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1) Daping gold deposit
大坪金矿
1.
Concentration of platinum group elements(PGE) of various gold ores and around rocks and Re-Os isotopic compositions of major ore minerals of Daping gold deposit were analyzed by using an inductively coupled plasma mass spectrometry(ICP-MS) with nickel sulfide fire assay pre-concentration and carius tube decomposing technique with acetone extracted Re method.
采用镍硫火试金ICP-MS法和Carius管溶矿与ICP-MS联合测定法分析了云南大坪金矿各类金矿石和主要围岩的PGE和矿石矿物的Re-Os同位素组成,结果显示各类金矿石的ΣPGE变化较大,为(3。
2.
Mineralization epochs of the Daping gold deposits are divided into three stages:the early stage or scheelite-bearing quartz vein stage,the major stage or massive polymetallic sulphide typed auriferous quartz vein stage and the late stage or carbonate-quartz stage.
大坪金矿成矿可分为三个成矿阶段:早期成矿阶段(白钨矿石英脉)、主成矿阶段(团块状多金属硫化物含金石英脉)和晚成矿阶段(碳酸盐石英脉)。
2) Daping gold mine
云南大坪金矿
1.
Noble gases isotopic composition of fluid inclusions in scheelites collected from Daping gold mine,Yunnan province,China,and its application for ore genesis.;
云南大坪金矿白钨矿惰性气体同位素组成及其成矿意义
3) Dongping Gold Mine
东坪金矿
1.
The application of filling technique of filling-mining method in Dongping Gold Mine;
东坪金矿充填采矿法充填工艺的实践
4) Dongping gold deposit
东坪金矿
1.
The faults of various times coincided with,and rebuilded by the ore-formation in the later mineralizing process,and became the ore-occurrence structures of the Dongping gold deposit.
运用里德尔 (Riedel)剪切裂隙理论 ,在东坪金矿构造区域内划分出若干种剪切类型。
2.
4 Ma, showing a significant time gap as compared with the ore-forming age of the spatially closely related Dongping gold deposit.
本文对与东坪金矿有密切空间关系的上水泉花岗岩进行了单颗粒锆石U－Pb同位素定年，结果为135。
3.
The natural gold from Dongping gold deposit is various in morphological characteristic,mainly in form of inclusion gold and fissure gold with large grain size (0.
东坪金矿自然金形态多样，主要以包裹金和裂隙金为主。
5) Jinjiaping manganese deposit
金家坪锰矿
1.
Through analyzing regional geological setting and geological characteristics in Jinjiaping manganese deposit,it is supposed that the formation of manganese deposit in this area is divided into such 4 stages as continental facies,marine facies,solidification-dehydration-crystallization of ore-forming materials,the deposit is classified into marine sedimentation-sub-recomposed deposit.
通过对该区区域地质背景及金家坪锰矿地质特征的分析,认为该锰矿石形成可分为陆相期、海相期、成矿物质固化失水结晶期及成矿后裂隙充填期4个阶段。
6) Dongping gold deposit
东坪金矿床
1.
Geological features and ore-hunting orientation of Dongping gold deposit,Hebei Chongli;
河北崇礼东坪金矿床地质特征及找矿方向
2.
Study on the typomorphic characteristic of pyrite in Dongping Gold Deposit and their geologcal significance;
河北东坪金矿床黄铁矿标型特征研究及其地质意义
补充资料：大坪霁雪
大坪，危耸于黑白二水之间，一峰突起。位于峨眉山的中部，左与华严顶、长老坪、息心所、观心坡诸山，比肩相望；右有天池、宝掌、玉女、呼应诸峰，四绕回环；牛心顶鼎峙于前；九老洞屏临于后，海拔1450米。 山势险峻，孤峰脊岭，仅东北两侧各有一陡坡上下，东面蛇倒退险，北面猴子坡高，悬崖绝壁，行者如走在刀背之上，罕见人迹。峰顶平坦，林木蓊郁，云霞幻变。相传大坪有五奇：“猴回娘家”、“蛇不咬人”、“黑虎巡更”、“乌鸦请客”、“仙姑弹琴”（弹琴蛙）。而自然风光还有一奇，即“大坪霁雪”，为峨眉山十景之胜。 每年秋未，金顶开始飘雪；立冬一过，大坪已是雪花 满山飞舞，纷纷扬扬，一株株挺立的常绿乔木，如琼枝玉叶，白塔凌空。严冬时，峨眉山处 处雪树冰花，全山宛似银色世界。明代四川嘉定诗人蔡祯的《三峨雪霁》云：“三峨天下壮，秀色接青?。绝?千秋雪，危峰百仞银。日临观宝气，云敛见仙人，中有蓬莱客，丹砂远俗尘。”吴祖光在《雾里峨眉》一文中评说：“雪景最大特点是白雪压在绿枝上。在别的地方的冬天，雪下只有枯萎了的枝条”。经过一冬雪花的浓妆淡抹，大坪和周围的群峰，变成洁白的一片净土。赵循伯的《峨眉山》一书描述大坪冬景说：“冬季晴雪初霁，杉条掩盖，咸如瑶树琪花。仰视则九岭冈如屏风九叠，横遮天半；俯眺青莲、白云、宝掌、天池诸峰，玉琢银妆，弥望一白，备极幽峭精绝之胜。晴雪初霁，仁立在大坪以上高海拔的山峰上，鸟瞰大坪是另一番“幽峭精绝”的冬景。大坪和环绕四周的群峰，组合成一朵庞大的雪莲花：大坪如同花芯，丛丛参天古树活象花蕊，周围的峰峦宛似一裂裂花瓣。这朵洁白的雪莲花，正展瓣吐蕊，盛开在峨眉山的腹部，盛开在广阔无垠的天地之间；冬阳下，白中泛红，温润晶莹，冷艳妖娆。倘若在后山的霁雪亭，倚阑静观，举目回望，游者如同身处于雪莲花之，飘然有羽化成仙之感。”大坪霁雪“，凝聚着峨眉雪的形色美。宋代诗人白约在其《游峨杂咏》中叹曰：“岩静长留雪，山寒故放花。”
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
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