2) Beisantai area
北三台地区
1.
Through partitioning of the Cretaceous stratum in Beisantai area, the relationship of Cretaceous “bottom conglomerate” ages and their distribution features were classified.
本文通过对北三台地区白垩系层序单元的详细划分 ,理清了白垩系“底砾岩”的时代关系和分布特征 ,确定出各层序单元的沉积相类型及其展布 ,并探讨了本区白垩系的成藏条件和有利勘探目
2.
Rich carbazole compounds, including carbazole, alkylcarbazoles, benzocarbazoles and alkylbenzocarbazoles, were detected by GC/MS in lacustrine oils from Beisantai area, Junggar Basin.
准噶尔盆地北三台地区北 82井、北 83井和沙 10 8井湖相原油咔唑类化合物的分布特征表明 ,油气运移作用是影响该区原油中咔唑类化合物分布的重要因素。
3) Taiwan
[英][tai'wæn] [美]['taɪ'wɑn]
台湾地区
1.
A Case Study on Eco-City Development Assessment in Taiwan;
台湾地区生态城市发展评价案例
2.
Regulation Mechanism Analysis of Nurse Professionist in Taiwan;
我国台湾地区护理人员体系及管理制度分析
3.
Regulation Mechanism Analysis of Professional Pharmacist in Taiwan;
我国台湾地区药学专业人员管理制度分析
4) Hongtai area
红台地区
1.
Logging Evaluation for Low Porosity and Low Permeability Reservoir in Hongtai area in Tuha Basin;
吐哈盆地红台地区低孔、低渗储层测井评价
2.
Analysis of Middle-Jurassic seismic facies in Hongtai area of Tu-Ha basin;
吐哈盆地红台地区中侏罗统地震相分析
3.
Sandstone reservoir microscopic characteristics of braid delta of Hongtai area in Tuha Basin;
吐哈盆地红台地区辫状河三角洲砂岩储层微观特征
5) Toutai area
头台地区
1.
Sedimentary characteristics of Fuyu oil layer in Toutai area of Songliao basin;
松辽盆地头台地区扶余油层沉积特征
6) Yingtai area
英台地区
1.
Logging interpretation standard and its application in Putaohua reservoirs in Yingtai area;
英台地区葡萄花油层录井解释标准及应用
2.
antitatively evaluating the control function of sedimentary microfacies on reservoir physical properties-taking Qingshankou formation and sandstone member I of the fourth member of Quantou formation in Yingtai area as an example.;
沉积微相对储层物性控制作用的定量评价——以英台地区青山口组、泉头组四段Ⅰ砂组为例
3.
Development of mm-level mud-films and significance for reservoirs in Yingtai area,Daqing Oilfield
大庆英台地区毫米级泥膜发育特征及储集意义
补充资料：阿拉伯台地
| 阿拉伯台地 Arabian Platform 西亚阿拉伯半岛主体部分。地跨沙特阿拉伯、也门、叙利亚、伊拉克、约旦5国。西起红海沿岸的希贾兹山脉，东至阿曼湾岸的哈杰尔山脉，北至叙利亚中央高地，南达亚丁湾岸的也门高地。面积250万平方千米以上。为古老平坦地台，核心部分位于沙特阿拉伯的内志高原。台地自寒武纪以来，几乎未受到褶皱变动，古地质时代的沉积岩层基本保持平整。台地面海拔1200～2500米，地势自西南向东北缓倾。第四纪大规模的断裂运动，造成大量岩浆喷出，致使台地西部被深厚的熔岩所覆盖。属热带荒漠气候，表面沙漠广布，河道干涸，仅在地下水抬升处有零星绿洲。较大沙漠有鲁卜哈利沙漠、内夫得沙漠、代赫纳沙漠等。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条