1) the northern part of Liupanshan Basin
六盘山盆地北部
1.
Based on the theory of petrolrum system, this article makes an analysis on the formation and evolution process of the Mz petroleum system in the northern part of Liupanshan Basin, as well as the pre-sent characteristics of Mz petroleum system, which guides the petroleum exploration in this area.
该文运用含油气系统理论,分析六盘山盆地北部中生界油气系统形成演化过程,以及现今盆地北部中生界油气系统特征,并以此指导该地区的中(新)生界油气勘探。
2) Liupanshan Basin
六盘山盆地
1.
Mesozoic Geological Characteristics and Hydrocarbon Exploration Direction in Liupanshan Basin;
六盘山盆地中生界地质特征与油气勘探方向
2.
Geochemistry of hydrocarbon source rocks in the Liupanshan basin at the northeastern margin of the Qinghai-Tibet Plateau;
青藏高原东北缘六盘山盆地烃源岩的地球化学特征
3.
Formation and modification history of the Liupanshan basin on the southwestern margin of the Ordos block and tectonic stress field evolution;
六盘山盆地形成和改造历史及构造应力场演化
3) Minhe-Liupanshan basins
民和-六盘山盆地
1.
Minhe-Liupanshan basins are located in the same structural belt of Hexi aisle and belong to the same south edge of ancient continent in north of China,among them Liupanshan basin is the eastward-extending part of the basins in Hexi aisle,both of them have very good geological conditions of petroleum.
民和-六盘山盆地同处河西走廊构造带,同属华北古大陆的南缘,六盘山盆地是河西走廊诸盆地的东延部分,二者地处我国东部构造域和西部构造域的过渡带,都有着很好的石油地质条件,喜山期的旋卷构造,不仅产生了盆地群内盆地的轴向自北西向近南北向的偏转,在盆地内也产生了相应的旋卷构造变形,早期的钻探都集中在靠近旋扭核部,都产生了"口口见显示,口口不流油"的现象。
4) Beishan Basins group
北山盆地群
1.
The Jurassic to Cretaceous sedimentary systems and their distribution and evolution in the Beishan Basins group;
北山盆地群侏罗、白垩系沉积体系及其分布、演化
5) Beibuwan Basin
北部湾盆地
1.
Prediction of reservoir permeability with improved artificial neural network principle:taking the Southwest Weizhou Depression in Beibuwan Basin as an example;
改进人工神经网络原理对储层渗透率的预测——以北部湾盆地涠西南凹陷为例
2.
Distribution and Composition of Biomarkers in Crude Oils from Different Sags of Beibuwan Basin;
北部湾盆地不同凹陷原油生物标志物分布与组成特征
3.
A discussion on hydrocarbon accumulation dating determined by homogenization temperature and burial history of fluid inclusions——An example from the Fushan depression,Beibuwan basin;
由流体包裹体均一温度和埋藏史确定油气成藏时间的几个问题——以北部湾盆地福山凹陷为例
6) the Beibuwan Basin
北部湾盆地
1.
It was indicated that there were two different inversion structures formed in two period based on analysis of seismic profiles in Weixi exploration region of the Beibuwan Basin.
在系统分析北部湾盆地涠西勘查区地震剖面的基础上,认为北部湾盆地涠西勘查区发育两期反转构造即渐新世末期及中新世末期反转构造。
补充资料:北部地方
北部地方
旧译“澳北区”。澳大利亚联邦的一个直属行政区。位于大陆中北部。面积134.7万平方公里。人口15.8万(1991),其中土著居民2.9万(1984)。首府达尔文。北部阿拉弗拉海沿岸曲折低平,东北部为巴克利高原,中西部为平原草地,南部为山地和沙漠地区。北部阿纳姆地为土著居民保留地。约五分之四面积位于热带内,普遍高温,大部地区年平均雨量不足510毫米。最大河维多利亚河,流注帝汶海。西南部多干涸盐湖。麦克唐奈山脉的齐尔山为本区最高峰。采矿业重要,主要有锰、铜、金、铋和铝土矿,其次为锡、银、铅、锌和铀。七十年代又发现几处铀矿藏。肉牛饲养为基本经济部门。主要城镇有艾丽斯斯普林斯、膝南特克里克等。
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