石英是花岗岩类岩石的主要矿物。
花岗岩类记录了祁连地块与秦岭地块碰撞的重要证据。
The important evidence of plates collision of the granitoids are recorded between Qilian and North Qinlingin.
中国花岗岩类的出露面积，约占我国陆地总面积的10％。
The exposed area of granitoids in China represents about 10% land area of this country.
大别山高-超高压变质带中的变质花岗岩类是碱性花岗岩。
The metagranitoid found in the high ultrahigh pressure metamorphic belt ( HP UHPMB ) in the Dabie Mountains is alkali meta granite.
依据12265个样品求出中国花岗岩类的总平均化学成分；
The total average chemical composition of granitoids in whole China is calculated with 12265 samples.
寄主花岗岩在矿物地球化学上对微花岗岩类包体有明显的制约。
The mineralogy and geochemistry of enclaves are evidently controlled by their host granites.
控矿因素分析表明该区花岗岩类侵入体具有提供成矿金属的潜力。
Granitoid intrusions are received to have the potential to offer metal elements when mineralized by the analyses of ore-controlling factors.
岩石属于大陆板内张性构造环境下高侵位形成的壳源重熔型花岗岩类。
The rocks are crustal remelting, shall level granites formed in a within-plate tensional tectonic environment.
环斑花岗岩是一种特殊结构的花岗岩类，并且多数产在元古宙克拉通中。
Rapakivi granite, a special kind of granite with rapakivi texture, mostly occurs in Proterozoic cratons.
皖南太平花岗闪长岩为一典型的同熔型花岗岩类(或I型)，其I (？)
Taiping granodiorite in south Anhui provence is a typical syntexis type (or I type) granitoid.
花岗岩类的成分既受构造背景控制，又与岩浆来源、起源和演化过程有关。
Granitoid composition is controlled by tectonic Settings, magma sources, initiation and evolution processes.
其余各岩体是本区造山后与大陆抬升作用以及大陆裂谷作用有关的花岗岩类。
The other intrusive bodies are post-orogenic granitoid in association with the continental uplifting and rifting.
已知成矿的花岗岩类侵入体主要为中生代岩体，其次为晚古生代华力西期岩体。
The most important metallogenic granitoid intrusions are mainly formed in Mesozoic, secondly late Variscan period.
对比研究了江南隆起带皖南地区与赣东北地区燕山期花岗岩类形成的构造背景。
The tectonic setting of granitoids of Yanshanian Stage in the south of Anhui Province and the northeast of Jiangxi Province in Jiangnan Uplift is studied.
对比研究了江南隆起带皖南地区与赣东北地区燕山期花岗岩类形成的构造背景。
Rare Earths of Magmatic Rocks of Yanshanian Stage in Adjacent Region of Anhui and Jiangxi Province, Jiangnan Uplift;
灰池子岩体主要由花岗岩类岩石组成，该岩体岩石普遍具变形结构，变形过程较复杂。
The Hueichizi granitic pluton consists mainly of granitoid rocks. which have in common deformation fabric and complicated deformation processes.
通过对虹螺山一带酸性花岗岩类副矿物的研究，获得了一些岩体含钼性的矿物学标志。
The study of accessary minerals in acidic granitoids from the Hongluoshandistrict, has revealed some mineralogical markers of molybdenum-bearing potential of certain rock bodies.
花岗岩类的常量化学成分，属高钾钙碱性系列花岗岩类，具同熔型或i—型花岗岩的特征。
The petrochemistry composition belongs to high potassium Ca-alkaline series, showing the special feature of syntectic or I-typed granite.
因此，花岗岩类是地质学最复杂的话题之一，因为其源区岩石多种多样和形成过程非常复杂。
Therefore, granitoid is one of the most difficult topics in geology due to its complex sources and formation processes.
花岗岩类演化序列表征了造山带花岗岩成分定向演化的规律，是陆壳增生和其成熟度渐高的例证。
The sequence shows the directional compositional evolution of granitoids in a collisional orogen, which illustrates the vertical and lateral crust growth and the enhancement of crustal maturity.
花岗岩类演化序列表征了造山带花岗岩成分定向演化的规律，是陆壳增生和其成熟度渐高的例证。
The sequence shows the directionally compositional evolution of granitoids in a collisional orogen, which illustrates the vertical and lateral crust growth and the enhancement of crustal maturity.
本文所称的花岗岩属花岗岩类岩石，包括变质-混合花岗岩、酸性-中酸性火山岩和普通花岗岩。
The granite rocks in this paper belong to granitic rocks, including metamorphic-mix granite, acid-intermediate acidic volcanic rocks and common granite.
现行的单元-超单元填图方法是依据花岗岩类的i型、s型分类理论和同源岩浆演化理论而建立的。
The unit and super-unit mapping method in use is based on the theories of the i-type and s-type classification as well as the comagmatic evolution theory.
对沽源-多伦盆地火山岩类和花岗岩类进行了同位素地质年代学、地球化学和铀成矿条件的系统研究。
The results of systematic studies of geochronology, geochemistry and uranium metallogenic condition of volcanic rocks and granites in Guyuan-Duolun Basin are reported.
本文介绍的横岭关、北峪、永济、野庙滩、太峪和烟庄岩体是中条山古裂谷中的早元古代花岗岩类岩体。
The rock masses of HengLingguan, Beiyu, Yongji, Yiemiaotan, Taiyu and Yianzhuan are early proterozoic granide rock masses which are located in the paleo rift of Zhongtiao Mountain.
产于钨(钼锡铋)矿床密集区与花岗岩类有关的金矿床是一种具重要经济价值和找矿前景的新类型金矿床。
The gold deposit which exists in tungsten deposit compact district and relates to granite is a new type of gold deposit and is of great economy value and good exploration prospects.
揭示了不同岩石组合谱系类型成矿花岗岩类的岩浆源岩主要是地壳物质，具有地幔和地壳双重物源的特征。
It is revealed that the source of different types of metallogenetic granitic assemblages is mainly crustal materials, with mantle material adding.
因此，花岗岩类是深成岩的一个大类，包括象花岗闪长岩、二长花岗岩、正长花岗岩、英云闪长岩等这样的岩石。
Therefore, the granitoid is a big group of plutonic rocks including such as granodiorite, monzonite, syenogranite, tonalite, and so on.
详细研究了燕山东段地区花岗岩类的侵入时代、产出形式和成因类型，指出该区与花岗岩有关的三个金属成矿系列。
A close research has been carried out on the intrusion age, occurrence and genetic type of granitoid rocks in east section of Yanshan area. Three metallogenic series have been pointed out.
详细研究了燕山东段地区花岗岩类的侵入时代、产出形式和成因类型，指出该区与花岗岩有关的三个金属成矿系列。
A close research has been carried out on the intrusion age, occurrence and genetic type of granitoid rocks in east section of Yanshan area. Three metallogenic series have been pointed out.
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