2013Journal of Oil and Gas TechnologyRequires access

Depositional Filling Characteristics of Paleogene in Heshan Sag of Ultra Deepwater Area in the Northern South China Sea

Jun Liu

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Abstract

Heshan Sag was located in lower continental slope of northern margin of the South China Sea , its south side was close to the NW subbasin , it had special geological conditions such as thinning crust , ductile deformation of the lithosphere and high heat flow anomalies.Therefore Heshan Sag had special characteristics of depositional filling.Sequence stratigraphy and seismic facies studies show that Wenchang , Enping and Zhuhai Formations are developed in the Paleogene of Heshan Sag , the top and base of the formation are large unconformity.Terrestrial lacustrine deposition is developed during Wenchang and Enping Formations , in which the seismic reflection characteristics of middle-deep lacustrine mudstone are similar to the source rock of Baiyun Sag , it is the main hydrocarbon source rock in Heshan Sag , the shallow marine delta deposits are developed in Zhuhai Formation with S Type of progradational reflections , delta sandstone is the main reservoir in Heshan Sag.In addition , There exist the gravity flow deepwater fan sands

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Heshan Sag was located in lower continental slope of northern margin of the South China Sea , its south side was close to the NW subbasin , it had special geological conditions such as thinning crust , ductile deformation of the lithosphere and high heat flow anomalies.Therefore Heshan Sag had special characteristics of depositional filling.Sequence stratigraphy and seismic facies studies show that Wenchang , Enping and Zhuhai Formations are developed in the Paleogene of Heshan Sag , the top and base of the formation are large unconformity.Terrestrial lacustrine deposition is developed during Wenchang and Enping Formations , in which the seismic reflection characteristics of middle-deep lacustrine mudstone are similar to the source rock of Baiyun Sag , it is the main hydrocarbon source rock in Heshan Sag , the shallow marine delta deposits are developed in Zhuhai Formation with S Type of progradational reflections , delta sandstone is the main reservoir in Heshan Sag.In addition , There exist the gravity flow deepwater fan sands

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Available abstract

Heshan Sag was located in lower continental slope of northern margin of the South China Sea , its south side was close to the NW subbasin , it had special geological conditions such as thinning crust , ductile deformation of the lithosphere and high heat flow anomalies.Therefore Heshan Sag had special characteristics of depositional filling.Sequence stratigraphy and seismic facies studies show that Wenchang , Enping and Zhuhai Formations are developed in the Paleogene of Heshan Sag , the top and base of the formation are large unconformity.Terrestrial lacustrine deposition is developed during Wenchang and Enping Formations , in which the seismic reflection characteristics of middle-deep lacustrine mudstone are similar to the source rock of Baiyun Sag , it is the main hydrocarbon source rock in Heshan Sag , the shallow marine delta deposits are developed in Zhuhai Formation with S Type of progradational reflections , delta sandstone is the main reservoir in Heshan Sag.In addition , There exist the gravity flow deepwater fan sands

Key concepts: Geology, Sedimentary depositional environment, Paleogene, Paleontology, Geochemistry, Geomorphology, Unconformity, Facies

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