珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比

doi:10.11743/ogg20140512

石油与天然气地质 ›› 2014, Vol. 35 ›› Issue (5): 670-678.doi: 10.11743/ogg20140512

珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比

易雪斐¹, 张昌民², 李少华², 杜家元^2,3, 罗明³, 李向阳⁴

1. 非常规油气湖北省协同创新中心, 湖北武汉 430100;
2. 长江大学油气资源与勘探技术教育部重点实验室, 湖北武汉 430100;
3. 中海石油(中国)有限公司深圳分公司, 广东广州 510240;
4. 河南省核工业地质局, 河南信阳 464000

收稿日期:2013-09-28 修回日期:2014-08-18 出版日期:2014-10-08 发布日期:2014-10-17
通讯作者: 张昌民（1963- ），男，博士生导师，沉积学和开发地质。
作者简介:易雪斐（1986- ），女，博士，沉积学和层序地层学。E-mail：xuefeiyi1986@163.com。
基金资助:
国家“十二五”重大专项（2011ZX05023-002）。

Comparison between shelf-margin delta of 21 Ma and 13.8 Ma in Pearl River Mouth Basin

Yi Xuefei¹, Zhang Changmin², Li Shaohua², Du Jiayuan^2,3, Luo Ming³, Li Xiangyang⁴

1. Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Wuhan, Hubei 430100, China;
2. Key Laboratory of Oil and Gas Resources and Exploration, Yangtze University, Wuhan, Hubei 430100, China;
3. Shenzhen Branch of CNOOC Ltd., Guangzhou, Guangdong 510240, China;
4. Nuclear Industry Geological Survey of Henan Province, Xinyang, Henan 464000, China

Received:2013-09-28 Revised:2014-08-18 Online:2014-10-08 Published:2014-10-17

摘要/Abstract

摘要：

陆架边缘三角洲是三角洲动态分类中一种比较重要的三角洲类型，已经成为科学研究和勘探开发的热点。根据驱动因素，可将陆架边缘三角洲分为物源供给驱动型和可容纳空间驱动型两类。珠江口盆地距今21 Ma和13.8 Ma时期具备发育陆架边缘三角洲的地质条件。通过对录井、测井曲线和地震资料的综合分析，从地形、相对海平面变化和沉积物供给三方面对21 Ma和13.8 Ma进行对比，对陆架边缘三角洲形成条件进行了分析，认为21 Ma时期为物源供给驱动型，而13.8 Ma时期为可容纳空间驱动型。虽然层序SQ2和SQ9在地形、相对海平面变化和沉积物供给三方面都存在较大差异，但它们都为典型的Ⅰ型层序，发育低位扇体、陆架边缘三角洲和三角洲前缘的滑塌体，均为稳定的陆架边缘三角洲。

关键词: 物源供给驱动型, 可容纳空间驱动型, 坡折, 陆架边缘三角洲, 珠江口盆地

Abstract:

Shelf-margin delta,an important type in the dynamic classification of delta,has become the focus of science researches and hot spot in oil & gas exploration.According to the driving factors,shelf-margin delta can be categorized into two types,namely sediment supply-driving delta and accommodation-driving delta.The Pearl River Mouth Basin had favorable geological condition for shelf-margin delta development at 21 Ma and 13.8 Ma.Shelf-margin deltas(21 Ma and 13.8 Ma)are analyzed in respects of topography,relative sea-level change and sediment supply through integration of well logging,logging curves and seismic data.The forming condition analysis shows that the delta at 21 Ma is of sediment supply-dri-ving type,while the delta at 13.8 Ma is of accommodation-driving type.Although SQ2 and SQ9 are obviously different in respects of topography,relative sea-level change and sediment supply,they both are type I sequences,and have well-developed lowstand fans,shelf-margin delta and delta-front slumping deposits,which belonging to stable shelf-margin deltas.

Key words: sediment supply-driving type, accommodation-driving type, slope break, shelf-margin delta, Pearl River Mouth Basin

中图分类号:

TE121.3

易雪斐,张昌民,李少华,等. 珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比[J]. 石油与天然气地质, 2014, 35(5): 670-678. doi: 10.11743/ogg20140512 Yi Xuefei,Zhang Changmin,Li Shaohua,et al. Comparison between shelf-margin delta of 21 Ma and 13.8 Ma in Pearl River Mouth Basin[J]. Oil & Gas Geology, 2014, 35(5): 670-678. doi: 10.11743/ogg20140512

参考文献

[1] Edwards M B.Upper wilcox rosita delta system of South Texas:Growth-faulted shelf-edge deltas[J].AAPG Bulletin, 1981, 65(1):54-73.
[2] Suter J R, Berryhill Jr H L.Late Quaternary shelf-margin deltas, northwest Gulf of Mexico[J].AAPG Bulletin, 1985, 69(1):77-91.
[3] Porebski S J, Steel R J.Delta types and sea level cycle[C]//AAPG Annual Convention June 3-6, Denver, Colorado, 2001, 12(10):160.
[4] Abdulah K C, Anderson J B, Snow J N, et al.The Late Quaternary Brazos and Colorado deltas, offshore Texas, USA:Their evolution and the factors that controlled their deposition[C]//Anderson J B, Fillon R H.Late Quaternary stratigraphic evolution of the northern Gulf of Mexico margin.SEPM Special Publication, 2004, 79:237-269.
[5] Anderson J B, Rodriguez A, Abdulah K C, et al.Late Quaternary stratigraphic evolution of the northern Gulf of Mexico margin:A synthesis[C]//Anderson J B, Fillon R H.Late Quaternary stratigraphic evolution of the northern Gulf of Mexico margin.SEPM Special Publication, 2004, 79:1-23.
[6] Roberts H H, Fillon R H, Kohl B, et al.Depositional architecture of the Lagniappe delta: Sediment characteristics, timing of depositional events, and temporal relationship with adjacent shelf-edge deltas[C]//Anderson J B, Fillon R H.Late Quaternary stratigraphic evolution of the northern Gulf of Mexico margin.SEPM Special Publication, 2004, 79:143-188.
[7] Wellner J S, Sarzalejo S, Lagoe M, et al.Late Quaternary stratigraphic evolution of the west Louisiana/east Texas continental shelf[C]//Anderson J B, Fillon R H.Late Quaternary stratigraphic evolution of the northern Gulf of Mexico margin.SEPM Special Publication, 2004, 79:217-235.
[8] Porebski S J, Steel R J.Shelf-margin deltas:Their stratigraphic signi-ficance and relation to deepwater sands[J].Earth-Science Reviews, 2003, 62:283-326.
[9] Grigoriy P, Janok P B.Pleistocene shelf-margin delta:Intradeltaic deformation and sediment bypass, northern Gulf of Mexico[J].AAPG Bulletin, 2011, 95(9):1617-1641.
[10] 陶维祥, 丁放, 何仕斌, 等.国外深水油气勘探述评及中国深水油气勘探前景[J].地质科技情报, 2006, 25(6):60-66. Tao Weixiang, Ding Fang, He Shibin, et al.Deepwater petroleum exploration abroad and deepwater petroleum exploration prospect of China[J].Geological Science and Technology Information, 2006, 25(6):60-66.
[11] 李大伟, 李德生, 陈长民, 等.深海扇油气勘探综述[J].中国海上油气, 2007, 19(1):18-24. Li Dawei, Li Desheng, Chen Changmin, et al.Summary of oil explorations in deep-sea fans[J].China Offshore Oil and Gas, 2007, 19(1):18-24.
[12] 何家雄, 夏斌, 施小斌, 等.世界深水油气勘探进展与南海深水油气勘探前景[J].天然气地球科学, 2006, 17(6):747-806. He Jiaxiong, Xia Bin, Shi Xiaobin, et al.Prospect and progress for oil and gas in deep waters of the world, and the potential and prospect forerground for oil and gas in deep waters of the South China Sea[J].Natural Gas Geoscience, 2006, 17(6):747-806.
[13] 吕福亮, 贺训云, 武金云, 等.世界深水油气勘探现状、发展趋势及对我国深水勘探的启示[J].石油地质, 2007, 6:28-31. Lv Fuliang, He Xunyun, Wu Jinyun, et al.Current situation and ten-dency of deepwater oil and gas exploraiton in the world[J].Petroleum Geology, 2007, 6:28-31.
[14] 武强, 解习农, 姜涛.陆架边缘三角洲的研究现状及其意义[J].海洋地质动态, 2005, 21(3):1-5. Wu Qiang, Xie Xinong, Jiang Tao.Study situation of shelf-margin delta and its significance[J].Marine Geology Letters, 2005, 21(3):1-5.
[15] 吴景富, 徐强, 祝彦贺.南海白云凹陷深水区渐新世—中新世陆架边缘三角洲形成及演化[J].地球科学——中国地质大学学报, 2010, 35(4):681-690. Wu Jingfu, Xu Qiang, Zhu Yanhe.Generation and evolution of the shelf-edge delta in Oligocene and Miocene of Baiyun sag in the South China Sea[J].Earth Science—Journal of China University of Geosciences, 2010, 35(4):681-690.
[16] 徐强, 王英民, 吕明, 等.陆架边缘三角洲在层序地层格架中的识别及其意义——以南海白云凹陷为例[J].石油与天然气地质, 2011, 32(54):733-742. Xu Qiang, Wang Yingmin, Lv Ming, et al.Identification of the shelf margin delta in sequence stratigraphic frameworks and its significance:A case study of the Baiyun sag, South China Sea[J].Oil & Gas Geology, 2011, 32(54):733-742.
[17] 王永凤, 王英民, 李冬, 等.陆架边缘三角洲沉积特征研究及其油气意义[J].海洋地质前沿, 2011, 27(7):28-33. Wang Yongfeng, Wang Yingmin, Li Dong, et al.Depositional characteristics of shelf-margin deltas and their petroleum significance[J].Marine Geology Frontiers, 2011, 27(7):28-33.
[18] 祝彦贺, 朱伟林, 徐强, 等.珠江口盆地13.8 Ma陆架边缘三角洲与陆坡深水扇的“源-汇”关系[J].中南大学学报(自然科学版), 2011, 42(12):3827-3834. Zhu Yanhe, Zhu Weilin, Xu Qiang, et al.Sedimentary response to shelf-edge delta and slope deep-water fanin 13.8 Ma of Miocene epoch in Pearl River Mouth Basin[J].Journal of Central South University(Science and Technology Edition), 2011, 42(12):3827-3834.
[19] 易雪斐, 张昌民, 李少华, 等.珠江口盆地NSQ2陆架边缘三角洲的识别标志及沉积模式[J].成都理工大学学报(自然科学版), 2012, 39(3):257-261. Yi Xuefei, Zhang Changmin, Li Shaohua, et al.Identification marks and depositional model of the shelf-margin delta from NSQ2 of the Pearl River Mouth basin, China[J].Journal of Chengdou University of Technology(Science & Technology Edition), 2012, 39 (3):257-261.
[20] 周祖翼.珠江口盆地的形成与南海的构造演化[J].海洋科学, 1993, 5:62-66. Zhou Zuyi.Basement structure and tectonic evolution of the Pearl River Mouth Basin[J].Marine Sciences, 1993, 5:62-66.
[21] 崔莎莎, 何家雄, 陈胜红, 等.珠江口盆地发育演化特征及其油气成藏地质条件[J].天然气地球科学, 2009, 20(3):384-391. Cui Shasha, He Jiaxiong, Chen Shenghong, et al.Development cha-racteristics of Pearl River Mouth basin and its geological conditions for oil and gas accumulation[J].Natural Gas Geoscience, 2009, 20(3):384-391.
[22] 钟建强.珠江口盆地的构造特征与盆地演化[J].海洋湖沼通报, 1994, (1):1-8. Zhong Jianqiang.Chracteristics of geologic structure and basin evolution in Pearl River Mouth Basin[J].Transaction of Oceanology and Limnology, 1994, (1):1-8.
[23] 邵磊, 雷永昌, 庞雄, 等.珠江口盆地构造演化及对沉积环境的控制作用[J].同济大学学报(自然科学版), 2005, 33(9):1177-1181. Shao Lei, Lei Yongchang, Pang Xiong, et al.Tectonic evolution and its controlling for sedimentary environment in Pearl River Mouth Basin[J].Journal of Tongji University, 2005, 33(9):1177-1181.
[24] 侯国伟, 于兴河, 客伟利, 等.番禺低隆起东区中新世早-中期沉积演化特征[J].石油天然气学报(江汉石油学院学报), 2005, 27(1):26-28. Hou Weiguo, Yu Xinghe, Ke Weili, et al.Sedimentary evolution cha-racteristics of Early-Mid Miocene in the eastern of Panyu Uplift[J].Journal of Oil and Gas Technology, 2005, 27(1):26-28.
[25] 许仕策, 杨少坤, 黄丽芬.层序地层学在地层对比中的应用[J].地学前缘, 1995, 2 (3/4):115-123. Xu Shice, Yang Shaokun, Huang Lifen.The application of sequence stratigraphy to stratigraphic correlation[J].Earth Science Frontiers, 1995, 2(3/4):115-123.
[26] 秦国权.珠江口盆地新生代晚期层序地层划分和海平面变化[J].中国海上油气(地质), 2002, 16(1):1-18. Qin Guoquan.Late Cenozoic sequence stratigraphy and sea-level changes inPearl River Mouth Basin, South China Sea[J].China Offshore Oil and Gas(Geology), 2002, 16(1):1-18.
[27] 董伟, 林畅松, 秦成岗, 等.珠江口盆地番禺低隆起韩江组高精度层序格架和沉积样式与岩性地层圈闭的发育分布[J].现代地质, 2008, 22(5):794-802. Dong Wei, Lin Changsong, Qin Chenggang, et al.High resolution sequence framework, depositional pattern and litho-stratigraphic traps of Hanjiang Formation in Panyu Uplift, Pearl River Mouth Basin[J].Geoscience, 2008, 22(5):794-802.
[28] 李向阳, 张昌民, 张尚锋, 等.珠江口盆地新近系层序划分与发育模式[J].石油天然气学报, 2012, 34(4):47-51. Li Xiangyang, Zhang Changmin, Zhang Shangfen, et al.Neogene sequence subdivision and its development pattern in Pearl River Mouth Basin[J].Journal of Oil and Gas Technology, 2012, 34(4):47-51.
[29] 庞雄, 陈长民, 邵磊, 等.白云运动:南海北部渐新统—中新统重大地质事件及其意义[J].地质论评, 2007, 53(2):145-151. Pang Xiong, Chen Changmin, Shao Lei, et al.Baiyun movement, a great tectonic event on the Oligocene-Miocene boundary in the nor-thern South China Sea and its implications[J].Geological Review, 2007, 53 (2):145-151.
[30] 柳保军, 庞雄, 颜承志, 等.珠江口盆地白云深水区渐新世—中新世陆架坡折带演化及油气勘探意义[J].石油学报, 2011, 32(2):234-242. Liu Baojun, Pang Xiong, Yan Chengzhi, et al.Evolution of the Oligocene-Miocene shelf slope-break zone in the Baiyun deep-waterarea of the Pearl River Mouth Basin and its significance in oil-gas exploration[J].Acta Petrolei Sinica, 2011, 32(2):234-242.
[31] 杨少坤, 黄丽芬, 李希, 等.珠江口盆地特殊层序地层模式及其对勘探的指导意义[J].中国海上油气(地质), 1996, 10(3):137-152. Yang Shaokun, Huang Lifeng, Li Xi, et al.Special sequential stratigraphic pattern in the Pearl River Mouth Basin and its significance to exploration[J].China Offshore Oil and Gas(Geology), 1996, 10(3):137-152.
[32] 李坦, 殷小舟.地震属性的地质意义分析[J].复杂油气藏, 2009, 3(2):25-28. Li Tan, Yin Xiaozhou.Analysis on the geological significance of seismic attributes[J].Complex Hydrocarbon Reservoirs, 2009, 3(2):25-28.
[33] 王小杰, 印兴耀, 吴国忱.基于S变换的吸收衰减技术在含气储层预测中的应用研究[J].石油物探, 2012, 51(1):37-42. Wang Xiaojie, Yin Xingyao, Wu Guochen.The application of an S transform based absorption and attenuation technique for prediction of gas-bearing reservoir[J].Geophysical Prospecting for Petroleum, 2012, 51(1):37-42.
[34] 黄鸿光, 陆永潮, 邹卓超.琼东南盆地松南三维区台缘礁地震沉积学研究[J].石油实验地质, 2012, 34(1):25-29. Huang Hongguang, Lu Yongchao, Zou Zhuochao.Application of seismic sedimentology in platform edge reef, Songnan 3D area, Qiongdongnan Basin[J].Petroleum Geology & Experiment, 2012, 34(1):25-29.
[35] 梁国胜, 陈清棠, 王淑玉, 等.地震综合解释技术在构造岩性油气藏勘探中的应用[J].断块油气田, 2011, 18(1):47-50, 69. Liang Guosheng, Chen Qingtang, Wang Shuyu, et al. Application of comprehensive seismic interpretation technology in exploration of structural-lithological reservoir[J]. Fault-Block Oil & Gas Field, 2011, 18(1):47-50, 69.
[36] 张兆辉, 苏明军, 刘化清, 等.精细地震层序地层分析技术及应用——以渤海湾盆地歧口凹陷滨海地区为例[J].石油实验地质, 2012, 34(6):648-652. Zhang Zhaohui, Su Mingjun, Liu Huaqing, et al.High precision ana-lysis technology of seismic sequence strata and its application:A case study of Binhai region in Qikou Sag, Bohai Bay Basin[J].Petroleum Geology & Experiment, 2012, 34(6):648-652.

珠江口盆地21Ma和13.8Ma陆架边缘三角洲对比

Comparison between shelf-margin delta of 21 Ma and 13.8 Ma in Pearl River Mouth Basin

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