1) quartz diorite porphyry
石英闪长斑岩
1.
Detailed field geology, mineralogy,petrology and geochemistry investigations have been made on the quartz diorite porphyry in Shaxi porphyry copper(gold) deposit,Investigation results have shown that the quartz diorite porphyry is the main ore-bearing stock of this deposit and its distribution, evolution and genesis are controlled obviously by the Tancheng-Lujiang deep fault.
详细的野外地质调查和系统的室内研究 ,揭示了石英闪长斑岩是沙溪斑岩铜 (金 )矿床的含矿岩体。
2) chlorophyr(e)
斑英闪长岩
3) quartz-diorite-porphyry
石闪长斑岩
4) quartz diorite
石英闪长岩
1.
Zircon SHRIMP U-Pb age of quartz diorite in Qagan Obo of Inner Mongolia and its geological significance;
内蒙古查干敖包石英闪长岩锆石SHRIMP U-Pb年龄及其地质意义
2.
Zircon U-Pb age of the quartz diorite in North Daqing mountains, central Inner Mongolia;
内蒙古大青山北前壕石英闪长岩锆石U-Pb年龄及地质意义
3.
The correlation has been found between An and the other27 trace elements in the gold zone of quartz diorite which belongs to plutonic primary formation.
Ａｕ与Ｃｄ等２７种微量元素的相关关系，构成石英闪长岩原生含金建造金矿带中元素地球化学规律的独特性。
5) quartz-diorite
石英闪长岩
1.
The intrusive rocks trend NE-NEE,are closely related to the Xinlin Gol complex in space and are mainly quartz-diorite and quartz-biotite-diorite.
侵入岩岩性主要为石英闪长岩和英云闪长岩。
2.
The chromium mineral is produced in a gray middle-fine grain quartz-diorite inDabanshan.
大坂山“铬矿物”产出于灰绿色中细粒石英闪长岩中,笔者从区域地质特征、岩石学、岩石化学、地球化学、同位素等方面对石英闪长岩进行了较全面的研究后认为,该套岩石成因为壳幔混合型,构造环境为北祁连加里东洋盆收缩阶段板块俯冲作用下形成的火山弧,岩石成岩时代为早奥陶世,铬矿物形成深度约30km,受区域性岩石圈断裂带控制。
3.
LA-ICP-MS dating for zircon separated from the Daqinhundi and Jinxing quartz-diorite plutons indicates that both plutons formed at 325±3Ma and 322±3Ma respectively.
本文对达其浑迪和金星石英闪长岩进行了锆石LA-ICP-MSU-Pb定年,结果表明两个岩体分别形成于325±3Ma和322±3Ma。
6) quartz mica dioritic porphyry
英云闪长斑岩
1.
Appearing as different sized rock stems and formed in middle latter part of Yanshan Period,the quartz mica dioritic porphyry is the host rock of Nong ping porphyry typed gold copper deposit.
英云闪长斑岩是农坪斑岩型金 (铜 )矿床的赋矿岩体 ,呈大小不等的小岩株 ,形成于燕山中晚期。
补充资料：斜长角闪岩
| 斜长角闪岩 amphibolite 由区域变质作用形成的一种变质岩。主要由普通角闪石和斜长石组成（两者含量大体相等），可含少量黑云母、石英、铁铝榴石、绿帘石等。具粒状、柱状变晶结构，片状，片麻状构造。可根据构造＋特征矿物＋基本名称的原则命名，如条带状石榴子石斜 长角闪岩、芝麻 点榴辉斜长角闪岩等。通常认为它形成于高绿片岩相（绿帘角闪岩相）至角闪岩相的变质条件，有时也可形成于接触变质作用。在老变质岩地区广泛发育。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条