２１００公里南北向深层地震反射剖面反映的中印度洋板内缩短Ｎ．Ｃｈａｍｏｔ－Ｒｏｏｋｅ等自中印度洋被确认为是大洋岩石圈活动压缩变形的场所以来，人们已经竭尽全力来确定该地区的缩短量。其目的是了解在很高压应力下的板内变形会对周围板块的运动学起什么作用以及大... 2100 km deep north-south seismic reflection profile reflects the shortening of the Indian Ocean plate. Since the Mid-Indian Ocean, Chamot-Rooke, etc., has been identified as a site of compressive deformation of oceanic lithosphere activity, every effort has been made to determine the amount of shortening in the area. Its purpose is to understand what effect of intraplate deformation under high compressive stress will have on the kinematics of the surrounding plate and ...