Variscan orogeny 华力西造山运动
Variscan mountains 华力西山地
Late Variscan 华力西晚期侵入岩
Variscan stage 华力西阶段
mid-late Variscan 海西中晚期
middle Variscan stage 华力西中期
Variscan Unconformable Contact 华力西不整合面控矿
Hailar basin is a fault-depressed basin formed on Variscan folded basement.
海拉尔盆地是在华力西褶皱基底上形成的中生代断陷盆地。
The development of the fractures and the distribution of basic rocks of Variscan age are also mentioned.
指出了该区断裂发育及华力西期基性岩的分布情况。
The most important metallogenic granitoid intrusions are mainly formed in Mesozoic, secondly late Variscan period.
已知成矿的花岗岩类侵入体主要为中生代岩体，其次为晚古生代华力西期岩体。
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