1) tuberous
隆起的
2) Mature and upheaval basement
成熟并隆起的基底
3) uplift
隆起
1.
Formation of Paleo-uplift and Petroleum Occurrence in Tarim Basin;
塔里木盆地古隆起的形成和油气控制
2.
Discussion for Origin Hydrocarbon Potential of the Central Uplift in Bayanhaote Basin;
巴彦浩特盆地中央隆起带成因机制及油气远景初探
3.
Xiahe area is located in the northern part of the central Bachu uplift in the Tarim Basin.
夏河地区位于塔里木盆地巴楚隆起中段的北部,20世纪90年代以来,巴楚隆起南缘相继发现了一批以构造圈闭为主体的油气藏。
4) heave
隆起
1.
This paper studies the displacement rule of tunnel under excavation,the influence of time and space on the heave during the excavation,and proposes the affection coefficient of time and of excavation width as well.
为此研究了处于软土基坑之下的地铁隧道的位移变化规律 ,分析了基坑工程中时间、空间效应对隆起的影响规律 ,提出了时间、开挖宽度影响系数 ,推导出考虑基坑施工影响的隧道位移变形的实用计算方
5) upheaval
隆起
1.
An inquiry into the problem of upheaval in the bottom of the deep foundation pit;
对深基坑坑底隆起问题的探讨
2.
The reasons of the bottom plate s upheaval,rupture, the reinforced concrete posts displacements and fractures in the clean-water pool and the rupture of the diversion wall of a waterworks are investigated and analyzed.
对某水厂清水池底板严重隆起、开裂,池内钢筋混凝土柱子严重位移、断裂,导流墙开裂破坏的原因进行了调查分析。
3.
The results show that the upheaval of the excavation using the top-down method is about 1/3 compared with the excavation using the bottom-up method.
分析结果表明:逆作法施工的带有抗浮抗拔桩基坑的坑底隆起量约为顺作法施工的带有抗浮抗拔桩基坑的坑底隆起量的1/3。
6) paleo-uplift
古隆起
1.
Accumulation and distribution of oil and gas controlled by paleo-uplift in poly-history superimposed basin;
多期叠加盆地古隆起控油规律
2.
Formation mechanism and tectonic types of intracratonic paleo-uplifts in the Tarim basin;
塔里木盆地克拉通内古隆起的成因机制与构造类型
3.
The Research on Ordovician Sedimentology and Reservoir Property of Leshan～Longnvsi Paleo-uplift in Centre Sichuan Area;
川中地区乐山～龙女寺古隆起奥陶系沉积、储层特征研究
参考词条
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。