钾长花岗岩

根据不同期次钾长花岗岩在地球化学组分方面存在的差异变化，有助于了解地壳成分及地壳构造运动在时间上的演化。

There is variation of geochemical composition in the different stage moyite , which will help us to understand the evolution of the crustal composition and movement in the time .

岩石类型以钾长花岗岩为主，二长花岗岩次之。

The main rock type is moyite , and the next is monzogranite .

碱性花岗岩类，包括钠铁闪石花岗岩以及孪生的钾长花岗岩类；

The alkaline granitoid including arfvedsonite granite and assemblage moyite ;

福建不同期次钾长花岗岩的地球化学特征及其地质意义

Geochemical Features of Different-stage Moyites in Fujian Province and Its Geological Significance

浙江普陀山黑云母钾长花岗岩及其岩石包体的地球化学与岩浆混合作用

Geochemistry and magmatic mixing of the Putuoshan biotite moyites and their enclaves , Zhejiang Province

利用钾长花岗岩石材废料制备陶瓷釉料

Ceramic Glaze Preparation with K-Feldspar Granite Waste

都庞岭复式岩体由加里东期、印支期和燕山早期花岗岩组成。燕山早期侵入岩以二长花岗岩、黑云钾长花岗岩为主，其次为花岗闪长岩。

The Complex rock mass consists of Caledonian granite , Indo-Sinian granite and early Yanshanian granite .

新疆库鲁克塔格地块东南缘钾长花岗岩的地球化学特征及同位素测年

Geochemical characteristics and isotope dating of moyite at the southeastern margin of the Kuruktag block , Xinjiang , China

本矿泉水赋存岩石为硅质白云岩、灰质白云岩、钾长花岗岩和火山碎屑岩。

Siliceous dolostone , lime dolostone , moyite and volcanic detrital rocks are the mainhostrocks of the mineral water .

外环为碱性辉长岩、石英正长岩、碱长花岗岩，内环为钙碱系列的石英闪长岩-花岗闪长岩-二长花岗岩-钾长花岗岩。

The outer circle consists of alkaline gabbro , quartz syenite and alkali-feldspar granite . The inner circle consists of quartz diorite-granodiorite-adamellite-moyite of calc-alkaline series .

云英岩一种主要由石英和云母构成的花岗石燕山早期侵入岩以二长花岗岩、黑云钾长花岗岩为主，其次为花岗闪长岩。

A granitic rock composed chiefly of quartz and mica . Early Yanshanian intrusions are mainly adamellite , biotite K-feldspar granite with small amount of granodiorite .

根据成矿地质条件和找矿标志分析，指明地处褶断带构造中的钾长花岗岩分布位置，是该类矿床的找矿方向。

On the basis of the analyses on the metallogenic geological conditions and the guides of prospecting ore , the paper has pointed out that the potash feldspar granite distributed in the fold-fault belt is the prospect of exploration .

110～100Ma为早期高钾钙碱性英安岩流纹岩（伴生闪长岩花岗闪长岩）向晚期玄武岩流纹岩（伴生钾长花岗岩碱性花岗岩）过渡的转折期。

The period of 110-100 Ma is a transitional stage from the early high-K calc-alka-line dacite-rhyolite ( associated with diorite-granodiorite ) to the late basalt-rhyolite ( associated with K-feldspar granite-alkali granite ) .