Taiping granodiorite in south Anhui provence is a typical syntexis type (or I type) granitoid.
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 (？)
The Geda Village weathered granitoid resources have the good development value with rich and high quality.
伊通县爱民乡疙瘩屯麦饭石资源丰富且品质优异，具有良好的开发价值。
Granitoid composition is controlled by tectonic Settings, magma sources, initiation and evolution processes.
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。
The other intrusive bodies are post-orogenic granitoid in association with the continental uplifting and rifting.
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 most important metallogenic granitoid intrusions are mainly formed in Mesozoic, secondly late Variscan period.
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。
Being an important pluton in the western part of Altay orogen, Tielieke pluton shows arc granitoid characteristics.
铁列克岩体是阿尔泰造山带西段的一个重要的岩体，显示弧花岗岩特征，其侵位时代一直没有解决。
Therefore, granitoid is one of the most difficult topics in geology due to its complex sources and formation processes.
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。
Deferent plutons composing Linglong composite granitoid batholith have deferent degrees of anisotropy of magnetic susceptibility.
组成玲珑花岗岩基的各个岩体具有不同的磁化率各向异性度。
Therefore, the granitoid is a big group of plutonic rocks including such as granodiorite, monzonite, syenogranite, tonalite, and so on.
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。
Granitoid intrusions are received to have the potential to offer metal elements when mineralized by the analyses of ore-controlling factors.
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。
The Hueichizi granitic pluton consists mainly of granitoid rocks. which have in common deformation fabric and complicated deformation processes.
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 previous lithodemic units of Mesozoic granitoid in east Guangxi are discussed based on the dividing principle and method of granitoid hierarchy.
运用花岗岩类等级体制划分的原则和方法，对前人建立的广西东部中生代花岗岩类岩石谱系单位的相关问题进行讨论。
The emplacement mechanism for granitoid, magmas is determined by rheological behaviour of the magma and the host rock as well as the tectonic, environment.
花岗质岩浆的上升、侵位机制除取决于岩浆与围岩的流变性质外，也受构造环境的制约。
The extent of ree enrichment and differentiation is affected by ree concentrations and distributions in the primary granitoid rocks, weathering degree, etc.
REE在风化壳中富集分异受风化壳发育程度、花岗岩原岩中ree含量及其分布和分配的影响。
According to the analyse of petrochemistry, microelement, lanthanon and cause of formation type of rock body, sum up the all sequences are S-type granitoid .
经岩石化学特征、微量、稀土元素地球化学特征研究以及岩体成因类型图解判别，获得五个序列岩体均为S型花岗岩的认识；
In this thesis, we research into the geochemical data of the groundwater from the granitoid weathering crust of the fogang granite in baisha region, guangdong province.
本文研究了广东省白沙地区花岗岩风化壳地下水的水化学特征，特别是与花岗岩的风化过程有关的稀土元素含量及其分布模式。
The process of generation and differentiation of granitoid magmas is con trolled not only by physical-chemical condition, but also is related to regional tectonic event.
花岗质岩浆的生成、分异过程不仅与物理-化学条件有关，而且受控于区域构造。
The enrichment and differentiation of REE in granitoid rocks during weathering-leaching processes, may lead to the formation of a natural continuous ion-chromatographic column.
花岗岩中的稀土元素在风化淋滤作用下发生富集和分异，形成REE的天然离子色谱层。
In northern Liaoning Province, there exists a great area of Archaean granitoid, which is dual-evolutionary, and represents a tonalitic-trondhjemitic(TT) trend and a calc-alkali(CA) trend.
辽北地区大面积出露的太古宙花岗岩是奥长花岗岩和钙碱性岩浆双重演化趋势的复合产物。
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。
The Fogang granitoid complex is the largest Late Mesozoic batholith in Nanling region, and the Wushi diorite-hornblende gabbros are the most basic end-member of Fogang calc-alkaline series rocks.
佛冈花岗杂岩体是南岭地区最大的晚中生代岩基，乌石闪长岩角闪辉长岩是佛冈钙碱性系列花岗岩中最基性的端员。
Cordillera type has a close relationship with high-temperature metamorphism and accompanied the emplacement of granitoid, giving rise to isothermal decompression and then isobaric cooling pT-t paths.
科迪勒拉型伸展与高温变质作用关系密切，伴随花岗质岩体的侵位，并使变质岩系近等温减压之后近等压冷却。
Cordillera type has a close relationship with high-temperature metamorphism and accompanied the emplacement of granitoid, giving rise to isothermal decompression and then isobaric cooling pT-t paths.
科迪勒拉型伸展与高温变质作用关系密切，伴随花岗质岩体的侵位，并使变质岩系近等温减压之后近等压冷却。
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