西部凹陷中南部潜山储层特征研究
[Abstract]:The study area is located in the central and southern part of the west slope of the western sag, rising from the west slope to the lower steps, and from the east to the clear water sag. The buried hills on the west slope are only located in Huanxiling, Qijia, Dujiatai, Shengtang and Shuguang buried hills to predict the proven oil geological reserves, most of which are concentrated in the middle and high buried hill zones, but there are blank areas in the deep buried hills and the deep layers of the proven buried hills. The exploration degree of Paleogene in the central and southern part of the western sag is relatively high, and the difficulty of finding and implementing the favorable targets of the Paleogene is increasing day by day, while the exploration degree of buried hill is relatively low, and the favorable exploration area is large. The Proterozoic and Mesozoic. There are various types of reservoirs, including eroded residual mountain reservoirs and fault-block mountain reservoirs, and different reservoir forming conditions of buried hill in different periods and types. Because of the different types of buried hill reservoirs on the west slope, various formation conditions, complexity of lithologic changes and difficulty in determining the distribution of oil, gas and water, the process of buried hill exploration in the western sag is affected. The development of this paper is based on structural interpretation, supplemented by reservoir forming condition analysis. In the structural interpretation, comprehensive use of logging, seismic, drilling and analysis of laboratory data, for fine structural interpretation and reservoir characteristics analysis, By constructing several geological sections running through the north and south of the east, west and east of the working area, establishing the macroscopic frame of seismic interpretation, and determining the top interface of the buried hill in the middle and deep layers by logging calibration and VSP, earthquake prediction is the main factor in the cross-well area and the area where the wells are lacking. And combined with attribute analysis to determine. Based on the analysis of tectonic evolution and fault growth index, it is considered that buried hill traps formed embryonic form before Tertiary system, and the main growth period is the fourth stage of sand, which is fixed in the third stage of sand. The traps in favorable target areas are not affected by late faults but by the favorable transformation of early faults. In the analysis of reservoir conditions, it is possible that the deep fault, sufficient oil source and the interlayer of buried hill interior are the accumulation of buried hill insider. In combination with the previous understanding and analysis of the lithologic types of metamorphic rocks in the study area, it is determined that the predicted lithology of buried hills is migmatite and gneiss, which has a certain predominance over diabase and amphibolite in the dominant lithologic sequence. Fracture is the key of buried hill and inside reservoir formation. By analyzing the data of adjacent wells, it is considered that the fractures in this research area are relatively developed and easy to form fractured reservoirs, and the overlying sand 3 and sand 4 member of buried hill have large formation thickness and mudstone development. It can be used as the caprock in the region and as a favorable source rock in the study area. The target of optimal selection is in Manan buried hill area. According to the discussion of oil supply window of previous data, there is a large range of hydrocarbon supply in the proposed target area, which is conducive to the formation of reservoir in the target area. According to the type and location of reservoir formation in this area, two types of reservoir forming models are divided, and the possibility of reservoir formation of favorable target is discussed theoretically. Finally, hydrocarbon detection is carried out in the target area, and it is effective to analyze the accumulation of weathering crust and inside of buried hill in the target area. Based on the above studies, the characteristics of buried hill reservoirs in the study area are summarized and the controlling factors of hydrocarbon accumulation are analyzed, the types of buried hill reservoirs are classified, and the model of buried hill reservoir formation is determined. The structural morphology and fault distribution of buried hill are carried out, lithologic assemblages, distribution and reservoir control factors of buried hill are made clear, the contact relationship between buried hill and effective source rock is determined, so as to select favorable target and propose well location.
【学位授予单位】:长江大学
【学位级别】:硕士
【学位授予年份】:2015
【分类号】:P618.13
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