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。
They are fault metamorphic rocks formed in thrusting nappe structure inside continental plate during Variscan-Indonian Stage.
它们是华力西—印支期板内逆冲推覆构造所形成的断裂变质岩。
The intermediate-co-acrid hypabyssal intrusive rock of middle to later Variscan epoch to Indosinian epoch had close relation with gold metallization.
华力西中晚期—印支早期中酸性浅成相侵入岩类与金成矿关系密切。
The Chaganuoer copper deposit is located near the assembly belt of Siberian plate and North China plate, and within the tectonic-magma belt of late Variscan.
查干诺尔铜矿床产在西伯利亚板块和华北板块汇聚带附近，华力西晚期构造岩浆带内。
The Chaganuoer copper deposit is located near the assembly belt of Siberian plate and North China plate, and within the tectonic-magma belt of late Variscan.
查干诺尔铜矿床产在西伯利亚板块和华北板块汇聚带附近，华力西晚期构造岩浆带内。
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