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1)  calc granite
钙质花岗岩
2)  calc-alkali granite
钙碱花岗岩
3)  Precambrian granitoid
花岗质岩
1.
The Precambrian granitoid pluton emplaced in the Paleoproterozoic-Mesoproterozoic Baoban Group in Gezhen area, northwest Hainan Island, south China was dated by SHRIMP U-Pb analysis assisted by CL image.
对海南岛北西部戈枕地区侵位于古中元古代抱板群花岗质岩进行了CL成像制约下的SHRIMP锆石U-Pb年龄测定,获得了1455±12Ma的U-Pb谐和年龄、1454±12Ma有利的207Pb/206Pb中值年龄。
4)  granitic rock
花岗质岩石
1.
Recommendation for the new geochemical classification scheme of granitic rocks and review for the relevant subjects;
花岗质岩石新地球化学分类介绍及有关问题评述
2.
Using LA-ICPMS,this study firstly reports magmatic zircon ages for granitic rocks from the Nansha micro-block,South China Sea.
本文首次报道了南沙微地块花岗质岩石岩浆锆石年龄。
3.
The streaky structures of granitic rock extraordinarily develop in Tiantangshan area, they can be regarded as two types as differentiated streaky structure and transpositional-compound streaky structure according to their geneses.
天堂山地区花岗质岩石中条带状构造异常发育,据成因可分为分异条带状构造和构造置换———复合条带状构造两种类型。
5)  granitic rocks
花岗质岩石
1.
Geochemistry of the Carboniferous-Permian post-collisional granitic rocks from Tianshan;
天山石炭-二叠纪后碰撞花岗质岩石地球化学研究
2.
Automatic realization of the classification for granitic rocks by computer;
花岗质岩石地球化学分类的计算机自动实现
3.
The distributive characters of Au content in granitic rocks from Au mineralized district inShenglidaban has been studied with fractal theory,The study indlcates that, during ductile shearactiveity,certain part of Au orebodies formed in this way is usually in large-scale,but Au grade isrelatively low and there is no distinct boundary between the orebody and its country rocks.
用分形理论研究了胜利达圾金矿区花岗质岩石中金含量的分布特征,得出花岗质岩石的金是在韧性剪切活动中被激化的。
6)  granitic magma
花岗质岩浆
1.
New evidence for the liquation mineralizing processes has been presented using two se-ries of experimental results in the granitic magmatic system.
花岗质岩浆体系中,钨、锡的流-熔分配和熔-熔分配实验结果为花岗质岩浆液态分离成矿作用提供了新证据,在实验范围内,钨、锡的流-熔分配系数和都很小,其最大值然而,钨、锡的熔-熔分配系数都大于1,其最大值分析估算表明,花岗质岩浆期后热液成矿作用难以形成大、中型钨锡矿床,而液态分离作用是形成钨锡矿床的主要途径。
补充资料:钙质海绵纲
钙质海绵纲
Calcarea

   多孔动物门的一纲。以具碳酸钙构成的骨针为主要特征。钙质海绵全部海产,大多生活在沿岸浅海,体型一般很小,常呈暗灰色或灰色。骨针顶端常突出体外,致使海绵呈刺状;典型的钙质海绵为辐射对称的瓶状,顶端是出水口,常被竖立的长单轴骨针围绕,称出水口繸。骨针大小不一,但在分类学上都算作大骨针,有3种基本型:单轴骨针、三辐骨针和四辐骨针,形状多种多样。钙质海绵纲分成钙质海绵亚纲和石灰海绵亚纲。
   钙质海绵在地层中的出现晚于寻常海绵(见寻常海绵纲)和六放海绵(见六放海绵纲)。
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