1、

Geological mapping methods of granites are defined by granite classifications.

花岗岩类的分类理论决定其填图方法.

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2、

The rapakivi granites have a number of petrological peculiarities.

环斑花岗岩具有若干岩石学的特征.

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3、

Petroloyical and geochemical characteristics suggest that Jinningian granites in Alongshan area were formed in thesys-collisional setting.

岩石学岩石地球化学特征表明具岩浆成因特点,形成于同碰撞构造环境.

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4、

Maksym : There are a lot of beautiful granites in Ukraine.

Maksym: 乌克兰有很多很漂亮的花岗岩.

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5、

The ore-forming material transfered from Taihua group to Huashan andSongpinggou granites , and deposited into orefield finally.

成矿物质由太华群运移到花山花岗岩和蒿坪沟花岗岩,最终形成矿田.

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6、

They are in fact metamorphosed rocks , predominantly schist , amphibolites, granites and sand stones and Muruwa Precambrian.

事实上,它们主要由地片岩、闪岩 、 花岗岩和细沙,小石头变质而来.

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7、

The pinetrees in various shape are rooted in granites cracks. The deeper into mountain andpinetrees are.

黄山松之奇,主要在于生长在坚硬的花岗岩缝隙中, 形态多姿,“入山愈深,则松愈古、形愈奇”.

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8、

Fufang granites are exposure in the middle section of the west slop of Wuyi Mountain.

付坊花岗岩出露在武夷山西坡中段.

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9、

Ore-forming metals maybe mostly derived from the granites.

花岗岩浆是成矿物质来源和成矿热源.

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10、

A-type granites keep abreast of I-type and S-type granitites, and are animportant genetic type.

与I型和S型花岗岩一样, A型花岗岩也是一种重要的成因类型.

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11、

S-type granites should not be considered as the evidence of plume magmatism.

不能把S - 型花岗岩作为地幔柱岩浆作用的证据.

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12、

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.

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13、

Igneous topazites found recently in South China are closely associated with F-rich granites in space.

新近在华南发现的黄英岩与富氟花岗岩存在密切的时空联系.

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14、

Yali Stone has been at natural quarry exploitation and granites international trade more than ten years.

雅利石材,十余年来专注于天然石材矿山的开发和石材荒料的国际贸易.

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15、

Wear mechanism of diamond segments while sawing granites is analyzed.

分析了锯切花岗石过程中金刚石节块磨损机理.

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16、

The granites and granite-porphyry of late Yanshan provided with the-forming thermal condition and part of-forming materials.

燕山晚期花岗岩、花岗斑岩为成矿的热动力条件,并提供了部分成矿物质.

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17、

Granites belong to S-type granite, but the biotite granite was affected by the mantle or mantle fluid.

黑云母花岗岩是壳源花岗岩但又受到幔源岩浆或幔源流体的影响。

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18、

On the basis of detailed studies of geochemistry and zircon geochronology, there existed agenetic link among the basement rocks, migmatites and granites in NW Fujian Province.

详细的地球化学及锆石年代学研究表明,闽西北地区基底变质岩-混合岩-花岗岩存在成因联系。

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19、

Decoration Rock Materials from Nantianmen& Characteristics of Mid-Coarse Grained potassic Granites

南天门的饰面石材&中粒钾质花岗岩特征

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20、

Late Hercynian intrusions are dominated by acid granites with small amount of diorite.

华力西晚期以酸性花岗岩为主,另有少量闪长岩.

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