1) Early Himalayan
喜山早期
2) Himalayan period
喜山期
1.
Among which, endogenetic deposits were formed during Himalayan period, distribute mainly in Geladandong mountain with strong Himalayan magamatism and mineralization may be related to magmatic hydrothermal activities; Antimony deposits usually occurred in and controlled by the souther.
对区内铁、锑、铜、银多金属及石膏、水晶等主要矿产的矿化特征和成矿条件进行了总结,指出铁、铜、银多金属和水晶等内生矿产主要分布在岩浆活动较强烈的各拉丹冬地区,矿化与岩浆侵位过程中的热液活动有关;锑矿分布于该区南部的NW向断裂中,是藏北美多锑矿带的组成部分,矿化受断裂控制明显,为低温热液充填型;上述矿化形成于喜山期,与藏北地区新生代构造岩浆热事件相耦合。
3) Early Yanshanian
燕山早期
1.
Tectonic-Magmatic Mechanisms of the Two Types of Early Yanshanian W-Sn-Polymetallic and Pb-Zn-Polymetallic Deposit Assemblages in Southeast Hunan;
湘东南燕山早期钨锡与铅锌多金属矿床组合形成的构造-岩浆动力学机制
2.
Important significance of regional tectonic regime to metallogenic capacity of Indosinian and Early Yanshanian granites in southeastern Hunan:A case study of Qianlishan and Wangxianling plutons;
区域构造体制对湘东南印支期与燕山早期花岗岩成矿能力的重要意义——以千里山岩体和王仙岭岩体为例
3.
Some Further Discussions on the Genetic Type of the Early Yanshanian (Jurassic) Granitoids in the Nanling area,SE China;
南岭燕山早期花岗岩成因类型的进一步探讨
4) early Yanshanian period
早燕山期
1.
Strong crustal movement and tectono magmatic activity of early Yanshanian period occurred in the Kuancheng Qinglong Jinchangyu gold deposit concentrated region of east Hebei Province,and resulted in the formation of major regional compressional shear faults and magmatic zones and more than 20 gold deposits.
冀东宽城－青龙－金厂峪金矿集中区早燕山期地壳运动与构造－岩浆活动强烈，形成了区内ＮＥ向、ＥＷ向与ＮＷ向压扭性－扭性主干断裂构造－岩浆带与２０多个金矿床。
6) modification during Himalaya movement
喜山期改造
补充资料：春喜友人至山舍
【诗文】：
鸟鸣春日晓，喜见竹门开。路自高岩出，人骑大马来。
折花林影断，移石洞阴回。更欲留深语，重城暮色催。
【注释】：
【出处】：
全唐诗：卷503-56
鸟鸣春日晓，喜见竹门开。路自高岩出，人骑大马来。
折花林影断，移石洞阴回。更欲留深语，重城暮色催。
【注释】：
【出处】：
全唐诗：卷503-56
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