THE SEQUENCE STRATIGRAPHY OF HUANGLIU FORMATION AND THE INTERNAL STRUCTURES OF SUBMARINE FAN IN DONGFANG AREA,YINGGEHAI BASIN

ZHONG Zehong; ZHANG Yingzhao; HE Xiaohu; XU Tao; REN Jianye; LIU Xiaoyan; LING Tao; HAN Guangming

doi:10.3724/SP.J.1140.2015.02091

2015 Vol. 35, No. 2

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Article navigation > Marine Geology & Quaternary Geology > 2015 > 35(2): 91-99

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ZHONG Zehong, ZHANG Yingzhao, HE Xiaohu, XU Tao, REN Jianye, LIU Xiaoyan, LING Tao, HAN Guangming. THE SEQUENCE STRATIGRAPHY OF HUANGLIU FORMATION AND THE INTERNAL STRUCTURES OF SUBMARINE FAN IN DONGFANG AREA,YINGGEHAI BASIN[J]. Marine Geology & Quaternary Geology, 2015, 35(2): 91-99. doi: 10.3724/SP.J.1140.2015.02091

Citation:

ZHONG Zehong, ZHANG Yingzhao, HE Xiaohu, XU Tao, REN Jianye, LIU Xiaoyan, LING Tao, HAN Guangming. THE SEQUENCE STRATIGRAPHY OF HUANGLIU FORMATION AND THE INTERNAL STRUCTURES OF SUBMARINE FAN IN DONGFANG AREA,YINGGEHAI BASIN[J]. Marine Geology & Quaternary Geology, 2015, 35(2): 91-99. doi: 10.3724/SP.J.1140.2015.02091

THE SEQUENCE STRATIGRAPHY OF HUANGLIU FORMATION AND THE INTERNAL STRUCTURES OF SUBMARINE FAN IN DONGFANG AREA,YINGGEHAI BASIN

1. Zhanjiang Branch of CNOOC Ltd., Zhanjiang 524057, China;
2. Institute of Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 17 May 2014

Revised Date: 29 August 2014

Abstract

Abstract

A large submarine fan complex was discovered in the Dongfang area of the Yinggehai Basin. Six 4-order sequences in the 1st Member of Huangliu Formation (SQHL1) were recognized. The submarine fan complex was mainly developed in SQHL11-SQHL13 (in LST). High resolution sequence stratigraphic analysis reveals that the submarine fan is consisted of several lobes formed in different times and the sands, which are formed as the 5th-order sequences, exhibit various shapes in a plane view. The lobes can be classified into three kinds, i.e. the simple fan lobes, complex fan lobes and single channels. Simple fan lobes, which are mainly occurred in the Dongfang 29-1 are, are rarely observed. The complex fan lobes are common, which are formed by cutting and stacking within simple fan lobes or curved channels, and could not be divided further. Single channel is the one isolated. Research shows that the simple fan and complex fan lobes in this area are related with channels and branch channels. The internal complicated structures of submarine fan owe their origin to regional tectonics, filling deposits and the development of structural transfer zone nearby. A series of regional tectonic activities occurred while the T31 sequence boundary was formed, which controlled the sedimentation of the time. In addition, the Yingxi Slope to the west of the Dongfang area was located in a structural transfer zone where the deposits from the ancient Lam River were transported through the Kontum Uplif to the Dongfang area. As the result, a huge delta and a large submarine fan complex were formed.
- sequence stratigraphy /
- submarine fan /
- simple fan lobe /
- complex fan lobe /
- single channel /
- structural transfer /
- Yinggehai Basin

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References

[1]	谢玉洪.构造活动型盆地层序地层分析及天然气成藏模式——以莺歌海盆地为例[M].北京:地质出版社,2009:29-109.[XIE Yuhong.Sequence Stratigraphic Analysis and Hydrocarbon Accumulation Models in Tectonically Active Basins:Case Study on the Yinggehai Basin[M].Beijing:Geological Publishing House,2009:29 Google Scholar -109.] Google Scholar
[2]	王振峰,裴健翔.莺歌海盆地中深层黄流组高压气藏形成新模式——DF14井钻获强超压优质高产天然气层的意义[J].中国海上油气, 2011,23(4):213-217. Google Scholar [WANG Zhenfeng,PEI Jiangxiang.A new accumulation model of high pressure gas in Huangliu Formation of the middle-deep interval in Yinggehai Basin:the significance of discovering a good-quality gas pay with overpressure and high production in Well DF14[J]. China Offshore Oil and Gas,2011,23(4):213-217.] Google Scholar
[3]	王立锋,马光克,周家雄,等.东方气田储层非均质性描述[J].天然气工业,2009:29(1):38-40. Google Scholar [WANG Lifeng, MA Guangke, ZHOU Jiaxiong, et al. Seismic description of reservoir heterogeneity in Dongfang gas field[J]. Natural Gas Industry, 2009,29(1):38-40.] Google Scholar
[4]	裴健翔,于俊峰,王立锋,等.莺歌海盆地中深层天然气勘探的关键问题及对策[J].石油学报,2011,32(4):573-579. Google Scholar [PEI Jianxiang, YU Junfeng, WANG Lifeng,et a1.Key challenges and strategies for the success of natural gas exploration in mid-deep strata of the Yinggehai Basin[J]. Acta Petrolei Sinica, 2011,32(4):573-579.] Google Scholar
[5]	谢玉洪,王振峰,解习农,等.莺歌海盆地坡折带特征及其对沉积体系的控制[J].地球科学-中国地质大学学报,2004,29(5):569-574. Google Scholar [XIE Yuhong, WANG Zhenfeng, XIE Xinong, et al. Patterns of slope-break zone and their depositional models in the Yinggehai Basin[J]. Earth Science-Journal of China university of Geology, 2004,29(5):569-574.] Google Scholar
[6]	谢玉洪,刘平,黄志龙.莺歌海盆地高温超压天然气成藏地质条件及成藏过程[J].天然气工业, 2012:32(4):19-23. Google Scholar [XIE Yuhong, LIU Ping, HUANG Zhilong. The forming conditions and accumulation process analysis on high temperature-pressure natural gas reservoir in Yinggehai basin[J].Natural Gas Industry, 2012:32(4):19-23.] Google Scholar
[7]	谢玉洪.莺歌海高温超压盆地压力预测模式及成藏新认识[J].天然气工业,2011,31(12):21-25. Google Scholar [XIE Yuhong. Models of pressure prediction and new understandings of hydrocarbon accumulation in Yinggehai basin with high temperature and super-high pressure[J].Natural Gas Industry, 2011,31(12):21-25.] Google Scholar
[8]	童传新, 王振峰,李绪深.莺歌海盆地东方1-1气田成藏条件及其启示[J].天然气工业,2012,32(8):11-15. Google Scholar [TONG Chuanxin, WANG Zhenfeng, LI Xushen. Pooling conditions of gas reservoirs in the Dongfang 1-1 Gas Field,Yinggehai Basin[J].Natural Gas Industry, 2012,32(8):11-15.] Google Scholar
[9]	黄保家,李绪深,谢瑞永.莺歌海盆地输导系统及天然气主运移方向[J].天然气工业,2007,27(4):4-6. Google Scholar [HUANG Baojia, LI Xushen, XIE Ruiyong. Carrier system and dominant migration direction of natural gas in Yinggehai basin[J].Natural Gas Industry, 2007,27(4):4-6.] Google Scholar
[10]	徐强,何汉漪,等.莺歌海盆地变密度流和喷溢流沉积及其油气勘探意义[J].中国海上油气,2005,17(4):217-224. Google Scholar [XU Qiang,HE Hanyi, et al.Modified-density flow and shedding flow sediments and their petroleum exploration significance in Yinggehai basin[J]. China Offshore Oil and Gas, 2005,17(4):217-224.] Google Scholar
[11]	朱建成,何家雄,等.莺歌海盆地底辟带中深层高温超压领域天然气勘探前景分析[J].海洋石油,2004,24(4):21-26. Google Scholar [ZHU Jiancheng, HE Jiaxiong,et al. The Exploration Outlook of Natural Gas under High Temperature and High Pressure in Medium-Deep Layer in the Shale Diapir Belt of the Yinggehai Basin[J]. Offshore Oil,2004,24(4):21-26.] Google Scholar
[12]	王亚辉,赵鹏肖,左倩媚,等,测井信号小波变换在层序地层划分中的应用——以南海北部莺歌海盆地D14井黄流组为例[J].沉积与特提斯地质,2011,31(4):58-63. Google Scholar [WANG Yahui,ZHAO Pengxiao,ZUO Qianmei,et al. An application of the wavelet transformation to sequence stratigraphy:A case study of the Huangliu Formation in the Yinggehai Basin,northern South China Sea[J]. Sedimentary Geology and Tethyan Geology, 2011,31(4):58-63.] Google Scholar
[13]	谢玉洪,范彩伟.莺歌海盆地东方区黄流组储层成因新认识[J].中国海上油气,2010,22(6):355-359. Google Scholar [XIE Yuhong, FAN Caiwei. Some new knowledge about the origin of Huangliu Formation reservoirs in Dongfang area, Yinggehai basin[J]. China Offshore Oil and Gas,2010,22(6):355-359.] Google Scholar
[14]	谢玉洪,张迎朝,李绪深,等.莺歌海盆地超压气藏控藏要素与成藏模式[J].石油学报,2012,33(4):601-609. Google Scholar [XIE Yuhong, ZHANG Yingzhao, LI Xushen, et al. Main controlling factors and formation models of natural gas reservoirs with high-temperature and overpressure in Yinggehai Basin[J]. Acta Petrolei Sinica, 2012,33(4):601-609.] Google Scholar
[15]	谢金有,祝幼华,李绪深,等.南海北部大陆架莺琼盆地海平面变化[J].海相油气地质,2012,17(1):53-55. Google Scholar [XIE Jinyou, ZHU Youhua, LI Xushen,et al. The Cenozoic sea-level changes in Yinggehai-Qiongdongnan basin, Northern South China Sea[J]. Marine Origin Petroleum Geology, 2012,17(1):53-55.] Google Scholar
[16]	李俊良,何卫军,何小胡,等.南海北部莺歌海盆地新近纪古环境与层序地层格架再认识[J].微体古生物学报,2011,28(4):403-410. Google Scholar [LI Junliang, HE Weijun, HE Xiaohu,et al. Paleoenviormental reconstruction and re-examination of the Neogene Yinggehai asin, northern South China Sea[J].Acta Micropalaeontologica Sinica, 2011,28(4):403-410.] Google Scholar
[17]	Catuneanu O, Abreu V, Bhattacharya J P, et al.Towards the standardization of sequence stratigraphy[J].Earth-Science Reviews,2009,92:1-33. Google Scholar
[18]	钟泽红,刘景环,张道军,等,莺歌海盆地东方区大型海底扇成因及沉积储层特征[J].石油学报,2013,34(S2):102-111. Google Scholar [ZHONG Zehong,LIU Jinghua,ZHANG Daojun,et al. Oriqin and sedimentary reservoir characteristics of a large submarine fan in Dongfang area, Yinggehai basin.[J].Acta Petrolei Sinica, 2013,34(S2):102-111.] Google Scholar
[19]	庞雄,陈长民,彭大钧,等.南海珠江深水扇系统的层序地层学研究[J].地学前缘,2007,14(1):220-229. Google Scholar [PANG Xiong, CHEN Changmin, PENG Dajun, et al. Sequence stratigraphy of Pearl River Deep-water Fan System in the South China Sea[J].Earth Science Frontiers,2007,14(1):220-229.] Google Scholar
[20]	庞雄,柳保军,颜承志,等.关于南海北部深水重力流沉积问题的讨论[J].海洋学报,2012,34(3):114-119. Google Scholar [PANG Xiong, LIU Baojun, YAN Chengzhi,et al. Some reviews on deep-water gravity-flow deposition in the northern South China Sea[J]. Acta Oceanologica Sinica, 2012,34(3):114-119.] Google Scholar
[21]	龚再升,李思田,谢俊泰,等.南海北部大陆边缘盆地分析与油气聚集[M].北京:科学出版社,1997:44-126.[GONG Zaisheng, LI Sitian,XIE Juntai, et a1.Basin analysis and hydrocarbon accumulation in the northern continental margin of South China Sea[M].Beijing:Science Press,1997 Google Scholar :44-126.] Google Scholar
[22]	姚根顺,吕福亮,等.深水油气地质导论[M].北京:石油工业出版社,2012.[Paul Weimer,Roger M Statt.Introduction to the Petroleum Geology of Deepwater Settings[M]. Beijing:Petroleum Industry Publishing House,2012.] Google Scholar
[23]