

FOLLOWUS
1.Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
3.Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, China
4.Oil Industry Training Center, China University of Petroleum (East China), Qingdao 266580, China
XIAO Guolin, xgl253@163.com
ZENG Zhigang, zgzeng@qdio.ac.cn
收稿:2020-01-28,
录用:2020-3-15,
网络首发:2020-03-28,
纸质出版:2020-07
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New insights into marine hydrocarbon geological conditions in the South Yellow Sea Basin: evidence from borehole CSDP-2[J]. 海洋湖沼学报(英文), 2020,38(4):1169-1187.
Laixing CAI, Guolin XIAO, Zhigang ZENG, et al. New insights into marine hydrocarbon geological conditions in the South Yellow Sea Basin: evidence from borehole CSDP-2[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1169-1187.
New insights into marine hydrocarbon geological conditions in the South Yellow Sea Basin: evidence from borehole CSDP-2[J]. 海洋湖沼学报(英文), 2020,38(4):1169-1187. DOI: 10.1007/s00343-020-0068-8.
Laixing CAI, Guolin XIAO, Zhigang ZENG, et al. New insights into marine hydrocarbon geological conditions in the South Yellow Sea Basin: evidence from borehole CSDP-2[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1169-1187. DOI: 10.1007/s00343-020-0068-8.
The South Yellow Sea Basin (SYSB) has multiple sets of proven source rocks and good hydrocarbon prospects
but no industrial oil and gas has been explored at present. To solve this puzzle for petroleum geologists
we systematically investigated the marine hydrocarbon geological conditions based on cores and testing data from borehole CSDP-2
the first exploration well with continuous coring in SYSB. The qualities of source rocks are evaluated in detail according to organic matter abundance
type
and maturity. The reservoir characterization mainly includes porosity
permeability
and reservoir space. Displacement pressure test and stratum thickness are the main foundations for defining the caprocks. Then
the oil-source rock correlation in the Permian and stratum model are analyzed to determine the favorable source-reservoir-caprock assemblages. The results show that three sets of effective source rocks (the Lower Triassic
Upper Permian
and Lower Permian)
two sets of tight sandstone reservoirs (the Upper Permian and Lower Silurian-Upper Devonian)
and two sets of caprocks (the Lower Triassic and Carboniferous) combine to constitute the hydrocarbon reservoir-forming assemblages of "lower-generation and upper-accumulation" and "self-generation and self-accumulation"
thus laying a solid foundation for promising petroleum prospects. The three sets of marine source rocks are characterized by successive generation and expulsion stages
which guarantees multistage hydrocarbon accumulation. Another three sets of continental source rocks distributed across the Middle Jurassic
Upper Cretaceous
and Paleogene depression areas
especially in the Northern Depression
may supplement some hydrocarbons for the Central Uplift through faults and the Indosinian unconformity. The favorable Permian exploration strata have been identified in the Central Uplift of SYSB. First
the Lower Permian and Upper Permian source rocks with high organic matter abundance and high thermal maturity supply sufficient hydrocarbons. Secondly
the interbedding relationship between the source rocks and sandstones in the Upper Permian strata ensures that hydrocarbons have been migrated into the nearby Upper Permian sandstones
reflecting near-source hydrocarbon accumulation. Finally
the good sealing property of the Lower Triassic Qinglong Formation caprocks plays an indispensable role in hydrocarbon preservation of the Permian reservoirs. This conclusion is supported by direct oil shows
gas logging anomalous layers
and hydrocarbon-bearing fluid inclusions.
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