Characteristics and main controlling factors of the limy source rock gas reservoir in the first member of the Middle Permian Maokou Formation in the southern Sichuan and western Chongqing area: a case study of well DB 1
-
摘要: 四川盆地中二叠统茅口组是天然气的重要产层，近期浙江油田分公司在渝西大安探区DB1井茅一段“眼皮眼球”灰岩的灰质源岩气储层中，直井试气获得42 000 m3/d、水平井(DB1H井)试气初产55.6×104 m3/d以上的工业气流，实现了蜀南—渝西泥质灰岩非常规天然气勘探突破，展示了该区良好的勘探前景。四川盆地茅一段眼皮眼球灰岩具有自生自储特征，连续稳定展布，且热演化成熟度高，中缓坡相带纯灰岩不具有水敏和酸敏特性，以碳酸盐脆性矿物为主，易于酸化压力开发，因此开展富有机质灰岩储层特征及主控因素研究意义重大。以DB1井为例，研究茅一段岩石学、沉积学及储层特征，发现沉积于水体较震荡、生物发育的中缓坡相带、主体为深灰—灰黑色富有机质的泥晶灰岩储层物性较好，总体上茅一c亚段好于茅一a亚段，眼皮灰岩大孔发育程度高于眼球灰岩，微孔发育程度差别不大。茅一段主要储集空间类型有溶蚀孔、裂缝、黏土矿物孔缝和有机质孔，黏土矿物(主要是滑石)和有机质内的孔隙主要分布于眼皮灰岩中；沉积过程与成岩作用是控制茅一段眼皮、眼球灰岩储层发育的主要因素，中缓坡沉积相带控制了富有机质纯泥晶生屑灰岩储层的发育特征和区域展布，成岩作用和断裂、断溶作用影响灰岩储层储集性能的改善，并成为富集高产的主因。渝西DB1井区“黑茅口”富有机质的茅一段直井、水平井突破商业气流获得稳定高产，表明茅一段灰质源岩气成藏赋存条件好，具有自生自储为主+局部构造带短距离聚集的2种成藏模式以及气藏连续型展布、资源规模大的特征，茅一段灰质源岩气“连续型气藏”勘探潜力大，将成为四川盆地重要的潜在勘探新层系。Abstract: The Middle Permian Maokou Formation in the Sichuan Basin is an important natural gas payzone. Recently, Zhejiang Oilfield Company of CNPC obtained industrial gas flow of vertical well test 42×103 m3/d and horizontal well (well DB 1H) test 556×103 m3/d in the limy source rock gas reservoir of eyelid and eyeball- shaped limestone in the first member of the Maokou Formation in well DB 1, Da'an exploration area, western Chongqing. A breakthrough has been made in the unconventional gas exploration of argillaceous limestone in the southern Sichuan and western Chongqing area, showing good exploration prospects in this area. The eyelid and eyeball-shaped limestone in the first member of the Maokou Formation in the Sichuan Basin has the characteristics of self-generation and self-storage, continuous and stable distribution and high thermal maturity. The limestone of central gentle slope facies shows no water sensitivity or acid sensitivity, and is dominated by carbonate brittle minerals, which is ideal for acid-fracturing development. It is of great significance to study the characteristics and main controlling factors of the organic rich limestone reservoir. Taking well DB 1 as an example, this paper carried out a study on the petrology, sedimentology and reservoir characteristics of the first member of the Maokou Formation, and it is found that, deposited on the central gentle slope with frequent water activity and abundant organism, the dark gray to black micrite with high organic matter content has good physical properties. In general, submember c has better physical properties than submember a. The development degree of macropores in eyelid-shaped limestone is higher than that in eyeball-shaped limestone, and the development degree of micropores is not much different. The main pore types of the first member of the Maokou Formation include dissolution pores, fractures, clay mineral apertures and organic pores. The pores in clay minerals (mainly talc) and organic matters are mainly distributed in the eyelid-shaped limestone. Depositional process and diagenesis are the main factors controlling the development of the eyelid and eyeball-shaped limestone reservoirs. The central gentle slope facies controls the development and distribution features of the organic-rich micrites. Diagenesis as well as fracture and dissolution effects improve the reservoir capacity of limestone, which is critical for hydrocarbon accumulation. Stable and high yield commercial gas flow was obtained in the vertical wells and horizontal wells in the first member of the Maokou Formation which has high organic matter content in well DB 1 block in the western Chongqing area, indicating that the accumulation and occurrence conditions of limestone source rock gas are good in the first member of the Maokou Formation. It has two kinds of accumulation modes with self-generation and self-storage dominance and short distance aggregation of local structural bands, and has the characteristics of continuous distribution of gas reservoir and large resource scale. The "continuous gas reservoir: in the limestone source rock in the first member of the Maokou Formation has great exploration potential, which will become an important exploration target with good potential in the Sichuan Basin.
-
图 1 四川盆地构造分区及DB1井位置
Figure 1. Structural sketch map of Sichuan Basin and location of well DB 1
图 2 蜀南—渝西地区DB1井中二叠统茅口组岩性、测井评价综合柱状图
Figure 2. Comprehensive histograms showing lithology and logging evaluation of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
图 3 蜀南—渝西地区DB1井中二叠统茅口组一段典型岩石类型的岩心和显微薄片照片
a.DB1井茅一段眼皮、眼球灰岩；b.泥晶灰岩，2 527.14 m (眼球灰岩)；c.含生屑泥质灰岩，2 527.71 m(眼皮灰岩)；d.泥晶灰岩，2 517.70 m (眼球灰岩)；e.生屑泥质灰岩，2 517.45 m(眼皮灰岩)；f.灰质云岩，2 727.13 m；g.灰质云岩，2 727.84 m。
Figure 3. Cores and micro-photos of typical rocks in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
图 4 蜀南—渝西地区DB1井中二叠统茅口组一段储集空间类型
a.2 723.73 m，眼皮灰岩，黄色箭头为溶蚀孔，茜素红染色，单偏光；b.2 725.26 m，眼球灰岩，黄色箭头为溶蚀孔，铸体薄片，正交偏光；c.2 729.19 m，眼球灰岩，黄色箭头指示生屑溶蚀孔，铸体薄片，单偏光；d.2 680.95 m，滑石中生屑溶蚀孔，单偏光；e-f.2 522.08~2 522.38 m，裂缝主要发育于眼球灰岩中，且多被方解石充填。
Figure 4. Typical reservoir space types in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
图 5 蜀南—渝西地区DB1井中二叠统茅口组一段与滑石和有机质相关的微孔特征
a.滑石晶格缝(2 718.15 m)；b.滑石与方解石之间的粒缘缝(2 718.15 m)；c.滑石交代生屑(2 728.88 m)；d.滑石交代生屑，与石英共生(2 727.81 m)；e.黄色箭头为滑石，红色箭头为萤石(2 517.45 m)；f.有机质孔(2 718.15 m)。
Figure 5. Micropore characteristics associated with talc and organic matter in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
图 6 蜀南—渝西地区DB1井中二叠统茅口组一段眼皮、眼球灰岩孔隙度分布
Figure 6. Porosity distribution of eyelid and eyeball-shaped limestone in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
图 7 蜀南—渝西地区DB1井中二叠统茅口组一段孔隙结构CT图
a-d.分别为眼皮灰岩(2 525.38 m)的xy、yz、xz以及三维岩心提取的孔隙图；e-h.分别为眼球灰岩(2 528.3 m)的xy、yz、xz以及三维岩心提取的孔隙图。
Figure 7. CT photos of pore structures in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
图 8 蜀南—渝西地区DB1井中二叠统茅口组一段眼皮、眼球灰岩孔径分布
Figure 8. Pore size distribution of eyelid and eyeball-shaped limestone in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
图 9 蜀南—渝西地区DB1井中二叠统茅口组一段眼皮灰岩和眼球灰岩孔喉模型
a.2 525.38 m眼皮灰岩喉道分布；b-c.2 525.38 m眼皮灰岩孔喉网络模型(球为孔隙，棍为喉道)；d.2 528.3 m眼球灰岩喉道分布；e-f.2 528.3 m眼球灰岩孔喉网络模型(球为孔隙，棍为喉道)。
Figure 9. Pore throat models of eyelid and eyeball-shaped limestone in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
表 1 蜀南—渝西地区DB1井中二叠统茅口组一段眼皮、眼球灰岩微孔、孔喉参数
Table 1. Micro-pore and pore throat parameters of eyelid and eyeball-shaped limestone in first member of Middle Permian Maokou Formation in well DB 1 in southern Sichuan and western Chongqing area
项目 茅口组一段样品 眼皮灰岩(2 525.38 m) 眼球灰岩(2 528.3 m) 孔隙 表面积/μm2 平均：4 108.89 平均：5 453.15 最小：768.78 最小：768.78 最大：2.55×107 最大：4.32×107 中间值：1 442.69 中间值：1 441.28 体积/μm3 平均：34 337.07 平均：46 319.06 最小：4 093.69 最小：4 093.69 最大：3.15×108 最大：4.98×108 中间值：8 181.71 中间值：8 174.52 直径/μm 平均：28.66 平均：29.76 最小：19.84 最小：19.84 最大：844.35 最大：983.73 中间值：24.99 中间值：24.99 喉道 长度/μm 最小：18.3 最小：16.96 最大：706.89 最大：588.79 体积/μm3 最小：3 678.74 最小：3 410.33 最大：1.78×105 最大：4.39×105 直径/μm 最小：15.98 最小：15.98 最大：42.64 最大：55.08 
下载: 导出CSV
-
[1] 何文渊, 蒙启安, 印长海, 等. 四川盆地合川—潼南地区栖霞组白云岩天然气地质特征及有利勘探区带[J]. 大庆石油地质与开发, 2022, 41(4): 1-11. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK202204001.htmCHE Wenyuan, MENG Qi'an, YIN Changhai, et al. Geological characteristics and favorable exploration plays of gas in Qixia Formation dolomite in Hechuan-Tongnan area of Sichuan Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2022, 41(4): 1-11. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK202204001.htm [2] 郝毅, 姚倩颖, 田瀚, 等. 四川盆地二叠系茅口组沉积特征及储层主控因素[J]. 海相油气地质, 2020, 25(3): 202-209. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ202003002.htmHAO Yi, YAO Qianying, TIAN Han, et al. Sedimentary characteristics and reservoir-controlling factors of the Permian Maokou Formation in Sichuan Basin[J]. Marine Origin Petroleum Geology, 2020, 25(3): 202-209. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ202003002.htm [3] 张培先, 何希鹏, 高全芳, 等. 四川盆地东南缘二叠系茅口组一段页岩气藏地质特征及富集模式[J]. 石油与天然气地质, 2021, 42(1): 146-157. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202101014.htmZHANG Peixian, HE Xipeng, GAO Quanfang, et al. Geological characteristics and enrichment pattern of Permian Mao 1 member shale gas reservoirs at the southeastern margin of Sichuan Basin[J]. Oil & Gas Geology, 2021, 42(1): 146-157. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202101014.htm [4] 谢继容, 李亚, 杨跃明, 等. 川西地区二叠系火山碎屑岩规模储层发育主控因素与天然气勘探潜力[J]. 天然气工业, 2021, 41(3): 48-57. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202103008.htmXIE Jirong, LI Ya, YANG Yueming, et al. Main controlling factors and natural gas exploration potential of Permian scale volcano clastic reservoirs in the western Sichuan Basin[J]. Natural Gas Industry, 2021, 41(3): 48-57. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202103008.htm [5] 杨跃明, 张少敏, 金涛, 等. 川南地区二叠系龙潭组页岩储层特征及勘探潜力[J]. 岩性油气藏, 2023, 35(1): 1-11. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX202301001.htmYANG Yueming, ZHANG Shaomin, JIN Tao, et al. Characteristics and exploration potential of shale reservoirs of Permian Longtan Formation in southern Sichuan Basin[J]. Lithologic Reservoirs, 2023, 35(1): 1-11. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX202301001.htm [6] 杨雨, 谢继容, 赵路子, 等. 四川盆地茅口组滩相孔隙型白云岩储层天然气勘探的突破及启示: 以川中北部地区JT1井天然气立体勘探为例[J]. 天然气工业, 2021, 41(2): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202102002.htmYANG Yu, XIE Jirong, ZHAO Luzi, et al. Breakthrough of natural gas exploration in the beach facies porous dolomite reservoir of Middle Permian Maokou Formation in the Sichuan Basin and its enlightenment: a case study of the tridimensional exploration of well JT1 in the central-northern Sichuan Basin[J]. Natural Gas Industry, 2021, 41(2): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202102002.htm [7] 焦方正, 杨雨, 冉崎, 等. 四川盆地中部地区走滑断层的分布与天然气勘探[J]. 天然气工业, 2021, 41(8): 92-101. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202108013.htmJIAO Fangzheng, YANG Yu, RAN Qi, et al. Distribution and gas exploration of the strike-slip faults in the central Sichuan Basin[J]. Natural Gas Industry, 2021, 41(8): 92-101. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202108013.htm [8] 吴亚军, 刘莉萍, 代平, 等. 四川盆地元坝二叠系长兴组气藏气水分布特征及水侵早期识别[J]. 海相油气地质, 2021, 26(3): 245-252. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ202103006.htmWU Yajun, LIU Liping, DAI Ping, et al. Gas-water distribution characteristics and early identification of water invasion of Permian Changxing Formation gas reservoir in Yuanba, Sichuan Basin[J]. Marine Origin Petroleum Geology, 2021, 26(3): 245-252. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ202103006.htm [9] 段文燊, 王同, 张南希. 四川盆地威远构造带发现二叠系梁山组页岩气[J]. 中国地质, 2021, 48(4): 1298-1299. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202104028.htmDUAN Wenshen, WANG Tong, ZHANG Nanxi. New discovery of shale gas in Permian Liangshan Formation in the Weiyuan tectonic zone Sichuan Basin[J]. Geology in China, 2021, 48(4): 1298-1299. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202104028.htm [10] 张宇, 曹清古, 罗开平, 等. 四川盆地二叠系茅口组油气藏勘探发现与启示[J]. 石油与天然气地质, 2022, 43(3): 610-620. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202203010.htmZHANG Yu, CAO Qinggu, LUO Kaiping, et al. Reservoir exploration of the Permian Maokou Formation in the Sichuan Basin and enlightenment obtained[J]. Oil & Gas Geology, 2022, 43(3): 610-620. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202203010.htm [11] 姜智利, 朱祥. 四川盆地元坝地区二叠系茅口组油气成藏特征及主控因素[J]. 石油实验地质, 2022, 44(4): 639-646. doi: 10.11781/sysydz202204639JIANG Zhili, ZHU Xiang. Hydrocarbon accumulation characte-ristics and main controlling factors for Permian Maokou Formation in Yuanba area, Sichuan Basin[J]. Petroleum Geology & Experiment, 2022, 44(4): 639-646. doi: 10.11781/sysydz202204639 [12] 郭彤楼. 四川盆地碳酸盐岩源岩气地质特征与勘探前景[J]. 西南石油大学学报(自然科学版), 2021, 43(1): 1-16. https://www.cnki.com.cn/Article/CJFDTOTAL-XNSY202101001.htmGUO Tonglou. Geological characteristics and exploration prospect of carbonate source rock gas in Sichuan Basin[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2021, 43(1): 1-16. https://www.cnki.com.cn/Article/CJFDTOTAL-XNSY202101001.htm [13] 颜佳新. 华南地区二叠纪栖霞组碳酸盐岩成因研究及其地质意义[J]. 沉积学报, 2004, 22(4): 579-587. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200404004.htmYAN Jiaxin. Origin of Permian Chihsian carbonates from South China and its geological implications[J]. Acta Sedimentologica Sinica, 2004, 22(4): 579-587. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200404004.htm [14] 包汉勇, 马仲武, 胡超涌, 等. 武汉地区二叠系栖霞组灰岩—含泥灰岩韵律层生物产率[J]. 地质科技情报, 2009, 28(2): 60-65. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200902010.htmBAO Hanyong, MA Zhongwu, HU Chaoyong, et al. Productivity of limestone-marl rhythms of Permain Chihsia Formation in Wuhan[J]. Geological Science and Technology Information, 2009, 28(2): 60-65. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200902010.htm [15] 罗进雄, 何幼斌, 何明薇, 等. 华南中二叠统眼球状石灰岩特征及成因的思考[J]. 古地理学报, 2019, 21(4): 613-626. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201904007.htmLUO Jinxiong, HE Youbin, HE Mingwei, et al. Thoughts on characteristics and origin of the Middle Permian eyeball-shaped limestone in South China[J]. Journal of Palaeogeography, 2019, 21(4): 613-626. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201904007.htm [16] MUNNECKE A, WESTPHAL H, KÖLBL-EBERT M. Diagenesis of plattenkalk: examples from the Solnhofen area (Upper Jurassic, southern Germany)[J]. Sedimentology, 2008, 55(6): 1931-1946. [17] WESTPHAL H, MUNNECKE A, PROSS J, et al. Multiproxy approach to understanding the origin of Cretaceous pelagic limestone-marl alternations (DSDP site 391, Blake-Bahama Basin)[J]. Sedimento-logy, 2004, 51(1): 109-126. [18] WESTPHAL H. Limestone–marl alternations as environmental archives and the role of early diagenesis: a critical review[J]. International Journal of Earth Sciences, 2006, 95(6): 947-961. [19] WESTPHAL H, HILGEN F, MUNNECKE A. An assessment of the suitability of individual rhythmic carbonate successions for astrochronological application[J]. Earth-Science Reviews, 2010, 99(1/2): 19-30. [20] PANG Qang, HU Guang, ZHANG Xihua, et al. Organic geochemistry, sedimentary environment, and organic matter enrichment of limestone-marlstone rhythms in the middle Permian northern Sichuan Basin, China[J]. Marine and Petroleum Geology, 2021, 134: 105306. [21] 胡东风, 王良军, 张汉荣, 等. 碳酸盐岩烃源岩气藏的发现及其油气地质意义: 以四川盆地涪陵地区中二叠统茅口组一段气藏为例[J]. 天然气工业, 2020, 40(7): 23-33. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202007005.htmHU Dongfeng, WANG Liangjun, ZHANG Hanrong, et al. Discovery of carbonate source rock gas reservoir and its petroleum geological implications: a case study of the gas reservoir in the first member of Middle Permian Maokou Formation in the Fuling area, Sichuan Basin[J]. Natural Gas Industry, 2020, 40(7): 23-33. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202007005.htm [22] LIU Xianfeng, LI Jie, CAI Zhongxian, et al. Contribution of clay on storage and adsorption capacities of the Middle Permian marls, South China[J]. Journal of Petroleum Science and Engineering, 2021, 207: 109193. [23] 韩月卿, 李双建, 韩文彪, 等. 川东南地区中二叠统茅口组灰泥灰岩储层孔隙特征[J]. 石油实验地质, 2022, 44(4): 666-676. doi: 10.11781/sysydz202204666HAN Yueqing, LI Shuangjian, HAN Wenbiao, et al. Pore characte-ristics of marl reservoir in Maokou Formation of Middle Permian, southeastern Sichuan Basin[J]. Petroleum Geology & Experiment, 2022, 44(4): 666-676. doi: 10.11781/sysydz202204666 [24] 谢知含, 侯宇, 雷开强, 等. XC地区茅口组岩溶储层发育有利区预测[J]. 断块油气田, 2021, 28(2): 230-234. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202102016.htmXIE Zhihan, HOU Yu, LEI Kaiqiang, et al. Prediction of favorable development area of Maokou Formation karst reservoir in XC area[J]. Fault-Block Oil and Gas Field, 2021, 28(2): 230-234. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202102016.htm [25] 范建平, 宋金民, 江青春, 等. 川东地区中二叠统茅口组一段储层特征与形成模式[J]. 石油与天然气地质, 2022, 43(6): 1413-1430. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202206011.htmFAN Jianping, SONG jinmin, JIANG Qingchun, et al. Reservoir characteristics and development model of the Middle Permian Mao-1 Member in eastern Sichuan Basin[J]. Oil & Gas Geology, 2022, 43(6): 1413-1430. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202206011.htm [26] 夏威, 蔡潇, 丁安徐, 等. 南川地区栖霞—茅口组碳酸盐岩储集空间研究[J]. 油气藏评价与开发, 2021, 11(2): 197-203. https://www.cnki.com.cn/Article/CJFDTOTAL-KTDQ202102008.htmXIA Wei, CAI Xiao, DING Anxu, et al. Reservoir spaces of carbo-nate rocks in Qixia-Maokou Formation of Nanchuan area[J]. Reservoir Evaluation and Development, 2021, 11(2): 197-203. https://www.cnki.com.cn/Article/CJFDTOTAL-KTDQ202102008.htm [27] 杨柳, 巫芙蓉, 郭鸿喜, 等. 川南YJ向斜区茅口组储层地震预测与主控因素分析[J]. 断块油气田, 2021, 28(3): 363-368. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202103015.htmYANG Liu, WU Furong, GUO Hongxi, et al. Reservoir seismic prediction and main controlling factors analysis of Maokou Formationin YJ Syncline area, South Sichuan Basin[J]. Fault-Block Oil and Gas Field, 2021, 28(3): 363-368. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202103015.htm [28] 姚威, 许锦, 夏文谦, 等. 四川盆地涪陵地区茅一段酸解气、吸附气特征及气源对比[J]. 天然气工业, 2019, 39(6): 45-50. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201906008.htmYAO Wei, XU Jin, XIA Wenqian, et al. A characteristic analysis between acidolysis gas and absorbed gas and its application to gas-source correlation in Mao 1 member, Fuling area, Sichuan Basin[J]. Natural Gas Industry, 2019, 39(6): 45-50. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201906008.htm [29] 江青春, 汪泽成, 苏旺, 等. 四川盆地中二叠统茅口组一段泥灰岩源内非常规天然气成藏条件及有利勘探方向[J]. 中国石油勘探, 2021, 26(6): 82-97. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY202106006.htmJIANG Qingchun, WANG Zecheng, SU Wang, et al. Accumulation conditions and favorable exploration orientation of unconventional natural gas in the marl source rock of the first member of the Middle Permian Maokou Formation, Sichuan Basin[J]. China Petroleum Exploration, 2021, 26(6): 82-97. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY202106006.htm [30] 刘喜停, 颜佳新, 薛武强. 灰岩—泥灰岩韵律层的差异成岩作用[J]. 地质论评, 2012, 58(4): 627-635. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201204003.htmLIU Xiting, YAN Jiaxin, XUE Wuqiang. Differential diagenesis of limestone-marl alternations[J]. Geological Review, 2012, 58(4): 627-635. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201204003.htm [31] 刘喜停, 颜佳新, 马志鑫, 等. 华南栖霞组灰岩—泥灰岩韵律层的成因[J]. 地球科学(中国地质大学学报), 2014, 39(2): 155-164. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201402003.htmLIU Xiting, YAN Jiaxin, MA Zhixin, et al. Origination of limestone-marl alternations from Qixia Formation of South China[J]. Earth Science(Journal of China University of Geosciences), 2014, 39(2): 155-164. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201402003.htm [32] 罗进雄, 何幼斌. 中—上扬子地区二叠系眼球状石灰岩特征及成因研究[J]. 地质论评, 2010, 56(5): 629-637. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201005005.htmLUO Jinxiong, HE Youbin. Origin and characteristics of Permian eyeball-shaped limestones in middle-upper Yangtze region[J]. Geological Review, 2010, 56(5): 629-637. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201005005.htm [33] 田小彬, 师江波, 董景海, 等. 川中地区茅口组一段沉积相新认识: 基于最新钻井资料[J]. 天然气地球科学, 2021, 32(11): 1646-1655. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202111005.htmTIAN Xiaobin, SHI Jiangbo, DONG Jinghai, et al. New understanding of sedimentary facies of the first member of Maokou Formation based on the latest drilling in central Sichuan Basin[J]. Natural Gas Geoscience, 2021, 32(11): 1646-1655. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202111005.htm [34] 李昂, 罗开平, 李风勋, 等. 眼球状灰岩成因及其油气地质意义[J]. 石油实验地质, 2021, 43(3): 452-460. doi: 10.11781/sysydz202103452LI Ang, LUO Kaiping, LI Fengxun, et al. Origin of eyeball-shaped limestone and its significance for petroleum geology[J]. Petroleum Geology & Experiment, 2021, 43(3): 452-460. doi: 10.11781/sysydz202103452 [35] 韩月卿, 郝运轻, 韩文彪, 等. 川东南地区中二叠统茅口组一段眼球状灰岩成因机理[J]. 油气地质与采收率, 2022, 29(6): 12-21. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS202206002.htmHAN Yueqing, HAO Yunqing, HAN Wenbiao, et al. Genetic mechanism of eyeball-shaped limestone in First Member of Middle Permian Maokou Formation in southeast Sichuan Basin[J]. Petroleum Geology and Recovery Efficiency, 2022, 29(6): 12-21. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS202206002.htm [36] 雷涵. 四川盆地茅口组一段眼球—眼皮状石灰岩成因及储层微观特征[D]. 北京: 中国地质大学(北京), 2021.LEI Han. Genesis and reservoir microscopic characteristics of eyelid-eyeball-shaped limestone in the 1st member of Maokou Formation, Sichuan Basin[D]. Beijing: China University of Geosciences (Beijing), 2021. [37] 赵培荣. 焦石坝地区茅一段储层特征及天然气勘探潜力[J]. 油气藏评价与开发, 2021, 11(5): 772-781. https://www.cnki.com.cn/Article/CJFDTOTAL-KTDQ202105016.htmZHAO Peirong. Reservoir characteristics and gas exploration potential of Permian Mao-1 member of Maokou Formation in Jiaoshiba area[J]. Petroleum Reservoir Evaluation and Development, 2021, 11(5): 772-781. https://www.cnki.com.cn/Article/CJFDTOTAL-KTDQ202105016.htm [38] 任海侠, 林小兵, 刘叶, 等. 川西南二叠系茅口组一段滑石特征及其形成机理: 以A1井茅一段样品为例[J]. 石油实验地质, 2021, 43(6): 1038-1047. doi: 10.11781/sysydz2021061038REN Haixia, LIN Xiaobing, LIU Ye, et al. Characteristics and formation mechanism of talc in Permian Maokou Formation, southwestern Sichuan Basin: a case study of first member of Maokou Formation in well A[J]. Petroleum Geology & Experiment, 2021, 43(6): 1038-1047. doi: 10.11781/sysydz2021061038 [39] 李蓉, 苏成鹏, 石国山, 等. 川南地区二叠系茅口组一段瘤状灰岩储层成因[J]. 天然气地球科学, 2021, 32(6): 806-815. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202106003.htmLI Rong, SU Chengpeng, SHI Guoshan, et al. The genesis of nodular limestone reservoirs of the first period of Maokou Formation of Permian in southern Sichuan Basin[J]. Natural Gas Geoscience, 2021, 32(6): 806-815. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202106003.htm -
点击查看大图
图(9) / 表(1)
计量
- 文章访问数: 118
- HTML全文浏览量: 49
- PDF下载量: 40
- 被引次数: 0
苏公网安备32021102000780号