Gravity flow sedimentary system and petroleum exploration prospect of deep water area in the Qiongdongnan Basin, South China Sea

被引:0
|
作者
Yao, Zhe [1 ]
Zhu, Jitian [1 ]
Zuo, Qianmei [1 ]
Man, Xiao [1 ]
Mao, Xuelian [1 ]
Wang, Zhenzhen [1 ]
Dang, Yayun [1 ]
机构
[1] CNOOC Zhanjiang Company, Zhanjiang,Guangdong,524057, China
关键词
Gas industry - Offshore gas fields - Petroleum prospecting - Hydrocarbons - Petroleum geology - Sedimentary rocks;
D O I
10.3787/j.issn.1000-0976.2015.10.003
中图分类号
学科分类号
摘要
Deep water petroleum exploration is still in start-up phase in China, and the study on the gravity flow theory of deep water sedimentation needs to be strengthened. In this paper, based on the seismic, coring, cuttings analysis and logging data, the gravity flow development conditions and sedimentary features of deep water area in the Qiongdongnan Basin were comprehensively analyzed, and the petroleum accumulation conditions of gravity flow realm in Central Depression of the deep water area were investigated in respect of the key factors like hydrocarbon source, reservoir and migration restricting the deep water hydrocarbon accumulation. The study results are obtained in three aspects. First, large reservoirs are developed in the deep water area, mainly including three gravity flow sedimentary systems, i. e. Huangliu Formation turbidite channel sand sedimentary system in the Central Canyon, Meishan Formation-Yinggehai Formation subsea apron sedimentary system in the Lingshui sag, and Lingshui Formation and Sanya Formation subsea apron sedimentary system in the Baodao-Changchang sag. Second, Lower Oligocene Yacheng Formation marine-terrestrial transitional facies coal-measure strata and semi-closed neritic facies mudstones are the important source rocks of deep water area in the Basin; Lingshui Formation subsea apron, Sanya Formation subsea apron, Meishan Formation subsea apron, Huangliu Formation canyon channel, and Yinggehai Formation subsea apron sandstone developed in Oligocene-Pliocene deep water area and the overlying bathyal-abyssal mudstone form five sets of regional reservoir-caprock assemblages; and proximal diapir and proximal fault are two kinds of efficient vertical source-connection modes in the deep water area. Third, the successful exploration of Lingshui 17-2 Gas Field in Central Canyon reveals that the gravity flow realm in Central Depression of the Qiongdongnan Basin represented by Central Canyon has a favorable exploration prospect. Conclusions are reached that the subsea aprons in both Ledong-Lingshui sag and Baodao-Changchang sag also have good petroleum accumulation conditions and exploration potential, and should be the future exploration targets in deep water area. ©, 2015, Natural Gas Industry Journal Agency. All right reserved.
引用
收藏
页码:21 / 30
相关论文
共 50 条
  • [31] Seismic geomorphology and main controls of deep-water gravity flow sedimentary process on the slope of the northern South China Sea
    LI Lei1*
    2 College of Geosciences
    3 CNOOC Research Institute
    Science China(Earth Sciences), 2012, 55 (05) : 747 - 757
  • [32] Seismic geomorphology and main controls of deep-water gravity flow sedimentary process on the slope of the northern South China Sea
    Li Lei
    Wang YingMin
    Xu Qiang
    Zhao JingZhou
    Li Dong
    SCIENCE CHINA-EARTH SCIENCES, 2012, 55 (05) : 747 - 757
  • [33] Seismic geomorphology and main controls of deep-water gravity flow sedimentary process on the slope of the northern South China Sea
    Lei Li
    YingMin Wang
    Qiang Xu
    JingZhou Zhao
    Dong Li
    Science China Earth Sciences, 2012, 55 : 747 - 757
  • [34] Control effects of the synsedimentary faults on the basin-marginal fans in the central part of the deep-water area of early Oligocene Qiongdongnan Basin, South China Sea
    Guangzeng Song
    Zengxue Li
    Haizhang Yang
    Dongdong Wang
    Ying Chen
    Rui Sun
    ActaOceanologicaSinica, 2021, 40 (02) : 54 - 64
  • [35] Deep-Water Sedimentary Characteristics and Response in the Reed Area of the Southern South China Sea
    Zheng Hong-Bo
    Pin, Yan
    Wang, Yan-Lin
    Xing, Yu-Qing
    MARINE GEORESOURCES & GEOTECHNOLOGY, 2016, 34 (02) : 162 - 168
  • [36] Control effects of the synsedimentary faults on the basin-marginal fans in the central part of the deep-water area of early Oligocene Qiongdongnan Basin, South China Sea
    Song, Guangzeng
    Li, Zengxue
    Yang, Haizhang
    Wang, Dongdong
    Chen, Ying
    Sun, Rui
    ACTA OCEANOLOGICA SINICA, 2021, 40 (02) : 54 - 64
  • [37] Control effects of the synsedimentary faults on the basin-marginal fans in the central part of the deep-water area of early Oligocene Qiongdongnan Basin, South China Sea
    Guangzeng Song
    Zengxue Li
    Haizhang Yang
    Dongdong Wang
    Ying Chen
    Rui Sun
    Acta Oceanologica Sinica, 2021, 40 : 54 - 64
  • [38] The Controlling Factors and Prediction of Deep-Water Mass Transport Deposits in the Pliocene Qiongdongnan Basin, South China Sea
    Ge, Jiawang
    Zhao, Xiaoming
    Fan, Qi
    Pang, Weixin
    Yue, Chong
    Chen, Yueyao
    JOURNAL OF MARINE SCIENCE AND ENGINEERING, 2024, 12 (12)
  • [39] Geochemistry, origin and accumulation of natural gases in the deepwater area of the Qiongdongnan Basin, South China Sea
    Huang, Baojia
    Tian, Hui
    Li, Xushen
    Wang, Zhenfeng
    Xiao, Xianming
    MARINE AND PETROLEUM GEOLOGY, 2016, 72 : 254 - 267
  • [40] Periodic Characteristics of the Paleogene Tectonic Activity and Sedimentation Responses in the Deep-Water of Qiongdongnan Basin, South China Sea
    Xu, Meng
    Song, Guangzeng
    Li, Zengxue
    Wang, Dongdong
    Sun, Rui
    Chen, Ying
    MINERALS, 2023, 13 (02)