1) Variscan
华力西期
1.
The main orebody of every ore area and metallized occurrence around it in ShengingguanDongpu Au metallogenetic zone are distributed along the Variscan uncomformable 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。
2.
The middle and late Variscan granite distributes widely in the Qimantage region, Eastern Kunlun.
通过对祁漫塔格地区华力西期花岗岩类型、空间分布、地质地球化学特征的研究表明 ,该区花岗岩分布最广的是华力西中、晚期花岗岩。
2) middle Variscan stage
华力西中期
3) late Caledonian mineralization
华力西晚期成矿
4) Late Caledonian Early Variscan
加里东晚期-华力西早期
5) Late Variscan
华力西晚期侵入岩
1.
Located on the northern margin of Qaidam massif,the Tanjianshan gold deposit occurs in the carbonaceous mylonite schist of Wandonggou Group of Mesoproterozoic Jixian System as well as in the Late Variscan intrusive rocks.
滩间山金矿床产于中元古界万洞沟群碳质糜棱片岩和华力西晚期侵入岩中。
6) Caledonian-Hercynian-Indosinian
加里东期-华力西期-印支期
补充资料：西华葛帔
1.《南史．任昉传》:"﹝昉﹞子西华冬月葛帔练裙﹐道逢平原刘孝标﹐泫然矜之﹐谓曰:'我当为卿计。'"因作《广绝交论》以讥其旧交。后因"西华葛帔"指人情势利﹐交道不终。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条