| 释义 |
VariscanBNC³²³⁹⁵
基本例句
华力西期
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。 cnki
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。 cnki
The basement of Mesozoic volcanic rocks in Fujian Province is mainly in the Caledonian fold system and is laid over the Variscan-Indosinian sedimental cover.
中生代火山岩的基底主要为加里东褶皱系，其上还有华力西—印支期沉积盖层； cnki
The deformation strata mainly are Statherian strata, mesoproterozoic strata, fore- Carboniferous strata, Variscan granite and granodiorite, etc, Constitution style is a parallel banded DSZ.
变形地层主要为长城系、蓟县系变质岩系、前石炭系博霍特组和华力西期花岗岩及花岗闪长岩等，其组成形式为平行带状韧性剪切带。 cnki
The main orebody of every ore area and metallized occurrence around it in ShengingguanDongpu Au metallogenetic zone are distributed along the Variscan unconformable contact.
胜境关东铺金成矿带矿田各矿区段主要矿体或外围矿化点，均沿华力西期不整合面分布。 dictall
After the closing of the two riftS in the late Variscan, the crust was compressed strongly and the tectonic effect within the plate occurred after a series of thrust- nappe structures collided.
华力西晚期两个裂谷闭合后，中上部地壳强烈水平挤压，产生一系列逆冲-推覆构造等碰撞期后极内构造效应。 cnki
Dongjiangkou and Zhashui rock bodies are located in south side of Shangdan fault zone, which belong to Variscan batholith.
南秦岭东江口、柞水岩体位于南丹断裂带南侧，为华力西期岩基。 dictall
During Middle- Late variscan intense tectonic- magmatic activity took place with Au-Gu mineral resources.
华力西中-晚期的构造岩浆活动强烈，并伴生有金、铜等多种矿产。 cnki
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。 cnki
It follows that the Variscan tectonic development is characterized by the intermittently active ancient land and steady transgressions in the study area.
由此可见，古陆间歇性活跃、海浸持续稳定是本区华力西期构造发展的基本特点。 cnki
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。 dictall
The diabase, lamprophyre, granite porphyry and quartz veins are formed after Variscan period.
辉绿岩、煌斑岩、花岗斑岩及石英脉形成于华力西期以后。 cnki
The Houdidong Au deposit occurred in the Permian, Kedao Formation contact zone between metamorphic rock series and Variscan gabbro body.
后底洞金矿床产于二叠纪柯岛组变质岩系与华力西期辉长岩体内外接触带。 chemyq
The result of the systematic, isotopic dating clearly shows that the Qinling Mountains are a Caledonian, Variscan, Indosinian, and Yanshanian polycyclic composite orogen.
同位素年代学的系统研究结果，充分反映出秦岭是一个加里东、华力西、印支、燕山多旋回复合造山带。 cagsbulletin
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。 geophy |