塔河油田九区白垩系舒善河组岩性圈闭识别与评价
[Abstract]:Tahe Oilfield is located in the northeast of Tarim Basin, Xinjiang. At present, the exploration and development of clastic rocks in Tahe Oilfield has entered the middle and late stage, and the exploration targets have gradually shifted from large structural traps to small scale lithologic traps. With the breakthrough of lithologic reservoir exploration in T903 well area in recent years, attention has been paid to the Cretaceous Shushanhe formation in Tahe Oilfield. The lithologic trap exploration degree of the Cretaceous Shushanhe formation is still relatively low, and the information available at present is relatively few, there are many problems which hinder the oil and gas exploration of the Shushanhe formation. The main layer studied in this paper is the Cretaceous Shushanhe formation. Based on the analysis of logging curves and seismic data and under the guidance of high resolution sequence stratigraphy theory, the long, medium and short term cycle datum levels are identified, and the Cretaceous Shushanhe formation is divided into a long term cycle (KLSC1). On the basis of three KMSC1~KMSC3 and several short term cycles, isochronous stratigraphic framework has been established. The transverse and longitudinal distribution characteristics of sand bodies and sedimentary facies are studied under the constraints of isochronous stratigraphic framework. The KMSC1 cycle of the Shushanhe formation is mainly braided delta front subfacies, the microfacies is the underwater distributary channel and the interdistributary bay, the sand body of the underwater distributary channel is mainly developed, and the sand body has good continuity. Log interpretation of oil-bearing gas reservoirs mainly concentrated in the upper sublayer of the cycle (No. 2 sand formation and No. 3 sand formation); The KMSC2 cycle of Shushanhe formation is mainly composed of shallow lacustrine subfacies, and the microfacies is shallow lake mud and sand dam. But the oil and gas interpretation of logging shows well, mainly in the lower sublayer of the cycle (4 sand formation and 5 sand formation). The KMSC3 cycle of Shushanhe formation is mainly braided river delta front subfacies, while the microfacies is underwater distributary channel and interdistributary bay, sand body is developed and continuity is good, but there is no oil and gas show. Through repeated comparison and analysis of various seismic attributes extracted, it is found that the average absolute amplitude attribute can well reflect the distribution of sand and mud. On this basis, the property values at the well point and the thickness of the solid sand body corresponding to the target layer are statistically analyzed, and the correlation can be obtained, and the distribution of the sand body can be roughly clarified. The conventional wave impedance inversion section in the study area can not distinguish sandstone and mudstone well. Using pseudo acoustic inversion can identify sand bodies over 8 m. A total of 11 traps were identified in the KMSC1~KMSC2 sublayer of the Cretaceous Shushanhe formation in the Jiulong area, including 8 lithologic traps and 3 tectonic-lithologic traps. According to the development of sand body, sealing property of caprock, oil and gas content and connection with oil source, a favorable trap is selected.
【学位授予单位】:成都理工大学
【学位级别】:硕士
【学位授予年份】:2017
【分类号】:P618.13
【参考文献】
相关期刊论文 前10条
1 Hao Liu;Chang-Song Lin;Rui-Bo Guo;Min Zhu;Yong-Qian Cui;;Characteristics of the Paleozoic slope break system and its control on stratigraphic-lithologic traps:An example from the Tarim Basin,western China[J];Journal of Palaeogeography;2015年03期
2 马庆佑;吕海涛;蒋华山;李晓益;;塔里木盆地台盆区构造单元划分方案[J];海相油气地质;2015年01期
3 陈欢庆;赵应成;高兴军;谢雯;穆剑东;;高分辨率层序地层学在地层精细划分与对比中的应用——以辽河西部凹陷某试验区于楼油层为例[J];地层学杂志;2014年03期
4 马丽娟;王明;林东升;;塔河地区中新生界岩性圈闭预测研究[J];石油天然气学报;2014年04期
5 陈新刚;张旭光;;塔河油田三叠系中油组岩性圈闭识别研究[J];新疆地质;2013年S1期
6 王开燕;徐清彦;张桂芳;程某存;李培海;;地震属性分析技术综述[J];地球物理学进展;2013年02期
7 李曰俊;杨海军;张光亚;郑多明;刘云祥;赵岩;李国会;刘亚雷;;重新划分塔里木盆地塔北隆起的次级构造单元[J];岩石学报;2012年08期
8 陈恭洋;陈玲;朱洁琼;曹兰柱;辛玮江;;地震属性分析在河流相储层预测中的应用[J];西南石油大学学报(自然科学版);2012年03期
9 刘凡t@;陈红汉;唐大卿;李楠;;塔里木盆地中—新生界构造单元划分[J];地质科技情报;2012年03期
10 阙晓辉;王淘;向参;;浅谈阿克库勒凸起构造演化模式[J];内江科技;2012年04期
相关博士学位论文 前1条
1 宋建勇;博兴洼陷高分辨率层序地层研究与储层预测[D];中国科学院研究生院(海洋研究所);2005年
相关硕士学位论文 前3条
1 兰宁;高分辨率层序地层学特征与储层预测研究[D];成都理工大学;2016年
2 陈玲;霸县凹陷文安斜坡沙二段—东营组地震属性分析[D];长江大学;2012年
3 黄龙;富县地区延长组高分辨率层序地层及层序格架内储集砂体展布规律研究[D];成都理工大学;2009年
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