3) the regional booming area
区域经济隆起带
1.
It is a significant attempt not only to built up the regional booming area for solving the economic development and its long-term growth in some undeveloped countries and regions,but to fill in the blank in the development of the economic system.
区域经济隆起带构建既是解决欠发达国家和地区经济发展和长期增长的一种有益的尝试,更是发展经济学自身理论体系需要研究和完善的一个理论空白。
5) uplift belt
隆起带
1.
Control of the Early Faulted Depression of Superimposed Basins on Uplift Belts and Depression Belts——A new explanation for the origin of uplift belts and depression belts in the northern Qaidam Basin;
叠合盆地早期断陷对隆起带与凹陷带的控制——柴北缘隆起带与凹陷带的成因新认识
6) palaeohigh belt
古隆起带
1.
The Carboniferous natural gas in eastern Sichuan is of cracked gas which had been accumulated, originally as oil, in Liangping-Changshou palaeohigh belt that was formed by Indosinian movement.
川东石炭系中的天然气属于油型气,初为原油,曾经聚集于印支运动中形成的梁平—长寿古隆起带里,形成油藏。
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