2) continent-continent collision
陆-陆碰撞
1.
A mathematical model of a simple continent-continent collision;
基于板块陆-陆碰撞的主要物理特性,经过合理简化,提出了陆-陆碰撞的起始阶段的几种模式,并就一类简单的陆-陆平直正撞建立了相应的数学模型及边界条件,得到岩石圈在变形时褶皱产生的力学条件,为定量研究陆-陆碰撞的地质过程提供了理论基础。
3) Continental collision
陆陆碰撞
1.
This sequence consisted of volcanic rocks of shoshonite series resulted from late continental collision.
西天山艾肯达坂地区较好发育了艾肯达坂组红色陆相火山岩建造,它不整合在下石炭统大哈拉军山组之上,未经变形和变质,属于陆陆碰撞晚期的橄榄安粗岩系,其年龄确定是厘定从碰撞造山向陆内构造演化的关键。
4) collision zone between two continental plates
陆-陆碰撞带
1.
67 in collision zone between two continental plates.
67),陆-陆碰撞带玄武岩的Th/Nb>0。
5) point-collision between two continents
陆-陆点碰撞
6) continental collision
大陆碰撞
1.
A retrospective and perspective view on continental collision and ultrahigh-pressure metamorphism;
大陆碰撞和超高压变质研究:进展和展望
2.
Sedimentary response to tectonic events: Reconstructed spatio-temporal scale of the Indo-Asian continental collision and Qinghai-Xizang Plateau uplift;
构造事件的沉积响应——建立青藏高原大陆碰撞、隆升过程时空坐标的设想和方法
3.
Recent studies considered that the former′s formation was resulted from the accretion of continental margins, occured in Late Riphean, Middle Late Cambrian, Middle Late Ordovician, and Middle Late Silurian; and the later consists of Variscan and Indosinian fold belts, resulted from the continental collision.
近年来的研究认为前者是由于陆缘增生作用而形成的，增生作用发生于晚里菲，中—晚寒武世，中—晚奥陶世和中—晚志留世；后者包括华力西和印支褶皱带，是大陆碰撞的产物。
补充资料：蔡陆仙
蔡陆仙
蔡陆仙 近代医家。江苏丹徒县人。其生平欠详，尝著有《中国医药汇海》、《民众医药指导丛书》计二十四种，行于世。
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