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一种由石英和云母构成的花岗石。A granitic rock composed chiefly of quartz and mica.

成矿作用主要与中侏罗世—晚侏罗世的花岗质岩浆活动相关。Mineralization is mainly related to Mid-Late Jurassic granitic magmatism.

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中生代大规模花岗质岩浆活动是金向上迁移的主要载体。Large scale granitic magma during Mesozoic was the major carrier for gold.

花岗石的几何尺寸、色差问题由于天然原因，不易解决。Granitic geometrical dimension, color due to natural causes, not easy to solve.

花岗石的几何尺寸、色差问题由于天然原因，不易解决。Because problem of granitic geometrical dimension, chromatism is natural reason, masty.

锡石在花岗质熔体中的溶解度，是阐明花岗岩全岩型锡矿成因的关键。One of the key problems in its origin is the solubility of cassiterite in granitic melt.

就像淹没在寓言里的朝圣者失去了内心中花岗岩般坚硬的那部分。Like pilgrims in a fable swallowed up and lost among the inward parts of some granitic beast.

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本文的目的是帮助普通旅游者识别花岗质岩石及其重要意义。This paper is used to help general tourists to recognize granitic rocks and their importance.

用岩相学方法研究浙江花岗岩的交代作用。Metasomatism of the granitic rocks in Zhejiang Province, China is investigated by petrography.

它们的成因系列应归属于壳幔混源型。The genetic series of these granitic rocks may belong to that of mixed crust-mantle derivation.

玲珑花岗质杂岩是一个多期次形成的复式岩体，最终定位于燕山期。Linglong granitic complex is a polyphase composite rock body, emplaced finally in Yenshan stage.

岩脉是沿着裂断系统侵入的，裂断系统以冷却火山岩与花岗岩质岩石形式形成。Dykes were intruded along a fracture system that formed as the volcanic and granitic rocks cooled.

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不同的造山旋回伴有相应的花岗岩。It was recognized that different orogenic cycles were accompanied by corresponding granitic rocks.

花岗质岩浆虽然起源于地壳，却是受地幔热引擎的驱动。The granitic magma generated in the crust, but the generation is driven by the mantle thermal engine.

花岗质岩石主要由石英、斜长石和碱性长石组成，并因此具有较低的密度。Granitic rocks mainly consist of quartz, plagioclase and alkaline feldspar and hence have lower densities.

古田-小陶花岗质杂岩体是由小陶、古田、华家、蛟洋和姑田等单元组成。The Gutian-Xiaotao granitic Complex is composed of the Xiaotao, Gutian, Huajia, Jiaoyang and Gutian units.

因此，花岗质岩石也记录了大量地球深部过程的信息。So, granitic rocks recorded a great of information about the geological processes in the depths of the earth.

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花岗岩-体氧同位素交换反应绝大多数为开放体系不平衡类型。The mineral-fluid oxygen isotope exchange in granitic rocks is mainly a non-equilibrium one in an open system.

这种矿床的晶质铀矿是从花岗岩浆分异出来的富铀岩浆中结晶而成的。Uraninite in this type of deposit is crystallized by U-rich magma which is differentiated from granitic magma.

科学家们一直认为英安岩可以从玄武质的岩浆中分离出来形成花岗岩，但他们从没奢望能在可操作的情况下看到这一过程。Scientists have long believed that dacite can separate from basaltic magma to form granitic rocks. But they'd never