鄂爾多斯盆地安邊—新安邊地區(qū)長6油層組成藏特征研究
[Abstract]:The Anbian-Xin 'anbian area is located in the central and western part of the Yishan slope of the secondary structural unit of the Ordos Basin. The Chang 6 oil formation is the main exploration horizon in this area. At present, many large reservoirs have been discovered. But there are obvious differences in hydrocarbon enrichment between different formations in different blocks in the study area. Based on petroleum geology and modern oil and gas accumulation theory, this paper uses a large amount of analytical and laboratory data to analyze the conditions of oil and gas accumulation and the reasons for the difference of oil and gas accumulation in the study area, on the basis of fully absorbing the previous research results and based on the theory of petroleum geology and modern oil and gas accumulation. The model of oil and gas reservoir formation is established and the main controlling factors of oil and gas accumulation are summarized, which provides a good guide for the further exploration and development of oil and gas in the study area. Based on the theories and methods of reservoir geology, sedimentary petrology and logging geology, this paper makes a systematic analysis and study on the reservoir characteristics and the distribution characteristics of sand bodies in the study area. The results show that the main rock types of Chang 6 in the study area are gray fine-grained feldspar sandstone and lithic feldspar sandstone with intergranular pore and feldspar dissolution pore as the main reservoir space and a small number of fractures. The porosity of Chang 6 is mainly distributed in the range of 6 ~ 18%, the main distribution of permeability is in the range of less than 0.1 脳 10 ~ (-3) 渭 m ~ (2), the physical property of longitudinal length 63 is the worst, Chang62 is the second, and Chang61 is the best. The physical properties of Anbian area on the plane are better than that of Xinanbian area. Chang 61 sand body is the most developed, the thickness is large, the transverse stability of sand body is good along the direction of material source, the second is long 62, the scale is longer 61 small, there are many sets of sand bodies overlay, also have certain connectivity in some areas. The length of 63 is the smallest, and the horizontal connectivity is the worst. The present exploration results show that Chang61, Chang62 and Chang63 are enriched in Xinanbian area, but only in Chang61, Chang62 and Chang63 in Anbian area. The oil source correlation indicates that Chang 6 crude oil in the study area mainly comes from the supply of source rock of Lower potential Chang 7, and the contribution of mudstone of Chang 6 itself is limited. According to the distribution map of Chang7 mudstone, Chang7 mudstone is relatively developed in Xinanbian area, but not developed in Anbian area, the main motive force of oil and gas accumulation is abnormal high pressure and hydrocarbon generating pressure caused by undercompaction of mudstone. The cracks are relatively developed in Xinanbian area, but not in Anbian area. It is concluded that the reservoir formation in Xinanbian area is the vertical migration of hydrocarbon products from source rock of Lower potential Chang 7 to Chang 6 reservoir, and the fracture is the key to reservoir formation in Xinanbian area. The reservoir formation in Anbian area is the lateral migration of Chang61 crude oil in Xinanbian area. Sand connectivity, physical property and monoclinic structure are the key factors for reservoir formation in Anbian area. The main controlling factors of hydrocarbon accumulation in the study area are summarized as follows: distribution of source rocks, distribution of fractures, reservoir physical properties, distribution of sand bodies and monoclinic structures.
【學位授予單位】:西南石油大學
【學位級別】:碩士
【學位授予年份】:2015
【分類號】:P618.13
【參考文獻】
相關期刊論文 前10條
1 徐波;孫衛(wèi);;姬塬油田長4+5砂巖儲層孔隙類型與成巖作用[J];吉林大學學報(地球科學版);2008年06期
2 藺宏斌;侯明才;陳洪德;董桂玉;;鄂爾多斯盆地上三疊統(tǒng)延長組沉積體系特征及演化[J];成都理工大學學報(自然科學版);2008年06期
3 竇偉坦;侯明才;陳洪德;董桂玉;;鄂爾多斯盆地三疊系延長組油氣成藏條件及主控因素研究[J];成都理工大學學報(自然科學版);2008年06期
4 李延鈞,王廷棟,張艷云,陳世加,王緒龍;準噶爾盆地南緣天然氣成因與成藏解剖[J];沉積學報;2004年03期
5 邱楠生;Peter Reiners;梅慶華;姜光;Nicolesco Stefan;陶成;;(U-Th)/He年齡在沉積盆地構造—熱演化研究中的應用——以塔里木盆地KQ1井為例[J];地球物理學報;2009年07期
6 郝芳,鄒華耀,姜建群;油氣成藏動力學及其研究進展[J];地學前緣;2000年03期
7 高先志,陳發(fā)景;應用流體包裹體研究油氣成藏期次——以柴達木盆地南八仙油田第三系儲層為例[J];地學前緣;2000年04期
8 楊友運,張蓬勃,張忠義;鄂爾多斯盆地西峰油田長8油組辮狀河三角洲沉積特征與層序演化[J];地質科技情報;2005年01期
9 付金華,郭正權,鄧秀芹;鄂爾多斯盆地西南地區(qū)上三疊統(tǒng)延長組沉積相及石油地質意義[J];古地理學報;2005年01期
10 鄧秀芹;付金華;姚涇利;龐錦蓮;孫勃;;鄂爾多斯盆地中及上三疊統(tǒng)延長組沉積相與油氣勘探的突破[J];古地理學報;2011年04期
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