白鎳礦 的英文怎麼說
中文拼音 [báinièkuàng]
白鎳礦
英文
white nickel ore-
In the light of tectonic evolution stage and metallogenesis, these metallogenic system ( assemblage ) could be classified as follows : ( 1 ) the pre - divergent metallogenic system in the southwest margin of north china paleocontinent in the archean - meso proterozoic : dongdashan iron, jinchuan nickel - copper. ( 2 ) the divergent metallogenic system in the northern margin of the qaidam paleoplate in the middle - late proterozoic : huashugou - liugouxia iron. ( 3 ) the metallogenic system in the active margin in the early paleozoic : the metallogenic assemblage in the island arc - rift in the early stage ( baiyinchang - qingshuigou copper - polymetallic ) ; the metallogenic assemblage in island arc in the middle - late stage ( honggou - jiaolongzhang copper - polymetallic ) ; the back - arc extensional basin ( zhuzhuiyaba - jiugequan - shijuli copper ) ; the metallogenic assemblage in connection with subduction and magmatic - hydatogenesis ( taergou - xiaoliugou wolfram ; huashugou - liugouxia copper ; dadonggou - diaodaban lead - zinc ) ; the metallogenic assemblage is related to the oceanic crustal shards ( dadaoerji chromite ; yushigou chromite ). ( 4 ) the metallogenic system has something to do with collision - type orogeny : the metallogenic assemblage in foreland basin ( tianlu copper ) ; the metallogenic assemblage with the intracontinental orogeny and ductile shear ( hanshan - yingzhuishan gold )
根據構造發展階段和成礦作用特點，確定本區成礦系統及組合如下： （ 1 ）華北板塊西南邊緣太古宙中元古代裂解期前成礦系統：東大山鐵成礦組合，金川鎳銅成礦組合； （ 2 ）柴達木板塊北緣中、新元古代裂解成礦系統：樺樹溝柳溝峽鐵成礦組合； （ 3 ）加里東期活動大陸邊緣成礦系統：早期島弧裂谷成礦組合（白銀廠清水溝銅及多金屬成礦組合） ，中、晚期島弧成礦組合（紅溝蛟龍掌銅及多金屬成礦組合） ，弧后擴張盆地成礦組合（豬咀啞巴九個泉石居里銅及多金屬成礦組合） ，與俯沖作用有關的巖漿熱液成礦組合（塔爾溝小柳溝鎢成礦組合，樺樹溝柳溝峽銅成礦組合，大東溝吊大坂鉛鋅成礦組合） ，洋殼殘片成礦組合（大道爾吉鉻成礦組合，玉石溝鉻成礦組合） ； （ 4 ）碰撞造山成礦系統：前陸盆地成礦組合（天鹿銅成礦組合） ，陸內造山韌性剪切成礦組合（寒山鷹咀山金成礦組合） 。Cu - ni sulfided mine complex locate in baimazai of jinping county is sub alkali iron - super iron, it ' s zoning is clear and it ' s ni - cu - co melting first and enrichment, its rare earth is rich in right lean light rare earth, but eu in olive rock is serious to be bad, gd - tb is tittles negative abnormity. above - mentioned show that the mineral is cone from mantle, and didn " t mix with crustal substance, and continent tholeiite magma turning into continent tholeiite emplacement after by surging
金平白馬寨銅鎳硫化礦床雜巖體分帶明顯、屬亞堿性鐵質-超鐵質巖、具ni - cu - co三元素先熔離，后富集的規律、稀土配分為右傾斜輕稀土富集型，但橄欖巖銪虧損顯著， gd - tb微小負異常，顯示成礦物質來源地幔，與地殼物質無混染和大陸拉斑玄武巖漿上涌后變為大洋拉斑玄武巖漿侵位特點。This paper researches the synthetical ore - forming feature of cu - ni sulfided mine of baimazai in jin ping county. this nine is the main force of ni manufacturer. it is exact to look for succeed resource because of the resource has been drying up
本文研究金平白馬寨銅鎳硫化礦綜合信息成礦特徵，該礦作為雲南鎳礦主力生產礦山，由於資源已盡枯竭，急需找尋接替資源。This system constructs the iii rock body ' s 3d figure of cu - ni sulfided mine of jinping baimazai in the round by using the database of mathematic and economical model and information, and locates the extent orientation and marginal form of this rock body. this system designs a project of iii rock body ( 650 - 755m ) ore - search according to it
運用礦床數學經濟模型數據庫，結合探采資料，系統全面直觀地建立了金平白馬寨銅鎳硫化礦號巖體的三維形態，對礦體的深部延伸方向和邊部形態進行定位，據此對號巖體深部（ 650 - 755m ）作了找礦勘探設計。So, in this system, we collected geological and mining information about the mine, investigated and researched about the regional geology and the features of rock and mine body. it establishes mathematic and economical model of this the mineral deposit and mining area warehouse about map and description of cu - ni sulfided mine of baimazai in jin - ping county using the software of mathematic and economical model and mapgis
為此，系統搜集了與礦山有關的地質、采礦圖文資料，對區域地質、巖體及礦體特徵展開了詳細的野外地質調查和深入的室內研究。分別運用礦床數學經濟模型軟體和mapgis地理信息系統軟體建立了金平白馬寨銅鎳硫化礦礦床數學經濟模型和礦區圖文庫。分享友人