少断裂深水油气成藏模式与有利区优选——以圭亚那盆地上白垩统为例
陶叶 , 何幼斌 , 吴东胜 , 马福康 , 李奕添 , 鲍志东
东北石油大学学报 ›› 2024, Vol. 48 ›› Issue (5) : 62 -74.
少断裂深水油气成藏模式与有利区优选——以圭亚那盆地上白垩统为例
Deepwater hydrocarbon accumulation model and optimal selection of favorable areas under the condition of few faults: a case study of the Upper Cretaceous in Guyana Basin
In order to clarify the hydrocarbon migration mechanism and accumulation mode under the condition of less faults, this paper takes the Upper Cretaceous in the Guyana Basin as an example, and studies the petroleum geological characteristics of the Upper Cretaceous in the Guyana Basin by using seismic data, drilling data and source rock analysis data. We have defined the reservoir-forming model of the study area and divided the favorable exploration areas. The results show that the source rocks of the Upper Cretaceous in the basin are huge thick black shales deposited in the Toulon-Coniacian stage. The TOC range of organic matter is , and the organic matter types are mainly type I and type II. The reservoirs in the study area are Kampan-Maastrichtian channel, embankment and foliar subfacies sandstone. The study area is mainly covered by mudstone and thick siltstone with poor physical properties deposited in the Early Paleogene. The migration system of "sand body superposition and fault oblique transport type" is developed in the continental shelf area of the basin, and the reservoir formation model of "source rock and reservoir close proximity, fault and sand body matching, and channel gathering" is formed. The migration system of "sand body superposition and fracture vertical transport type" is developed in the deep water area, and the reservoir formation mode of "source rock and reservoir separation, fracture and sand body matching and high point gathering" is formed. The overlapped area of source rock development and channel development in the deep water area of the central basin is the first exploration target, and the overlapped area of source rock development and bank development in the north or the channel development area that does not coincide with source rock development is the second exploration target. The results are of guiding significance to the exploration of basins with similar geological conditions.
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国家重点研发计划专项(2017YFC0603104)
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