北卡那封盆地沉积演化规律与烃源岩发育特征

doi:10.11885/j.issn.16745086.2016.04.07.01

西南石油大学学报(自然科学版) ›› 2017, Vol. 39 ›› Issue (5): 81-91.DOI: 10.11885/j.issn.16745086.2016.04.07.01

北卡那封盆地沉积演化规律与烃源岩发育特征

杨婷¹, 康洪全¹, 刘东旭², 李欣¹, 赵忠英³

1. 中海油研究总院, 北京朝阳 100028;
2. 中国石油天然气股份有限公司对外合作经理部, 北京东城 100007;
3. 中国石油勘探开发研究院, 北京海淀 100083

收稿日期:2016-04-07 出版日期:2017-10-01 发布日期:2017-10-01
作者简介:杨婷,1983年生,女,汉族,黑龙江哈尔滨人,工程师,博士,主要从事沉积学、储层地质学和油气地质综合研究。E-mail:yangting1983@139.com;康洪全,1969年生,男,汉族,河北三河人,高级工程师,主要从事综合油气地质勘探研究。E-mail:kanghq@cnooc.com.cn;刘东旭,1984年生,女,汉族,黑龙江绥化人,工程师,硕士,主要从事对外合作项目技术业务管理工作。E-mail:liudongxu84@petrochina.com.cn;李欣,1982年生,男,汉族,山西襄汾人,工程师,博士,主要从事地震资料解释和储层预测研究。E-mail:lixin11@cnooc.com.cn;赵忠英,1982年生,女,汉族,辽宁抚顺人,工程师,博士,主要从事岩性地层油气藏及非常规油气地质研究。E-mail:zhaozhongying@petrochina.com.cn
基金资助:
国家科技重大专项（2011ZX05030-001）

The Sedimentary Facies Evolution and the Development Characteristics of Source Rocks' in North Carnarvon Basin, Australia

YANG Ting¹, KANG Hongquan¹, LIU Dongxu², LI Xin¹, ZHAO Zhongying³

1. CNOOC Research Institute, Chaoyang, Beijing 100028, China;
2. PetroChina Foreign Cooperation Administration Department, Dongcheng, Beijing 100007, China;
3. Petrochina Research Institute of Petroleum Exploration & Development, Haidian, Beijing 100083, China

Received:2016-04-07 Online:2017-10-01 Published:2017-10-01
Contact: 杨婷,E-mail:yangting1983@139.com

摘要/Abstract

摘要： 以研究澳大利亚北卡那封盆地中生代沉积环境与烃源岩特征的关系为目的，根据盆地内400余口钻井及分析测试资料，首次系统开展了盆地中生代沉积演化规律研究，评价了北卡那封盆地有效烃源岩发育特征，深入探讨了沉积环境对烃源岩有机质发育的影响。研究认为，受构造活动的影响，北卡那封盆地中生代沉积格局发生多次转变：晚三叠世发育大型三角洲沉积，侏罗纪为隆拗相间的浅海、局限海沉积，早白垩世局部发育三角洲-海底扇沉积，晚白垩世为开阔海、半深海-深海沉积。盆地中生代发育两套优质烃源岩：上三叠统Mungaroo组三角洲平原沼泽环境倾气型烃源岩和上侏罗统Dingo组局限海环境倾油型烃源岩，其中Mungaroo组倾气型烃源岩为盆地主要的供烃层系。

关键词: 北卡那封盆地, 中生代, 沉积演化, 烃源岩, 三角洲, 局限海

Abstract: The main purpose of this study was to investigate the relationship between the Mesozoic sedimentary environment and the characteristics of the source rocks of the North Carnarvon Basin in Australia. Employing information gleaned from more than 400 drilling wells and the test data of the basin, the Mesozoic sedimentary evolution of the basin was characterized for the first time. In addition, the characteristics of the development of the source rock were evaluated, and the influence of the sedimentary environment on hydrocarbon development in the source rock is discussed. The research shows that the sedimentary pattern in the Mesozoic transformed the North Carnarvon Basin several times, e.g., in the Late Triassic, a large sedimentary delta developed; in the Jurassic, a concave and convex shallow sea developed, with restricted marine deposition; in the Early Cretaceous, fan delta-submarine fan delta sedimentary deposits developed locally; and, in the Late Cretaceous, an open sea developed, with bathyal-abyssal sea deposition. In the Mesozoic, two high-quality source rocks developed, including gas-type source rocks in the Mungaroo Group delta-plain swamp environment during the Upper Triassic, and oil-type source rocks in the restricted marine environment of the Dingo Group during the Upper Jurassic. The gas-type source rock of the Mungaroo Group is the source of hydrocarbon generation in the basin.

Key words: North Carnarvon Basin, Mesozoic, sedimentary evolution, source rocks, delta, restricted marine

中图分类号:

TE122

杨婷, 康洪全, 刘东旭, 李欣, 赵忠英. 北卡那封盆地沉积演化规律与烃源岩发育特征[J]. 西南石油大学学报(自然科学版), 2017, 39(5): 81-91.

YANG Ting, KANG Hongquan, LIU Dongxu, LI Xin, ZHAO Zhongying. The Sedimentary Facies Evolution and the Development Characteristics of Source Rocks' in North Carnarvon Basin, Australia[J]. 西南石油大学学报(自然科学版), 2017, 39(5): 81-91.

0
/ / 推荐

导出引用管理器 EndNote|Ris|BibTeX

链接本文: http://journal15.magtechjournal.com/Jwk_xnzk/CN/10.11885/j.issn.16745086.2016.04.07.01

http://journal15.magtechjournal.com/Jwk_xnzk/CN/Y2017/V39/I5/81

参考文献

[1] 张林晔,孔祥星,张春荣,等. 济阳坳陷下第三系优质烃源岩的发育及其意义[J]. 地球化学, 2003, 32(1):3542. doi:10.3321/j.issn:0379-1726.2003.01.005 ZHANG Linye, KONG Xiangxing, ZHANG Chunrong, et al. High-quality oil-prone source rocks in Jiyang Depression[J]. Geochimica, 2003, 32(1):35-42. doi:10.3321/j.-issn:0379-1726.2003.01.005
[2] 胡利民. 大河控制性影响下的陆架海沉积有机质的"源汇"作用——以渤、黄海为例[D]. 青岛:中国海洋大学, 2010. HU Limin. Sources and sinks of sedimentary organic matter in the river-dominated continental shelves:A case study in the Bohai and Yellow Seas[D]. Qingdao:Ocean University of China, 2010.
[3] 腾格尔. 海相地层元素、碳氧同位素分布与沉积环境和烃源岩发育关系——以鄂尔多斯盆地为例[D]. 兰州:中国科学院研究生院(兰州地质研究所), 2004. TENGER. The distribution of elements, carbon and oxygen isotopes on marine strata and environmental correlation between they and hydrocarbon source rocks formation:An example from Ordovician Basin, China[D]. Lanzhou:Lanzhou Institute of Geology, Chinese Academy of Science, 2004.
[4] 刘玉虎,赵丹丹,刘兴旺,等. 吐哈侏罗纪原型盆地演化对烃源岩分布的控制[J]. 西南石油大学学报(自然科学版),2012,34(4):2939. doi:10.3863/j.issn.1674-5086.2012.04.004 LIU Yuhu, ZHAO Dandan, LIU Xingwang, et al. The evolution of Turpan-Hami Jurassic Prototype Basin and its control on the distribution of source rocks[J]. Journal of Southwest Petroleum University(Science & Technology Edition), 2012, 34(4):29-39. doi:10.3863/j.issn.1674-5086.2012.04.004
[5] 邓运华. 论河流与油气的共生关系[J]. 石油学报,2010, 31(1):1217. doi:10.7623/syxb201001002 DENG Yunhua. Analysis on correlation of river and petroleum[J]. Acta Petrolei Sinica, 2010, 31(1):12-17. doi:10.7623/syxb201001002
[6] 白国平,殷进垠. 澳大利亚北卡那封盆地油气地质特征及勘探潜力分析[J]. 石油实验地质, 2007, 29(3):253258. doi:10.3969/j.issn.1001-6112.2007.03.006 BAI Guoping, YIN Jinyin. Petroleum geological features and exploration potential analyses of north Carnavon Basin, Australia[J]. Petroleum Geology & Experiment, 2007, 29(3):253-258. doi:10.3969/j.issn.1001-6112.2007.03.006
[7] 张建球,钱桂华,郭念发. 澳大利亚大型沉积盆地与油气成藏[M]. 北京:石油工业出版社, 2008. ZHANG Jianqiu, QIAN Guihua, GUO Nianfa. Large sedimentary basins and hydrocarbon reservoir formation, Australia[M]. Beijing:Petroleum Industry Press, 2008.
[8] METCALFE I. Palaeozoic and Mesozoic tectonic evolution and palaeogeography of East Asian crustal fragments:The Korean Peninsula in context[J]. Gondwana Research, 2006, 9(1/2):24-46. doi:10.1016/j.gr.2005.04.002
[9] VEEVERS J J. Updated Gondwana (Permian-Cretaceous) earth history of Australia[J]. Gondwana Research, 2006, 9(3):231-260. doi:10.1016/j.gr.2005.11.005
[10] JABLONSKI D, SAITTA A J. Permian to lower cretaceous plate tectonics and its impact on the Tectonostratigraphic development of the western Australian margin[J]. The APPEA Journal, 2004, 44(1):287-328.
[11] 许晓明,胡孝林,赵汝敏,等. 澳大利亚北卡那封盆地中上三叠统Mungaroo组油气勘探潜力分析[J]. 地质科技情报, 2014, 33(6):119127. XU Xiaoming, HU Xiaolin, ZHAO Rumin, et al. Exploration potential of Triassic Mungaroo Formation, North Carnarvon Basin, Australia[J]. Geological Science and Technology Information, 2014, 33(6):119-127.
[12] SCOTESE C R, BOUCOT A J, MCKERROW W S. Gondwanan palaeogeography and palaeoclimatology[J]. Journal of African Earth Sciences, 1999, 28(1):99-114. doi:10.1016/S0899-5362(98)00084-0
[13] GRICE K, BACKHOUSE J, ALEXANDER R, et al. Correlating terrestrial signatures from biomarker distributions,δ¹³C, and palynology in fluvio-deltaic deposits from NW Australia (Triassic-Jurassic)[J]. Organic Geochemistry, 2005, 36(10):1347-1358. doi:10.1016/j.orggeochem.-2005.06.003
[14] BURATTI N, CIRILLI S. Microfloristic provincialism in the upper Triassic Circum-Mediterranean area and palaeogeographic implication[J]. Geobios, 2007, 40(2):133-142. doi:10.1016/j.geobios.2006.06.003
[15] STEPHENSON A E, BLEVIN J E, WEST B G. The paleogeography of the Beagle Sub-basin, Northern Carnarvon Basin, Australia[J]. Journal of Sedimentary Research, 1998, 68(6):1131-1145. doi:10.2110/jsr.68.1131
[16] CATHRO D L, KARNER G D. Cretaceous-Tertiary inversion history of the Dampier Sub-basin, northwest Australia:Insights from quantitative basin modeling[J]. Marine and Petroleum Geology, 2006, 23(4):503-526. doi:10.1016/j.marpetgeo.2006.02.005
[17] LANGHI L, BOREL G D. Influence of the Neotethys rifting on the development of the Dampier Sub-basin(North West Shelf of Australia), highlighted by subsidence modelling[J]. Tectonophysics, 2005, 397(1/2):93-111. doi:10.1016/j.tecto.2004.10.005
[18] SMYTH M, MASTALERZ M. Organic petrological composition of Triassic source rocks and their clastic depositional environments in some Australian sedimentary basins[J]. International Journal of Coal Geology, 1991, 18(3/4):165-186. doi:10.1016/0166-5162(91)90049-O
[19] 牛杏,王任,杨香华,等. North Carnarvon盆地中-上三叠统沉积特征与有机质的空间展布[J]. 石油地质与工程,2012,26(56):1519. doi:10.3969/j.issn.1673-8217.2012.06.004 NIU Xing, WANG Ren, YANG Xianghua, et al. Sedimentary characteristics and the spatial distribution of organic matter of Middle-Late Triassic in North Carnarvon Basin[J]. Petroleum Geology and Engineering, 2012, 26(56):15-19. doi:10.3969/j.issn.1673-8217.2012.06.-004
[20] 李丹,杨香华,常吟善,等. 澳大利亚北卡那封盆地中上三叠统Mungaroo三角洲陆源有机质分布特征[J]. 古地理学报, 2014, 16(2):193204. doi:10.7605/gdlxb.-2014.02.018 LI Dan, YANG Xianghua, CHANG Yinshan, et al. Distribution of the Upper Triassic terrigenous organic matter in Mungaroo delta of North Carnarvon Basin, Australia[J]. Journal of Palaeogeography, 2014, 16(2):193-204. doi:10.7605/gdlxb.2014.02.018
[21] 宋来亮,刘华,徐昊清,等. 潍北凹陷孔店组烃源岩地化特征及油源对比[J]. 西南石油大学学报(自然科学版), 2016, 38(2):110. doi:10.11885/j.issn.1674-5086.2014.03.02.02 SONG Lailiang,LIU Hua,XU Haoqing,et al. Geochemical characteristics of hydrocarbon source rocks and oilsource correlation of Kongdian Formation, Weibei Depression[J]. Journal of Southwest Petroleum University(Science & Technology Edition), 2016, 38(2):1-10. doi:10.11885/j.issn.1674-5086.2014.03.02.02

北卡那封盆地沉积演化规律与烃源岩发育特征

The Sedimentary Facies Evolution and the Development Characteristics of Source Rocks' in North Carnarvon Basin, Australia

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	罗川, 杨虎. 论构造应力不是油气初次运移的主要动力[J]. 西南石油大学学报(自然科学版), 2020, 42(4): 104-110.
[2]	牟中海, 刘雪, 常琳, 苏秋, 吴千然. 薄互层型沉积体储层构型建模[J]. 西南石油大学学报(自然科学版), 2020, 42(3): 1-12.
[3]	夏世强, 林畅松, 杜晓峰, 李俊乾, 李虹. 辽东湾北部东营组同沉积断裂对沉积充填控制[J]. 西南石油大学学报(自然科学版), 2020, 42(1): 19-32.
[4]	赵汉卿, 郭诚, 陈晓明, 刘超, 张博. 垦利A油田辫状河三角洲前缘优质储层特征[J]. 西南石油大学学报(自然科学版), 2019, 41(5): 21-32.
[5]	刘建华, 汪利兵, 赵靖康, 张俊, 孟云涛. PL油田浅水辫状河三角洲隔夹层精细表征方法[J]. 西南石油大学学报(自然科学版), 2019, 41(5): 10-20.
[6]	夏志远, 李森明, 庞皓, 李文研. 咸化湖盆过渡相组沉积控储作用浅析[J]. 西南石油大学学报(自然科学版), 2019, 41(4): 12-22.
[7]	杨希冰, 金秋月, 胡林, 胡德胜. 北部湾盆地涠西南凹陷原油成因类型及分布特征[J]. 西南石油大学学报(自然科学版), 2019, 41(3): 51-60.
[8]	吴穹螈, 陈晓明, 赵汉卿, 张言辉, 曹龙. 分流砂坝型浅水三角洲储层构型研究[J]. 西南石油大学学报(自然科学版), 2019, 41(2): 53-63.
[9]	黄华. 江汉盐湖盆地油气形成与运聚特征[J]. 西南石油大学学报(自然科学版), 2018, 40(6): 69-76.
[10]	陈筱, 卜范青, 王昊, 陈国宁, 张旭. 西非深水浊积复合水道储层连通模式表征[J]. 西南石油大学学报(自然科学版), 2018, 40(6): 35-46.
[11]	邱争科, 王辉, 李婷, 陶武龙, 蒲波. 准噶尔盆地八道湾组湿地扇三角洲沉积特征[J]. 西南石油大学学报(自然科学版), 2018, 40(5): 47-58.
[12]	沈卫兵, 陈践发, 罗广平, 贺礼文. 塔中隆起奥陶系储层与油源断裂复合控藏模式[J]. 西南石油大学学报(自然科学版), 2018, 40(5): 71-83.
[13]	许磊, 王宗俊, 王盘根, 商志垒, 郭晓. 准噶尔盆地东缘J₁b¹扇三角洲沉积特征研究[J]. 西南石油大学学报(自然科学版), 2018, 40(4): 9-16.
[14]	贾怀存, 康洪全, 李明刚, 程涛, 孟金落. 大陆边缘三角洲盆地油气成藏特征类比研究[J]. 西南石油大学学报(自然科学版), 2018, 40(3): 34-42.
[15]	刘忠亮, 张成富, 李清辰, 刘军, 安海玲. 东濮凹陷西南部晚古生代-早新生代烃源研究[J]. 西南石油大学学报(自然科学版), 2018, 40(2): 35-45.