1) Tazhong uplift
塔中隆起
1.
Hydrocarbon accumulation and distributional characteristics of the Silurian reservoirs in the Tazhong uplift of the Tarim basin;
塔里木盆地塔中隆起志留系油气成藏及分布特点
2.
K-Ar isotopic dating of authigenic illite and its application to the investigation of hydrocarbon accumulation history of the Silurian bituminous sandstone reservoirs in the Tazhong uplift,Tarim basin;
塔中隆起志留系沥青砂岩油气储层自生伊利石K-Ar同位素测年研究与成藏年代探讨
3.
Multi-source and multi-stage hydrocarbon accumulation and exploration strategy of the Silurian reservoir in Tazhong uplift;
塔中隆起志留系混源多期油气聚集特征与勘探对策
2) central Tarim uplift
塔中隆起
1.
Tectonic evolution and its bearings to the oil and gas with in the central Tarim uplift of the Tarim Basin,Xinjiang;
塔里木盆地塔中隆起构造演化与油气关系
2.
Late Ordovician palaeogeomorphology and its sedimentary facies characteristics in central Tarim uplift
塔中隆起晚奥陶世古地貌及其沉积相特征
3.
Biota of the Lianglitag Formation(Lower Katian,Upper Ordovician)from the Central Tarim Uplift(Xinjiang,western China)include mainly microbialites,calcareous algae,foraminifera,sponges,corals,bryozoans,ostracodes,trilobites,gastropods,brachiopods,crinoids etc.
塔中隆起区的良里塔格组含菌藻类微生物岩、植物类的钙藻、原生动物中的有孔虫、后生动物中的海绵、珊瑚、苔藓虫、介形类、三叶虫、腹足类、腕足动物、棘皮动物等化石门类。
3) the Tazhong Low Uplift
塔中低隆起
5) Tazhong paleo-uplift
塔中古隆起
1.
The Tazhong paleo-uplift is a multiple oil-gas accumulation play,and medium-large scale reservoirs have been found in the Carboniferous,Silurian,Ordovician and Cambrian Systems.
塔中古隆起复式油气聚集区在石炭系、志留系、奥陶系及寒武系均发现了大中型油气藏。
6) the midwest of Tabei uplift
塔北隆起中西部
1.
The plane and profile geological models at the end of Neocene in the midwest of Tabei uplift are established on the basis of seismic data of oil field and tectonic analysis.
根据油田地震资料解释和构造分析,建立了新近纪末塔北隆起中西部平面与剖面地质模型,通过线弹性有限元方法的计算,得出该地区应力场模拟结果。
补充资料：大兴隆起
北京活动构造带。斜贯北京小平原中部，呈北东走向，隐伏于地表之下。面积约为1300平方公里。大兴区域大部处于隆起的中部。其西北侧为北京凹陷，东南侧为燕郊－牛堡屯断裂、大厂凹陷，两侧分别以南苑－通州断裂带及永乐店－夏垫－马坊断裂带为界。南段与南各庄－长子营断裂、廊固凹陷为邻。隆起西北高而东南低，高点埋深仅几十米，位于黄村镇与南苑镇之间，形成于第三纪，上覆50～1000米左右的第三系和第四系地层，内幕是由中上元古界和古生界组成的蓟县系、青白口系、寒武系、奥陶系地层。次级背斜轴部在高点东向，约在榆垡－马驹桥一线。新生界地层由西北向东南逐渐加厚。大兴隆起的两侧有次一级的断裂下降活动，与北京凹陷相应，形成地垒式的构造。隆起的上部地表呈平原地貌形态。
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