1) Huanan uplift
桦南隆起
1.
The relationships between Huanan uplift and its surrounding basins,such as Sanjiang Basin,Hulin Basin,Boli Basin,Jixi Basin,Shuangyashan Basin and Shuanghua Basin,are playing an important role in the regional oil and gas resources exploration and development.
黑龙江省东北部三江、虎林、勃利、鸡西、双鸭山、双桦等盆地与桦南隆起的关系对本区油气资源的勘探开发有重要的意义。
2) southeast uplift
东南隆起
1.
The pool-forming pattern in the condition of arching in the southeast uplift in Songliao Basin;
松辽盆地东南隆起区长期隆升背景下的油气成藏模式
3) Jiangnan Uplift
江南隆起
1.
Rare Earths of Magmatic Rocks of Yanshanian Stage in Adjacent Region of Anhui and Jiangxi Province, Jiangnan Uplift;
江南隆起带皖赣相邻区燕山期岩浆岩稀土对比研究
2.
Hydrocarbon Accumulation and Petroleum Formation in the Northern Margin of Jiangnan Uplift;
江南隆起北缘油气成藏带解剖及成藏规律探讨
3.
The tectonic setting of granitoids of Yanshanian Stage in the south of Anhui Province and the northeast of Jiangxi Province in Jiangnan Uplift is studied.
对比研究了江南隆起带皖南地区与赣东北地区燕山期花岗岩类形成的构造背景。
4) Jiaonan uplift
胶南隆起
1.
The eclogite bearing high pressure metamorphic belt in the Jiaonan uplift is the eastward extension of the Dabie ultra high pressure belt.
胶南隆起含榴辉岩高压变质带为大别超高压带的东延部分。
2.
Based on the detailed field regional geological mapping and research of microscopicstructures, as well as systernatic strain measurement of deformed mineral, a large-scaleleft-lateral normal slip ductile shear zone in the north margin of Jiaonan uplift is delimited.
在详细的野外地质填图的基础上,通过各种尺度的构造研究和系统的应变测量,确定了胶南隆起北缘中段的大型左行正滑韧性剪切带的存在及其延展范围,并提出了确定韧性剪切带边界的构造几何学准则。
5) southeast uplift
东南隆起区
1.
Application of analytic hierarchy process for hydrocarbon resource evaluation of faulted depression-an example from southeast uplift in Songliao Basin;
运用层次分析法进行断陷油气资源评价——以松辽盆地东南隆起区为例
2.
Southeast uplift, located in the southeast of Songliao Basin, is an extremely special and important structure unit.
本论文在总结前人研究资料的基础上,通过资料收集,数据分析,根据盆地模拟的原理和方法对研究区7口井进行了剥蚀量计算和埋藏史恢复,在此基础上对该区构造演化进行了分析,并将东南隆起区构造演化史分为初始裂陷期、断陷发育期、断坳转换期、坳陷发育期、坳陷期后构造反转期和构造萎缩期六个阶段,同时对主要时期的构造样式进行了分析研究。
6) Wunansha Uplift
勿南沙隆起
1.
Structural movement in Wunansha Uplift of offshore of Lower Yangtze is much weaker than onshore.
南黄海盆地勿南沙隆起受构造运动影响较弱,盖层保存良好,构造相对完整,该区A构造有地震含气异常,其周围还发育了一批背斜,是下扬子地台油气勘探的方向。
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