. 深层-超深层碳酸盐岩储层精细地质建模技术进展与攻关方向[J]. 石油与天然气地质, 2023, 44(1): 16-33.
[12]	丁茜, 王静彬, 杨磊磊, 朱东亚, 江文滨, 何治亮. 基于模拟实验探讨断裂-流体-岩石体系中的矿物溶解-沉淀过程[J]. 石油与天然气地质, 2023, 44(1): 164-177.
[13]	李剑, 杨春龙, 谢武仁, 芮宇润, 王晓波, 张璐, 谢增业, 郭泽清. 四川盆地安岳气田震旦系台缘带和台内地区天然气成藏差异性及勘探领域[J]. 石油与天然气地质, 2023, 44(1): 34-45.
[14]	钱一雄, 武恒志, 周凌方, 董少峰, 王琼仙, 宋晓波, 邓美洲, 李勇. 深埋条件下微生物碳酸盐岩成岩作用与孔隙演化——以四川盆地西部中三叠统雷口坡组为例[J]. 石油与天然气地质, 2023, 44(1): 55-74.
[15]	吕心瑞, 邬兴威, 孙建芳, 夏东领, 李彦普, 丁炎志, 王斌. 深层碳酸盐岩储层溶洞垮塌物理模拟及分布预测[J]. 石油与天然气地质, 2022, 43(6): 1505-1514.

黄骅坳陷大港探区下古生界碳酸盐岩潜山差异演化及优质储层成因

Differential evolution and origin of high-quality reservoirs in the Lower Paleozoic carbonate buried hills in Dagang prospecting area, Huanghua Depression

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

图/表 11

参考文献 55

相关文章 15

编辑推荐

Metrics