1) Jiaobei tectonic uplifting
胶北隆起
1.
In the Late Proterozoic, in the Jiaobei tectonic uplifting there existed the crustal extension from NW(W) to SE(E) during the late orogenic phase.
晚元古宙，胶北隆起在造山运动后期开始发生ＮＷ（Ｗ）→ＳＥ（Ｅ）方向的地壳伸展作用，突出表现于前寒武纪结晶基底内部，持续时间很长久（自晚元古宙开始，断续到中生代印支—燕山期），具有改造期伸展作用特点，区域构造处于十分激化的状态，导致褶皱变形及大规模花岗质岩浆侵
2) Jiaobei uplift belt
胶北隆起带
1.
Low greenschist factes(epizonal) regional metamorphism in the Ponglai Group has been determined in this paper by measurement of illite crystallinity values of the Ponglai slates in the Jiaobei uplift belt,eastern Shandong.
本文应用鲁东胶北隆起带上蓬莱群板岩中伊利石结晶度值测量，确定了蓬莱群经历过低绿片岩相（浅变带）区域变质。
3) Jiaobei uplift
胶北隆起区
1.
Late Mesozoic kinematics history of the two major fault zones (the Zhaoyuan-Pingdu and the Muping-Jimo ones)in the Jiaobei uplift has been studied based on field observations,fault kinematics analysis and paleostress inversion.
基于野外观察、断层滑动矢量分析和古构造应力场反演,研究了胶北隆起区两条主要断裂带(招远-平度断裂带和牟平-即墨断裂带北段)的活动历史及古构造应力状态,结合火成岩40Ar-39Ar、SHRIMP和LA-ICPMS锆石U-Pb测年结果,确定了该区晚中生代主要构造-热事件和构造应力体制的转换时限。
4) 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
5) Jinbei uplift
晋北隆起
6) 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。
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