1) Wutai granite-greenstone belt
五台花岗-绿岩带
1.
In Wangjiahui granitic pluton of Wutai granite-greenstone belt, gneissiosity and lineation structures were formed in the late stage of magmatic emplacement, when the pluton was a Bingham body.
五台花岗－绿岩带中王家会花岗质深成岩体中普遍发育的片麻理、矿物线理等内部构造是岩浆侵位晚期岩体处于宾厄姆体状态下形成的流动变形构造。
2) granite-greenstone belt
花岗绿岩带
1.
The deformation and metamorphic processes of mylonites in the granite-greenstone belt of Seerteng area, Inner Mongolia;
内蒙古色尔腾山地区花岗绿岩带糜棱岩变形变质过程探讨
3) Wutai greenstone belt
五台绿岩带
1.
The volcanic exhalative rocks of Baiziyan Formation in Wutai greenstone belt is composed of basic mid acid volcanic rocks, tuffs and tourmaline and flogopite bearing quartz marble, in which gold deposit occurs.
五台绿岩带柏枝岩组火山喷气岩由基－中酸性火山岩及其凝灰岩和含电气石、金云母的石英大理岩组成，其中赋存有金矿床。
4) granitoid-greenstone belts
花岗岩-绿岩带
1.
area underwent Neoarchean granitoid-greenstone belts forming,Paleoproterozoic rifting,Mesoproterozoic volcanism and Mesozoic magmatism totally four-times important events, which have relation with copper and gold mineralization.
西南段以新太古代花岗岩-绿岩带的地质事件为主,并叠加较为发育的中生代岩浆活动,成矿以金为主,其次为铜。
5) Jiaodong granite-greenstone terrain
胶东花岗-绿岩带
6) Wutaishan greenstone belt
五台山绿岩带
1.
Dongyaozhuang gold deposits is in Wutaishan greenstone belt.
在五台山绿岩带中的东腰庄金矿 ,发现部分容矿绢云母石英 (片 )岩实为变质基性岩 (变质辉绿岩—辉绿玢岩或安山玢岩 )岩床在五台期构造作用下发生强烈的剪切变形和变质热液蚀变的产物。
2.
Study on mineralogy, petrology, mineral deposit geology and determining prospecting criteria of such type gold deposit have great significance to prospecting they in Wutaishan greenstone belt.
东腰庄金矿位于山西省五台县境内,是五台山绿岩带金矿中发现的一种新型式的金矿床类型。
补充资料：台花
台花 主要用金属薄片胶贴于漆器上，然后用刀刻出花纹，填上彩漆，再涂髹底漆打磨推光显出银色图案，有台白花、台填、台彩之别。此法是福州著名漆艺家李芝卿所创，俗称“老虎尿”。
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