Characteristics and Exploration Direction of the Cambrian Shilongdong Formation Reservoir in Yichang and Surrounding Areas
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摘要:
宜昌地区寒武系页岩气的勘探发现表明该区域可能蕴藏巨大的油气资源潜力,寒武系石龙洞组上覆覃家庙组膏岩盖层使其成为常规油气勘探的重要层位。本文通过宜昌及周边的钻井岩心、薄片观察描述,物性、碳氧同位素等测试,对石龙洞组储层及控制因素做了研究。结果表明宜昌及周边地区石龙洞组储层主要形成于局限台地环境,储层岩性以细晶云岩、砂屑白云岩为主,孔隙度平均值为5.2%,渗透率平均值为8.638×10−3 μm2,孔隙类型以晶间溶孔和晶间孔为主。石龙洞组形成于温暖或炎热的亚热带环境,控制储层发育的主要因素有沉积相、白云岩化、溶蚀作用和构造裂缝。震旦纪-寒武纪之交古隆起控制了石龙洞组优质储层分布,同时也是油气运移的指向区。古隆起边缘烃源岩生烃时间晚,油气扩散时间短、保存条件相对有利。因此叠合石龙洞组储层、覃家庙组盖层、圈闭、构造保存条件等因素,宜昌地区围绕石龙洞组天然气勘探的有利区位于黄陵隆起东南缘-当阳复向斜一带。
Abstract:The exploration and discovery of Cambrian shale gas in the Yichang area indicates enormous potential for oil and gas resources. The Cambrian Shilongdong Formation, overlaid with the Qinjiamiao Formation gypsum rock cap, has become an important layer for conventional oil and gas exploration. This study has researched the reservoir and controlling factors of the Shilongdong Formation through observations and descriptions of drilling cores from Yichang and its surrounding areas, combined with the information on rock thin sections, physical properties, carbon and oxygen isotopes. The results indicate that the Shilongdong Formation reservoir in Yichang and surrounding areas was mainly formed in a confined platform environment. The reservoir lithology is dominantly fine crystalline dolomite and granular dolomite, with an average porosity of 5.2% and an average permeability of 8.638×10−3 μm2. The pore type is mainly dissolution pores. The Shilongdong Formation was formed in a warm or hot subtropical environment, and the main factors controlling reservoir development include sedimentary facies, dolomitization, dissolution, and structural fractures. The ancient uplift at the turn of the Cambrian and Cambrian periods controlled the distribution of high-quality reservoirs in the Shilongdong Formation and also served as a directional zone for oil and gas migration. The hydrocarbon generation time of the ancient uplift edge source rocks is late, the oil and gas diffusion time is short, and the preservation conditions are relatively favorable. Therefore, the favorable area for natural gas exploration of the Shilongdong Formation in the Yichang area is located in the southeast edge of the Huangling Uplift- Dangyang Syncline, due to factors such as the reservoir of the Shilongdong Formation, the cap rock of the Qinjiamiao Formation, traps, and structural preservation conditions.
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[1] 陈 科,翟刚毅,包书景,宋 腾,林 拓,李浩涵,金春爽,孟凡洋,唐显春,张焱林.2020.华南黄陵隆起构造演化及其对页岩气保存的控制作用[J]. 中国地质,47(1):161-172. doi: 10.12029/gc20200113
[2] 杜金虎,邹才能,徐春春,何海清,沈 平,杨跃明,李亚林,魏国齐,汪泽成,杨 雨.2014.川中古隆起龙王庙组特大型气田战略发现与理论技术创新[J]. 石油勘探与开发,41(3):268-277. doi: 10.11698/PED.2014.03.02
[3] 冯菊芳,林娟华,田海芹,沃玉进,朱东亚.2016.湘鄂西地区下寒武统石龙洞组古岩溶发育及储层特征[J]. 科技导报,34(2):121-128.
[4] 冯增昭.2004.单因素分析多因素综合作图法:定量岩相古地理重建[J]. 古地理学报,6(1):3-19. doi: 10.3969/j.issn.1671-1505.2004.01.002
[5] 郭战峰,刘新民,盛贤才,马登峰.2009.东秦岭—大别造山带南侧加里东期古隆起特征及油气地质意义[J]. 石油实验地质,31(2):181-185. doi: 10.3969/j.issn.1001-6112.2009.02.012
[6] 韩 波,何治亮,任娜娜,田海芹,马 强.2018.四川盆地东缘龙王庙组碳酸盐岩储层特征及主控因素[J]. 岩性油气藏,30(1):75-85. doi: 10.3969/j.issn.1673-8926.2018.01.008
[7] 何幼斌,蒋 蕾,顾志翔,罗慈航,张欣茹.2023.重庆石柱-彭水地区下寒武统石龙洞组沉积特征[J]. 长江大学学报(自然科学版),20(11):1-12.
[8] 金之钧,龙胜祥,周 雁,沃玉进,肖开华,杨志强,殷进垠.2006.中国南方膏盐岩分布特征[J]. 石油与天然气地质,27(5):571-584. doi: 10.3321/j.issn:0253-9985.2006.05.001
[9] 李熙喆,郭振华,万玉金,刘晓华,张满郎,谢武仁,苏云河,胡 勇,冯建伟,杨炳秀,马石玉,高树生.2017.安岳气田龙王庙组气藏地质特征与开发技术政策[J]. 石油勘探与开发,44(3):398-406. doi: 10.11698/PED.2017.03.09
[10] 李智武,冉 波,肖 斌,宋金民,郑 玲,李金玺,王 瀚,肖 斌,叶胡豪,蔡其新,刘树根.2019.四川盆地北缘震旦纪—早寒武世隆-坳格局及其油气勘探意义[J]. 地学前缘,26(1):59-85.
[11] 刘 安,陈孝红,李培军,周 鹏,李 海,蔡全升,罗胜元.2020.宜昌天阳坪断裂两侧页岩气保存条件对比研究[J]. 地质科技通报,39(2):10-19.
[12] 刘少峰,王 平,胡明卿,郜瑭郡,王 凯.2010.中、上扬子北部盆-山系统演化与动力学机制[J]. 地学前缘,17(3):14-26.
[13] 梅廉夫,刘昭茜,汤济广,沈传波,凡元芳.2010.湘鄂西-川东中生代陆内递进扩展变形:来自裂变径迹和平衡剖面的证据[J]. 地球科学,35(2):161-174.
[14] 任 影,钟大康,高崇龙,孙海涛,孟 昊,胡小林,姜振昌,王 爱.2015.川东及其周缘地区下寒武统龙王庙组储集层特征与控制因素[J]. 古地理学报,17(6):829-840. doi: 10.7605/gdlxb.2015.06.068
[15] 任 影,钟大康,高崇龙,杨雪琪,李海洋,杨 强,刘云龙,王 玉.2016.四川盆地东部下寒武统龙王庙组碳、氧同位素组成及古环境意义[J]. 海相油气地质,21(4):11-20. doi: 10.3969/j.issn.1672-9854.2016.04.002
[16] 邵龙义.1994.碳酸盐岩氧、碳同位素与古温度等的关系[J]. 中国矿业大学学报,23(1):39-45.
[17] 盛贤才,郭战峰,冯 畅,胡晓凤,包汉勇.2015.鄂西渝东地区下寒武统石龙洞组成岩作用特征[J]. 特种油气藏,22(4):4-7. doi: 10.3969/j.issn.1006-6535.2015.04.002
[18] 谢环羽,姜在兴,王培玺,谢武仁,杨 雨.2021.中—上扬子地区寒武系层序地层格架[J]. 石油学报,42(7):865-884. doi: 10.7623/syxb202107004
[19] 曾雄伟,王传尚,刘 安,危 凯.2016.湖北宜昌地区中寒武统天河板组沉积相及其油气意义[J]. 华南地质与矿产,32(2):142-148.
[20] 赵玉茹,高 达,胡明毅,郑 超,李 佳,谢武仁.2024.古气候和海平面变化对浅水碳酸盐岩高频层序及有利储层的控制—以川中地区龙王庙组为例[J]. 中国地质,51(2):577-591. doi: 10.12029/gc20210809001
[21] 赵宗举,朱 琰,邓红婴,徐云俊.2003.中国南方古隆起对中、古生界原生油气藏的控制作用[J]. 石油实验地质,25(1):1-9.
[22] 邹 辰,周松源,梅 珏,邵萌珠,秦 颦,余鑫培.2016.湖北当阳复向斜北部页岩气地质评价与有利区优选[J]. 海相油气地质,21(2):22-28. doi: 10.3969/j.issn.1672-9854.2016.02.003
[23] Epstein S, Mayeda T K. 1953. Variation of O18 content of waters from natural sources[J]. Geochimica et Cosmochimica Acta, 4(5): 213-224. doi: 10.1016/0016-7037(53)90051-9
[24] Keith M H, Weber J N. 1964. Carbon and oxygen isotopic composition of selected limestones and fossils[J]. Geochimica et Cosmochimica Acta, 28: 1787-1816. doi: 10.1016/0016-7037(64)90022-5
[25] Shen C B, Mei L F, Peng L, Chen Y Z, Yang Z, Hong G F. 2012. LA-ICPMS U-Pb zircon age constraints on the provenance of Cretaceous sediments in the Yichang area of the Jianghan Basin, central China[J]. Cretacous Research, 34: 172-183. doi: 10.1016/j.cretres.2011.10.016
[26] Wilson J L. 1975. Carbonate facies in geological history[M]. New York: Springer-Verlag.
[27] Zhu M Y, Yang A H, Yuan J L, Li G X, Zhang J M, Zhao F C, Ahn S Y, Miao L Y. 2019. Cambrian integrative stratigraphy and timescale of China[J]. Science China: Earth Sciences, 62: 25-60. doi: 10.1007/s11430-017-9291-0
[28] Zhu M Y, Zhang J M, Li G X, Yang A H. 2004. Evolution of C isotopes in the Cambrian of China: implications for Cambrian subdivision and trilobite mass extinctions-zhu maoyan[J]. Geobios, 37: 287-301. doi: 10.1016/j.geobios.2003.06.001
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