THE CONDITION AND PATTERN OF TURBIDITE FAN RESERVOIR FORMATION IN EASTERN DONGYING DEPRESSION, SHANDONG PROVINCE

SUN Hai-ning; XIA Jing-sheng; ZHONG Jian-hua; WANG Zhi-kun

2008 Vol. 14, No. 3

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Article navigation > Journal of Geomechanics > 2008 > 14(3): 221-230

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SUN Hai-ning, XIA Jing-sheng, ZHONG Jian-hua, WANG Zhi-kun. THE CONDITION AND PATTERN OF TURBIDITE FAN RESERVOIR FORMATION IN EASTERN DONGYING DEPRESSION, SHANDONG PROVINCE[J]. Journal of Geomechanics, 2008, 14(3): 221-230.

Citation:

THE CONDITION AND PATTERN OF TURBIDITE FAN RESERVOIR FORMATION IN EASTERN DONGYING DEPRESSION, SHANDONG PROVINCE

1.
Faculty of Geoscience, Dongxin Production Factory, Shengli Oilfield, SINOPEC, Dongying 257094, China
2.
Research Institute of Exploration and Development, PetroChina Jidong Oilfield Company, Tangshan 063004, China
3.
Faculty of Geo-Resources and Information, China University of Petroleum, Dongying 257061, China
4.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

Received Date: 15 January 2008

Publish Date: 25 September 2008

Abstract

Abstract

Lithologic hydrocarbon reservoir has been thought of a focal point of exploration in Dongying depression.A great amount of massive source rocks developed in Members 3 and 4 of the Shahejie Formation (S₃ and S₄) in eastern Dongying depression provide sufficient hydrocarbon resources for lithologic traps.In this area there are well developed fluxoturbidite in front of delta, deep-water turbidite fan and other little sand body, and such transportation systems as sand bodies, rifts, and unconformities, as well as mudstone seal, are often met with.There are good matching source rocks, reservoir bed and seal display a good match spatially and temporally, which provided a favourable conditions for formation of lithologic hydrocarbon reservoir and structure-lithologic hydrocarbon reservoir.
- accumulation condition /
- accumulation model /
- turbidite fan /
- lithologic hydrocarbon reservoir /
- eastern Dongying depression

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References

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