山体岩石为加里东期花岗岩和大理石，距今4——6亿年。
Rock Hill Caledonian granite and marble ago 4-6 billion years.
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.
加里东期断裂控制了加里东岩溶储层的发育，由此预测了加里东期岩溶储层的发育区带。
Based on the domination of Caledonian faults on the development of Caledonian karst reservoirs, this paper predicts the development area of Caledonian karst reservoirs.
鄂尔多斯盆地南部加里东期风化壳储集层的分布主要受岩溶古地貌、风化壳层位及沉积相控制。
The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies.
这些发现为研究本区加里东期的大地构造环境和变形特点、扬子板块与华南板块的相互作用提供了新资料。
These findings provide new information for the study of the Caledonian tectonic setting and deformation features in the area and the interaction between the Yangtze and South China plates.
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.
研究区主要发育加里东期—海西期近EW、NE向、NW向断裂，为油气运移提供良好的通道，同时控制着圈闭的形成与发育。
The faults in work area are mainly in EW, NE, NW and formed during Caledonian-Hercynian, offering favorable channels for petroleum's migration and controlling the formation and growth of traps.
该区经历了六个构造形变期，以相当于 主加里东期的第二期（D_2）与喜马拉雅期的第五期（D_5） 形变期最为重要。
The area has undergone six stages of tectonic deformation with the second episode of Caledonian Movement (D_2) and the fifth episode of Himalayan Movement (D_5) as the most important ones.
晚加里东-海西期花岗岩侵入体与金矿密切相关；
The formation of gold mine is closely related to the intrusive bodys of granite, which are formed between later Caledonian and Hercynian.
晚加里东-海西期花岗岩侵入体与金矿密切相关；
The formation of gold mine is closely related to the intrusive bodys of granite, which are formed between later Caledonian and Hercynian.
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