该类型构造形成于加里东期末，是该区加里东造山期后隆升背景的产物。
This kind of structure is the product under background of the uplift in Caledonian postorogenic phase formed at the end of the Caledonian Stage.
具“S”型花岗岩的特征，互相呈脉动侵入接触关系，形成于板内同造山期的环境。
It has features of "s" granite and as pulsation intrusion contact and formed the intraplate synorogenic period setting.
造山带核部上中地壳存在着规模很大的岩浆岩体的显示，与造山期后的地质作用有关。
The manifestations of large-scale magmatic intrusions occurring in the upper-mid crust in the cores of the orogenic belt were related to post-orogenic geological processes.
加里东期在东秦岭—大别造山带南侧江汉平原地区存在一个继承性古隆起，前人所称的“鄂中古陆”是其具体的表现。
There is a inherited paleouplift in the Jianghan Plain area of the southern margin of East Qinling and Dabie Orogenic Belt during Caledonian period.
第二期为平行造山带的挤压缩短变形，形成区域透入性共轭破劈理或膝折带。
The second episode is characterized by NW-SE direction compression-shortening deformation with formation of two conjugate fracture cleavages or kink bands.
白垩纪造山活动再次加强，盆地处于第二个发育期。
In Cretaceous, while the orogenic activity strengthened once more, the basin was in the second developing period.
喜山期残存盆地深埋，石炭系仅零星残存在造山带的低洼地带。
The residual basins were deeply buried in Himalayan Period, and the Carboniferous System was piecemeal distributed in the depressed belts of orogenic zone.
喜山期残存盆地深埋，石炭系仅零星残存在造山带的低洼地带。
The residual basins were deeply buried in Himalayan Period, and the Carboniferous System was piecemeal distributed in the depressed belts of orogenic zone.
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