1) palaeohigh of southern middle Guizhou province
黔中古隆起
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) middle Guizhou uplift
黔中隆起地区
5) Central Guizhou lift
黔中隆起西、南缘
1.
There are little studies concerning mineralization characteristics of bauxite in Longli-Huishui-Nayong region,south of Central Guizhou lift.
黔中隆起西、南缘的龙里—惠水—纳雍一带铝土矿成矿一直研究程度低,通过对龙里高坡场、纳雍董地含铝岩系研究,发现龙里铝土矿属于潟湖相沉积,部分铝土矿被第四纪风化形成坡积物产出;纳雍董地为冲积扇沉积铝土矿。
6) Central paleouplift
中央古隆起
1.
The northern one is called the Yimeng paleouplift, and the south-central one, the Central paleouplift.
基底结构复杂,具有明显的不均匀性,基底顶面表现为2个大型隆起,北部为伊克昭盟隆起,中南部为中央古隆起。
2.
To reveal the formation mechanism of the Carboniferous slender-waist-shaped central paleouplift in Ordos Basin,a series of stress-strain simulations were carried out,in which the basin was simplified into an isopachic,isotropic and elastic shell model and loaded with the NS trending extrusion.
将鄂尔多斯盆地简化为受南北挤压的等厚各向同性弹性薄板模型进行应力—应变场数值模拟,力图揭示鄂尔多斯地区石炭纪出现的细腰状中央古隆起的形成机制。
3.
The authors think that the central paleouplift in the Ordos basin was formed under the nearly E W lateral compressive stress produced by the collision and amalgamation of the Qilian trough and the Ordos basin in early Palaeozoic time.
运用板块构造理论,对鄂尔多斯盆地西缘和南缘的地质背景和构造变形特征进行分析,认为鄂尔多斯盆地中央古隆起在早古生代由祁连海槽与鄂尔多斯盆地碰撞拼贴产生的近东西方向的侧向挤压应力作用而形成。
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。
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