1) Ailaoshan-Jinshajiang potassic alkalic rocks zone
哀牢山-金沙江钾质碱性岩带
2) Ailaoshan-Jinshajiang alkaline intrusion belt
哀牢山-金沙江富碱侵入岩带
3) Ailaoshan-Jingshajiang belt
哀牢山-金沙江带
4) Ailaoshan epi-metamorphic rock belt
哀牢山浅变质岩带
1.
Ailaoshan epi-metamorphic rock belt is distributed in Paleozoic and Mesozoic strata between Ailaoshan and Jiujia-Anding deep faults.
哀牢山浅变质岩带分布于哀牢山深大断裂与九甲—安定深大断裂之间的古生界与中生界地层中,哀牢山金矿带目前已发现的主要金矿床(点)均产于其中,金矿类型以蚀变岩型和石英脉型为主,但近年来,相继发现了一批红土型金矿。
5) Ailaoshan gold mineralization belt
哀牢山金矿带
1.
The study of composition and physico-chemical characteristics of fluid inclusions from three gold deposits hosted in the Ailaoshan gold mineralization belt indicated that the ore-forming fluid was characterized as being rich in Na+, K+, Cl-,SO2-4,F-and CO2, and belongs to the Na type solution, epi- to mesothermal in nature, moderately saline, intermediate to weak alkaline, and relatively reducing.
本文系统研究了哀牢山金矿带主要金矿床主成矿阶段石英流体包裹体的化学组成和物理化学性质。
6) Ailao Shan metamorphic belt
哀牢山变质带
1.
Ailao Shan metamorphic belt can be subdivided into two metamorphic belts from their characteristics of metamorphism and deformation, a high-grade metamorphic belt in the east and a low-grade metamorphic belt in the west.
哀牢山变质带可以划分为两种不同变质变形特点的变质带:东部高级变质带和西部低级变质带,自北东向南西依次为三条边界断裂:红河断裂、哀牢山断裂和九甲—安定断裂。
补充资料：带质境
【带质境】
（术语）三类境之一。如第六识缘五根五境，第七识缘第八识，自心所现之相分带本质之实体，犹如镜中所现之影像带持镜外之实物者。
（术语）三类境之一。如第六识缘五根五境，第七识缘第八识，自心所现之相分带本质之实体，犹如镜中所现之影像带持镜外之实物者。
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