基本释义:

环斑花岗岩

网络释义

1)Rapakivi granite,环斑花岗岩

2)rapakivi granites,奥长环斑花岗岩

3)rapakivite,更长环斑花岗岩

4)granite-porphyry,花岗斑岩

5)granite porphyry,花岗斑岩

6)hidden granite porphyry,潜花岗斑岩

用法和例句

The discovery and significance of the rapakivi granites in Gyisong,Tangra Yumco,Xizang;

西藏当惹雍错吉松环斑花岗岩的发现及地质意义

Petrological characteristics of the Doupangling rapakivi granites;

都庞岭岩体环斑花岗岩的特征

Petrography and geochemistry of the Tataleng rapakivi granite on the northern margin of the Qaidam basin,northwestern China;

柴达木盆地北缘塔塔楞环斑花岗岩的岩相学和地球化学特征

This paper introduces the connotation of rapakivi texture and geological and geochemical characteristics of rapakivi granites.

本文介绍了环斑结构的含义及奥长环斑花岗岩的地质与地球化学特征。

Experimental research on dissolution properties of Au and Pd contained in granite-porphyry;

花岗斑岩类岩石中Au、Pd溶解性状的实验研究

LA-ICP-MS zircon U-Pb dating from granite-porphyry rcoks in Xikuangbei,East Junggar,Xinjiang,China

新疆东准噶尔锡矿北花岗斑岩的锆石LA-ICP-MS U-Pb测年

The Hengjian deposit, located in the northern Xiangshan complex, is a typical representation of the uranium deposits related to granite-porphyry in the Xiangshan ore field,in which the orebodies mainly occur in the Hengjian granite-porphyry, and some in the siltstones and metamorphic rocks of the exocontact belt.

横涧矿床位于相山火山—侵入杂岩体(相山铀矿田)的北部,是相山众多与花岗斑岩有关的铀矿床的典型代表,矿体主要产于横涧花岗斑岩体中,其外接触带粉砂岩、变质岩中也有矿体分布。

Zircon U-Pb ages of granite porphyry in the South Nileike,Xinjiang;

新疆尼勒克南部地区花岗斑岩锆石U-Pb年龄

Characteristics of the Laorite Co granite porphyry in central Qiangtang- northern Tibet and its tectonic significance;

藏北羌塘中部劳日特错花岗斑岩体的特征及构造意义

The rapakivi granites have a number of petrological peculiarities.

环斑花岗岩具有若干岩石学的特征。

Characteristics and significances of rapakivi in Yichun area of Xiaoxinganling,Heilongjiang Province

小兴安岭伊春地区环斑花岗岩组合特征及其地质意义

massive coarse grained porphyritic granite

块体粗粒斑状花岗岩

Geochemistry and Tectonic Setting of the Tangjiaping Mo-riched Granodiorite Porphyry in the Northern Dabie Mountains

北大别山商城汤家坪富钼花岗斑岩体地球化学特征及构造环境

Characteristics of giant annulus stripe K-feldspar phenocryst of Gangtangcuo granitic pluton in central Qiangtang, northern Tibet, China

藏北羌塘中部冈塘错花岗岩体中环带条纹钾长石巨斑晶的特征

Earthenware with a speckled glaze resembling granite.

花岗岩花纹陶器陶器上有类似花岗岩斑点的釉料

Tectonic Environments of Granitoids in the West Kunlun Orogenic Belt

西昆仑造山带花岗岩形成的构造环境

Nd-and Sr-Isotope Study on Greenschist and Granodiorite of the Bainaimiao District,Inner Mongolia,China Nie Fengjun Pei Rongfu

内蒙古白乃庙地区绿片岩和花岗闪长斑岩的钕和锶同位素研究

The granite porphyry occurred in Tuan?Jie?Gou Gold Field is rock plant like hypabyssal/super hypabyssal intrusive mass.

团结沟金矿区花岗斑岩为岩株状产出的浅成?超浅成侵入体。

The mineral-bodies of the two mineral deposits are mainly existed in the contacting zone of granite-porphyry and adjoining rock.

两矿床的矿体主要赋存在花岗斑岩及其与围岩的接触带中。

The Petrogenesis of Tuwu Plagiogranite Porphyry from East Tianshan:Evidence from Wallrock

东天山土屋斜长花岗斑岩的成因——来自围岩的证据

Granitic tectono-magmatic assemblages mainly reflect the genetic connections between the magma types of granites and tectonic environments.

花岗岩的构造岩浆组合主要反映花岗岩的岩浆类型与大地构造环境之间的成因联系。

Gneiss is called bastard granite.

片麻岩叫作粗花岗岩。

Granite comes in large masses.

花岗岩形成巨大的岩体。

granit is S-type and its evolution sequence might begranomonzonite → muscovite-granite(outcrop) → feldspar-granit →muscovite-granite(core);

花岗岩演化顺序可能为二长花岗岩→露头白云母花岗岩→钾长花岗岩→白云母花岗岩芯。

Geochemical Characteristics Study of Yaowugou Granite Porphyry in Taipusi Qi

内蒙古太仆寺旗姚五沟花岗斑岩地球化学特征研究

LA-ICP-MS zircon U-Pb dating from granite-porphyry rcoks in Xikuangbei,East Junggar,Xinjiang,China

新疆东准噶尔锡矿北花岗斑岩的锆石LA-ICP-MS U-Pb测年

ZIRCON SHRIMP OF JURASSIC PERIOD MONZONITIC GRANITE-PORPHYRY AND THEIR TECTONIC SIGNIFICANCE IN THE YUNWU RIDE AREA,SOUTHERN XINJIANG

新疆云雾岭斑状二长花岗岩体锆石SHRIMP U-Pb年龄及构造意义