TYPES AND DISTRIBUTION PATTERN OF SALT RELATED TRAPS IN THE SURESTE BASIN, MEXICO
-
摘要:
Sureste盆地位于墨西哥湾南部,为系统研究该区盐相关圈闭。基于第1手的地质、钻井、油田和地球物理资料,从盆地构造演化阶段、沉积充填特征、盐岩活动期次出发,系统分析了圈闭成因、发育特征、空间展布规律。结合盆地勘探程度指出,Comalcalco次盆东部侏罗—白垩系盐核背斜圈闭和Reforma褶皱带中北部牛津阶和基末利阶盐核背斜圈闭、伸展盐筏断块圈闭为最有潜力勘探目标,为该盆地盐上勘探目标的优选提供了科学依据。
Abstract:The Sureste Basin is located in the southern Gulf of Mexico and there is little discussion on this basin in literatures. In order to systematically study the salt related traps in this area, geologic, drilling, field and seismic data are used to systematically analyze the features, origins and spatial distribution patterns based upon basin tectonic evolution, sedimentary features and salt movement stages. In combination of exploration status, it is concluded that the Jurassic and Cretaceous anticline with salt cores in the Comalcalco Sub-bain are the most favorable prospecting target and the Salt core anticline, tensional salt draft fault block in the Oxfordian and Kimmeridgian Formations in the North of Reforma belt are the second. The study result is helpful for optimization of the exploration targets in post salt stratum of Mexico Sureste Basin.
-
Key words:
- salt related trap /
- trap type /
- distribution discipline /
- Sureste Basin /
- Mexico
-
[1] Valois C. A new approach of Tertiary plays in a multidisciplinary framework: Sureste Basin, Tabasco, Mexico[C]. Cancun: AAPG International Conference, 2004.
[2] 韩彧, 黄娟, 赵雯.墨西哥湾盆地深水区油气分布特征及勘探潜力[J].石油实验地质, 2015, 37(4):473-478. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sysydz201504010
[3] 周浩伟, 于水, 卢景美, 等.墨西哥Sureste盆地油气成藏模式[J].特种油气藏, 2016, 23(4):55-59. doi: 10.3969/j.issn.1006-6535.2016.04.012
[4] 郑民, 贾承造, 李建忠, 等.全球被动陆缘深水勘探领域富油气特征及与我国南海被动陆缘深水区对比[J].地质科技情报, 2010, 29(6):45-53. doi: 10.3969/j.issn.1000-7849.2010.06.008
[5] 罗群, 王崇孝, 唐敏, 等.不规则地质体隐蔽圈闭识别模式与关键技术应用尝试——以扇体圈闭为例[J].岩性油气藏, 2013, 25(6):30-34. doi: 10.3969/j.issn.1673-8926.2013.06.006
[6] 王威, 李臻, 田敏, 等.岩性-地层油气藏勘探方法技术研究现状及进展[J].岩性油气藏, 2009, 21(2):121-125. doi: 10.3969/j.issn.1673-8926.2009.02.026
[7] 李双林, 张生银.墨西哥及墨西哥湾盆地构造单元及其演化[J].海洋地质动态, 2010, 26(3):14-21.
[8] 史丹妮, 杨双.滨里海盆地盐岩运动及相关圈闭类型[J].岩性油气藏, 2007, 19(3):73-79. doi: 10.3969/j.issn.1673-8926.2007.03.013
[9] Mauduit T, Guerin G, Brun J P, et al. Raft tectonics: the effects of basal slope angle and sedimentation rate on progressive extension[J]. Journal of Structural Geology, 1997, 19(9): 1219-1230. doi: 10.1016/S0191-8141(97)00037-0
[10] 王芝尧, 苏俊青, 钱茂路, 等.断块区岩相古地理对岩性油气藏形成的影响——以歧口凹陷滨海斜坡区古近纪为例[J].天然气勘探与开发, 2010, 24(6):5-10. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqktykf201102002
[11] 杨占龙, 张正刚, 陈启林, 等.利用地震信息评价陆相盆地岩性圈闭的关键点分析[J].岩性油气藏, 2007, 19(4):57-63. doi: 10.3969/j.issn.1673-8926.2007.04.010
[12] 李德生.滚动背斜油气田[J].石油实验地质, 1980(2):1-8. doi: 10.11781/sysydz198002001
[13] Mitra S, Gonzalez J A, Garcia J H, et al. Ek-Balam field: A structure related to multiple stages of salt tectonics and extension[J].AAPG Bulletin, 2007, 91(11): 1619-1636. doi: 10.1306/06260706112
[14] 李涛, 胡望水, 何瑶瑶, 等.下刚果盆地重力滑脱构造发育特征及演化规律[J].大地构造与成矿学, 2012, 36(2):197-203. doi: 10.3969/j.issn.1001-1552.2012.02.006
[15] 胡望水, 李涛, 于水, 等.西非被动大陆边缘重力滑脱构造发育演化及成因机制[J].大地构造与成矿学, 2012, 36(2):186-196. doi: 10.3969/j.issn.1001-1552.2012.02.005
[16] 关利群, 屈红军, 张功成, 等.世界主要深水盆地圈闭特征[J].海洋地质与第四纪地质, 2010, 30(4):209-214. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201004025
[17] 岳建华, 康志宏, 韩燕英.新疆塔里木盆地艾协克-桑塔木油气区带圈闭类型及空间组合规律[J].石油实验地质, 1999, 21(4):316-319. doi: 10.3969/j.issn.1001-6112.1999.04.007
[18] 耿玉海, 李江海.塔里木盆地塔北隆起西部圈闭类型、分布及空间组合规律[J].北京大学学报:自然科学版, 2008, 44(2):193-200.doi:10.3321/j.issn:0479-8023.2008.02.005.
[19] 刘琼, 陶维祥, 于水, 等.西非下刚果—刚果扇盆地圈闭类型和分布特征[J].地质科技情报, 2013, 32(3):107-112. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201303017