沉降带 meaning in Chinese
geotectogene
su idencezone
subsidence zone
subsiding belt
zone of subsidence
zoneofsu idence
Examples
- In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric , karst region controlled by folded structures near depressed belts and blinded karst region in fault basins
目前开展的可有效利用的地下水资源调查评价将该区划分为隆起带裸露岩溶分布区、沉降带边缘褶皱构造控制岩溶分布区和断陷盆地隐伏岩溶分布区。 - During late mesozoic and cenozoic , extensions were widespread in eastern china and adjacent areas . the induced compressions and extensions , uplifting and subsidence as well as large - scale magamatism , increased the pre - existing ne - nne trending faults , uplifts and subsidence belts . this is how ; the giant transform structure led to the formation of xihu depression
在晚中生代与新生代，拉张作用广泛分布于中国东部及邻区，导致了挤压与拉张、隆起与沉降以及大规模的岩浆作用，于是使早先存在的北东北北东向断层、隆起带与沉降带增强，这也是大的转换断层形成西湖凹陷地层的机理。 - In this case during paleozoic , nearly east west trending arc structures resulted from the interaction between china plate and siberian plate . in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault , diaoyudao fault , okinawa fault , uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate
本文所涉及近东西向展布的弧形构造形成于古生代时期中国板块与西伯利亚板块的碰撞带，而在中生代，中国板块下的kula - pacific板块向西俯冲导致了北北东向和北东向构造（如duimadao断层、 diaoyudao断层、 okinawa断层、隆起带和沉降带）以及位于中国板块东部的火山岩浆带。