1) Mojiang Ni-Au deposit
墨江镍金矿床
2) Mojiang gold deposit
墨江金矿
1.
Geochemistry of depositional environment of siliceous rocks from Mojiang gold deposit in Yunnan Province;
云南墨江金矿床硅质岩沉积环境的地球化学探讨
2.
The physico and chemical characteristics and origin of ore forming fluid are discussed though the study of fluid inclusions in gold bearing quartz veins in the Mojiang gold deposit shed light on the ore genesis and prospective.
结合氢氧锶和稀有气体同位素研究 ,认为墨江金矿成矿流体曾发生过部分地幔流体、大气降水等多种类型水不充分的混合 ,水岩反应和多种流体混合可能为墨江金矿矿质迁移沉淀主要机制。
3.
The characteristics of geology and gold mineralization of the Mojiang gold deposit in the Ailaoshan orogenic belt are compared with those of the Mindyak gold deposit in southern Ural orogenic belt.
本文通过对产于两个不同造山带中金矿化特征的对比 ,认为墨江金矿与明加克金矿均具有造山带型金矿的一些特征 ,形成于造山晚期主构造带的逆冲走滑阶段 ,产于一级构造带的上盘 ,金矿化受二级和三级剪切张裂隙的控制。
3) mineralogical compositions
镇江金矿床
4) Jinchuan Ni-Cu deposit
金川镍铜矿床
6) Ni-Mo polymetallic deposit
镍钼多金属矿床
1.
The Ni-Mo polymetallic deposit in northwestern Hunan is highly enriched by Ni, Mo, Ptgroup elements and As, SE, and etc.
上述地球化学特征表明了湘西北镍钼多金属矿床的形成特征。
2.
A variety of elements,mainly Ni,Mo,Cu,Zn,Pd,Pt,Se,Ba,V and P,form a special association and are enriched in Ni-Mo polymetallic deposits in Northwestern Hunan.
湘西北镍钼多金属矿床富集了多种元素，形成一个以Ｎｉ、Ｍｏ、Ｃｕ、Ｚｎ、Ｐｄ、Ｐｔ、Ａｓ、Ｓｅ、Ｂａ、Ｖ、Ｐ为主的特殊元素组合；微量元素Ａｓ、Ｓｅ、Ｂａ等成１０１～１０３倍富集。
补充资料：金壶墨
1.晋王嘉《拾遗记．周灵王》﹕"浮提之国﹐献神通善书二人﹐乍老乍少﹐隐形则出影﹐闻声则藏形。出肘间金壶四寸﹐上有五龙之检﹐封以青泥﹐壶中有墨汁如淳漆﹐洒地及石﹐皆成篆隶科斗之字。记造化人伦之始……及金壶汁尽﹐二人刳心沥血﹐以代墨焉。"后因以指精良之墨。
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参考词条