1) Median eminence
正中隆起
1.
Scanning electron microscopic observation on neoplasm and its development on the ependymal surface of the median eminence;
正中隆起室管膜面赘生物及其形成过程的电镜观察
2.
Central administration of Orphanin FQ inhibits GnRH secretion by ORL1 receptor in the median eminence of freely moving ovariectomized rats
中枢注射孤啡肽通过孤儿受体可抑制去卵巢大鼠正中隆起GnRH释放(英文)
3.
Methods: Immunohistochemical staining method was used to show the characteristics of TAS lining the ventral part of the ventricle Ⅲ and median eminence.
方法 :采用免疫组织化学方法 ,显示第三脑室腹侧壁和正中隆起 (ME)TAS的特征。
2) Qianzhong uplift
黔中隆起
1.
A study of hydrocarbon fluid inclusions in Qianzhong uplift and its adjacent areas;
黔中隆起及周缘地区下组合含油气流体包裹体研究
2.
Fission Track Analysis of Meso-Cenozoic Uplift and Denudation in Jinsha Area, the Qianzhong Uplift
黔中隆起金沙地区中新生代隆升剥蚀的裂变径迹分析
3.
Based on the study of the main petroleum geologic features, burial history, thermal history and pooling conditions of the typical fossil oil reservoirs and residual oil and gas pools in the Qianzhong uplift and the adjacent areas, this paper gives clear definitions of fossil oil pool and residual oil and gas pools, and discusses their modes and patterns of hydrocarbon pooling.
通过对黔中隆起及其周缘地区典型古油藏和残余油气藏的石油地质主要特征、埋藏史、热史与成藏条件等进行分析研究,明确了古油藏和残余油气藏的含义,探讨了古油藏和残余油气藏的油气成藏模式和油气成藏规律。
3) Central Guizhou Uplift
黔中隆起
1.
Marine Lower Assemblage and exploration prospect of Central Guizhou Uplift and its adjacent areas;
黔中隆起及其周缘地区海相下组合与油气勘探前景
4) 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。
5) Chuanzhong uplift
川中隆起
6) 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
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