crustal architecture meaning in Chinese

地壳结构
地壳隆起结构

The geological and geophysical studies show that there are large discrepancies for the distribution , strike - slip direction and tectonic styles of the faults in the southern and northern parts of the qinghai - xizang plateau , and for the deep crustal architectures in the eastern and western parts of the southern plateau
摘要青藏高原南部与北部的断裂带走滑方向不同，断裂带在高原东、西两侧的展布规律和构造运动方式也存在极大的差异。
To calculate this boundary parameter , mohorovicic discontinuity palaeo - heat flow value during basin evolution process is identified through geotectonic background analogy method based on " peeling " method model , and the basin basement palaeo - heat flow is calculated through inversion from today to antiquity with current tectonic structure as constraint condition for palaeo - crustal architecture analogy
为了求取这个边界参数，以“剥层”法模型为基础，通过大地构造背景类比法确定盆地演化过程中莫霍面古热流值，以现今地壳结构为约束条件类比古地壳结构，从今至古反演求取了盆地基底的古热流。