1) alkaline rock
碱性岩
1.
LA-ICP-MS zircon dating of the alkaline rocks and lamprophyres in Gejiu area and its implications;
云南个旧锡矿田碱性岩和煌斑岩LA-ICP-MS锆石U-Pb测年及其地质意义
2.
Based on contrast study with the Dongping gold deposit in Hebei Province and Maoniuping REE deposit in Sichuan Province,it is concluded that the two deposits are related to alkaline rocks whose isotopic ages ranging from 256Ma to 290～380Ma and the Ganshahe REE deposit shows the characteristics of porphyry deposit.
对产于北祁连中段冷龙岭一带的青分岭金矿和干沙河稀土矿地质特征和控矿因素进行了概述 ,并将其与国内典型的河北东坪金矿和四川牦牛坪稀土矿进行对比研究 ,认为它们的成因与碱性岩有关 ,且干沙河稀土矿具有斑岩型矿床的特征。
3.
Dongping gold deposit is associated with alkaline rocks.
东坪金矿是与碱性岩有关的金矿床 ,其矿石矿物 ,尤其是金矿物具有与众不同的特征。
2) alkaline rocks
碱性岩
1.
Discovery of late Early Triassic alkaline rocks in the Gankugou area, northwestern Qiangtang, Tibet, China;
西藏羌塘西北部干枯沟地区早三叠世晚期碱性岩类的发现
2.
In recent years, significant advances have been made, including the further classification of the deposit, the evolution of the ore-forming fluid, the age determination of the ore precipitation, and the relationship of the deposit with alkaline rocks, and with porphyry and other types of ore deposits.
近年来对该类型矿床的深入研究 ,包括对该类矿床的进一步分类、流体形成演化、成矿时代、与碱性岩之间的关系 ,以及与斑岩型及其他类型矿床之间的内在联系等方面均取得了重要进展。
3.
In this paper,the author assured the concept of gold deposits associated with alkaline rocks,discussed the characteristics,origin and evolution,and the paragenetic relationship to calc alkaline rocks of the alkaline rocks related to gold mineralization,analysed the tectonic setting of alkaline rocks and their related gold deposits.
厘定了碱性岩型金矿床的概念 ,总结了与金矿床有关的碱性岩特征 ,从地球动力学角度 ,分析了碱性岩及其有关矿床形成的构造环境 ,讨论了碱性岩的起源演化及其与钙碱性岩共生的内因。
4) alkali ne magmatic rock
碱性岩浆岩
6) alkali series
碱性岩类
1.
Geological setting and main features of alkali series in Panzhihua-Xichang region are outlined.
概述了攀西地区碱性岩类产出的地质背景，岩体的主要特征。
补充资料：碱性岩
| 碱性岩 alkalic rock 火成岩的一种 。二氧化硅含量较低 ，碱质含量较高（Na2O＋K2O＞ Al2O3 ） 。一般呈浅灰 、浅绿或浅红色。主要浅色矿物为碱性长石（微斜长石、正长石、钠长石），暗色矿物为霓石、霓辉石、钠铁闪石、钠闪石等，副矿物有方钠石、锐钛矿和磷灰石等。可分为深成碱性岩，如霞石正长岩；浅成碱性岩，如霞石正长斑岩；喷出碱性岩，如响岩等。一般产在地壳构造运动较弱的稳定地区，很少形成独立岩体，多与基性岩、超基性岩、碱性正长岩、碳酸岩一起形成杂岩体。与之有关的矿产有铌、锆、稀土、铁、钛、磷等。可利用其钾含量高、二氧化硅含量低的特点，制作化肥和陶瓷原料。 |
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