论文部分内容阅读
鄂尔多斯盆地油气资源丰富,盆地构造平缓,以岩性、岩性-地层和古地貌油气藏为主,储层厚度薄.本文详细分析了鄂尔多斯盆地油气地质、油气资源的形成与分布,指出了鄂尔多斯盆地油气勘探方向及地震勘探技术系列在该盆地大油气田的发现中的不可替代的重要作用.
鄂尔多斯盆地油气地质与勘探
【摘 要】
：
鄂尔多斯盆地油气资源丰富,盆地构造平缓,以岩性、岩性-地层和古地貌油气藏为主,储层厚度薄.本文详细分析了鄂尔多斯盆地油气地质、油气资源的形成与分布,指出了鄂尔多斯盆地
【机 构】
：
长庆油田公司
【出 处】
：
应用地球物理（英文版）
【发表日期】
：
2004年期
其他文献
Measurement of Metallogenic Depth and Deep Second Enrichment Belt Forecasting in Jiaodong Gold Depos
The depth is important for ore finding in Jiaodong gold deposit. However, many geologists are still discussing how to confirm the depth for the tectonic and met
With a thermal manikin, the distribution pattern of thermal insulation in multi-layered clothing ensemble is studied. It is found that the thermal insulation of
Time-domain identification of dynamic properties of layered soil by using extended Kalman filter and
A novel time-domain identification technique is developed for the seismic response analysis of soil-structurc interaction. A two-degree-of-freedom (2DOF) model
A new method based on mass fluxes and observed ozone profiles was developed to estimate cross- tropopause ozone flux. Using this method, we estimated the cross-
The superlarge Baguamiao, large Liba and Xiaogouli gold deposits represent three typical gold deposits different from the Carlin type in the western Qinling Oro
鄂尔多斯盆地西缘前陆盆地属典型的黄土塬地貌,地表黄土切割剧烈,地下地质构造复杂.鉴于电磁阵列剖面(CEMP)法在山前带勘探的方法优势以及在西部多年的勘探成效,对鄂尔多斯盆
Quantitative research of the origin of sulfur isotopes is a difficult problem that has puzzled geochemists all along. In the study of the middle and lower reach
在频率选择性衰落环境下,作为一种有效的传输分集体制,空频 正交频分复用(spacefrequency orthogonalfrequencydivisionmultiplexing,SF OFDM)技术得到了广泛的关注。但是这
Seismic images of the mantle beneath the active Changbai intraplate volcano in Northeast China determined by teleseismic travel time tomography are presented. T
Geochemistry of the ophiolite and oceanic island basalt in the Kangxian-Pipasi-Nanping tectonic m la
Detailed studies indicate that Kangxian-Pipasi-Nanping tectonic zone is a complicated mélange zone which includes many tectonic slabs of different origins. Oph