Paleogeomorphic features and sedimentary facies model of Jurassic strata in Chaoshan sub-basin, northern South China Sea

QIANG Kunsheng; ZHANG Guangxue; ZHANG Li; LÜ Baofeng; ZHONG Guangjian; FENG Changmao; YI Hai

doi:10.12029/gc20180614

GEOLOGY IN CHINA > 2018 > 45(6): 1251-1258. > DOI: 10.12029/gc20180614

QIANG Kunsheng, ZHANG Guangxue, ZHANG Li, LÜ Baofeng, ZHONG Guangjian, FENG Changmao, YI Hai. Paleogeomorphic features and sedimentary facies model of Jurassic strata in Chaoshan sub-basin, northern South China Sea[J]. GEOLOGY IN CHINA, 2018, 45(6): 1251-1258. DOI: 10.12029/gc20180614

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Paleogeomorphic features and sedimentary facies model of Jurassic strata in Chaoshan sub-basin, northern South China Sea

1.
MLR Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Guangzhou 510760, Guangdong, China
2.
School of Marine Science, Sun Yat-Sen University, Guangzhou 510082, Guangdong, China

Funds:

Key Laboratory of Seabed Mineral Resources Open Fund project of Ministry of Land and Resources KLMMR-2017-A-15

China Geological Survey project, "Northern South China Sea and Taiwan Strait Hydrocarbon Resources Survey" DD20160154

More Information

Author Bio:
QIANG Kunsheng, male, born in 1980, engineer, engages in comprehensive geological study of marine oil and gas; E-mail: qks80@163.com
Corresponding author:
ZHANG Guangxue, male, born in 1965, professor, mainly engages in the offshore deepwater oil and gas hydrates research; E-mail: zhguangxue@tom.com
Received Date: July 17, 2018
Revised Date: November 09, 2018
Available Online: September 25, 2023

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Abstract

Abstract

The Mesozoic strata in the Chaoshan sub-basin of northern South China Sea have rich oil and gas resources. Seismic data and well logging data were used in combination with fine stratigraphic division and denudation calculation to restore paleogeomorphology of the Jurassic sedimentary strata.On the basis of sedimentary facies marker analysis of residual strata, a Jurassic sedimentary model was established. The Jurassic strata suffered denudation alterations at the end of Early Jurassic and Middle Jurassic. Various elements of paleogeomorphology influenced sedimentary system development. Ancient uplift (bulge) indicated the source and direction of sediments. The ancient sea bottom canyon was an important transport passage between source and sedimentation. The slope zone was an important deposition site and had great influence on the quality and size of reservoirs, thus restricting the accommodation space of the basin. The basin bottom (depression) topography controlled the morphology and occurrence of sediments and influenced the quality and size of source rocks. Effective combination of all the elements of paleogeomorphology in time and space seems to be the key to accurate determination of the distribution and range of a sedimentary system, and its control of sedimentary reservoirs and source rocks is very obvious. The conclusion has positive significance for the next exploration and favorable reservoir prediction of the Jurassic strata.
- sedimentary faces,
- depositional characteristics,
- Chaoshan Sub-basin,
- Jurassic

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References (37)

References

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Paleogeomorphic features and sedimentary facies model of Jurassic strata in Chaoshan sub-basin, northern South China Sea