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1)  Aluminous A-type granite
铝质A型花岗岩
1.
Discovery of the Siling aluminous A-type granite in Hangzhou and its tectonic significance;
杭州泗岭铝质A型花岗岩的发现及其构造意义
2.
The determination and a preliminary study of Sujiquan aluminous A-type granites in East Junggar, Xinjiang;
新疆东准噶尔苏吉泉铝质A型花岗岩的确立及其初步研究
3.
Geochemistry of aluminous A-type granites along Darabut tectonic belt in West Junggar, Xinjiang;
新疆西准噶尔达拉布特构造带铝质A型花岗岩的地球化学研究
2)  aluminous A-type granitic porphyry
铝质A型花岗斑岩
1.
The dating of zircon from Donggou aluminous A-type granitic porphyry determined by SHRIMP yields an age of 112±1 Ma.
采用SHRIMP锆石U-Pb测年技术,对东沟含矿铝质A型花岗斑岩体进行了年代学研究,获得成岩年龄为112±1Ma;采用ICP-MS法测定东沟钼矿中辉钼矿Re-Os同位素年龄,获得模式年龄为116。
3)  peraluminous granite
过铝质花岗岩
1.
The Yinieke agan granite mass consists of muscovite-bearing peraluminous granites occurring as a compound mass composed of adamellite and moyite.
伊涅克阿干花岗岩是含白云母过铝质花岗岩,由二长花岗岩—钾长花岗岩分3次侵入组成的复式岩体。
2.
The effect of phosphorous on liquidus temperature of peraluminous granite was experimentally studied in rapid-quenched cold+ sealed vessels(RQV) at 100 MPa in this paper.
以宜春414岩体中的钠长花岗岩作为实验初始物,利用"RQV-快速内冷淬火"高温高压装置实验研究了100MPa压力、含5%H2O条件下,P对过铝质花岗岩液相线温度的影响。
4)  strongly peraluminous granites
强过铝质花岗岩
1.
Phase equilibrium constraint on the generation of the Indosinian strongly peraluminous granites in central Inner Mongolia,and their geodynamic setting;
内蒙古中部印支期强过铝质花岗岩的相平衡约束及动力学背景
5)  A-type granitics gneiss
A型花岗质片麻岩
6)  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。
补充资料:福建南平铝厂铝型材氧化着色生产线


福建南平铝厂铝型材氧化着色生产线


谱瘫 福建南平铝厂铝到材萄廿善在片亦“.
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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