granite magma信息详情
花岗岩岩浆
magma───n.[地质]岩浆;糊剂;n.(Magma)人名;(英)马格马
granite───n.花岗岩;坚毅;冷酷无情
silicic magma───硅质岩浆
cooled magma───冷却岩浆
fayalite granite───辉橄榄花岗岩
phonolite magma───响岩岩浆
basaltic magma───[地质]玄武岩浆
orbicular granite───圆形花岗岩
scrub granite───磨砂花岗岩
The ore forming material and media came from the strata of the Taihua Group and its lower strata, the granite magma and Mesozoic lake basin.───成矿物质及介质来源于太华群及下部地层、花岗岩浆和中生代湖盆。
metallogenic mechanism is as follows: in the latest Jurassic, the melting layers of granite magma in the lower crust were formed by the regional plate movement.───成矿机理是:区域板块运动使本区在侏罗纪末下地壳形成花岗岩浆熔融层。
Beside fractional crystallization model, liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.───除了结晶分异模式外,富氟花岗岩浆液态不混溶作用也是伟晶岩成岩成矿的重要机制。
It was the moving of hydrothermal of granite magma that caused enrichment of REE in tectonic rocks.───矿区强烈的花岗岩岩浆汽热活动造成构造岩的稀土明显富集。
Yanshanian granite magma intrusion activities, and with the tungsten, tin, rare metal mineralization is very close relationship.───燕山期花岗岩浆侵入活动最盛,且与钨、锡、稀有等金属成矿关系极为密切。
The mineralizing material was origin from the Morich granite magma which partial melted from Proterozoic Dabie gneissic complex.───成矿物质来源于元古宙大别片麻杂岩部分熔融而形成的富钼花岗岩浆。
Beside fractional crystallization model, liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
- granite state college
- granitic crust
- granite system
- granitic ichor
- granitic juice
- granitic magma
- granitic mass
- granitic layer
- granitic rock
- granitegear
- granitic plaster
- granitic melt
- granitic pocket
- granitic shell
- granitic texture
- granitic vein
- granitics
- granitine
- granitoid texture
- grannum
- granitogene