1) south and north slope of protrusion
隆起南北斜坡
2) the north slope of Fuxin uplift zone
扶新隆起带北坡
3) The North Slope of Chengning Uplift
埕宁隆起北坡
1.
The north slope of Chengning uplift is one region which has huge prospect potential in Huanghua depression in Neogene.
埕宁隆起北坡是黄骅坳陷新近系具有较大勘探潜力的地区,研究其沉积与层序特征对于油气勘探和开发有重要的现实意义。
4) southern margin of Katake uplift
卡塔克隆起南坡
1.
Well Zhong-2 is the first and foremost important exploring well for identification of structure of platform margin and reservoir of reef-shoal of Lianglitaga Formation of the Upper Ordovician,southern margin of Katake uplift.
中2井是卡塔克隆起南坡的第一口以查清卡塔克隆起南缘下古生界碳酸盐岩台缘结构、探索良里塔格组礁滩相孔洞缝储集体为目的区探井。
5) Tabei uplift
塔北隆起
1.
Sequence division,sedimentary characteristics and reservoir characteristics of Jurassic in Tabei uplift;
塔北隆起侏罗系层序划分及沉积、储层特征
2.
Characteristics and evaluation of Mesozoic and Cenozoic clastic reservoirs in the Tabei Uplift;
塔北隆起中、新生界陆相碎屑岩储集层特征及评价
3.
New knowledge and exploration thought about Mesozoic traps in west of Tabei uplift, Tarim basin;
塔里木盆地塔北隆起西段中生界圈闭新认识与勘探思路
6) Jinbei uplift
晋北隆起
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