地壳增厚 meaning in English
crustal thickening
Examples
- Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward , which evolved from late jurassic to cretaceous . the extensional simple shear model of the chagan fault depression is established . the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure
讨论了查干凹陷及邻区中-新生代盆地构造演化及其地球动力学特征，三叠纪(印支期)为陆内造山作用与地壳增厚、隆升剥蚀阶段；侏罗纪(燕山早期)为造山后造山带的局部伸展垮塌阶段；白垩纪(燕山晚期)为造山期后大规模伸展垮塌作用与伸展盆地的发育阶段；新生代(喜山期)为远距离碰撞效应与弱挤压挠曲性质的稳定大陆内坳陷的发育阶段。 - In the light of new findings in geological studies and recent development in lithospheric delamination theory and numerical modeling experiments , we have come to the conclusion that the above - mentioned differences are caused by the crustal thickening and oblique collision prior to the hitting of the indian continent toward the eurasian continent
在充分利用高原地质研究最新成果的基础上，提出印度次大陆向欧亚大陆碰撞前地壳增厚及斜向碰撞是造成上述地质现象的根本原因，并由此对青藏高原构造演化的一些特点作了新的解释和探讨。