黄金
黃金
황금
GOLD JOURNAL
2013年
9期
23-29
,共7页
稀土元素地球化学%成矿物质来源%枣子沟金矿床%甘肃
稀土元素地毬化學%成礦物質來源%棘子溝金礦床%甘肅
희토원소지구화학%성광물질래원%조자구금광상%감숙
geochemistry of REE%source of ore-forming mineral%Zaozigou gold deposit%Gansu
对比研究了枣子沟金矿区内不同类型矿石与成矿有关的岩浆岩及地层的稀土元素地球化学特征,借以示踪成矿物质来源。研究表明,矿床不同类型矿石的稀土元素配分曲线既有相似又有差别,反映成矿物质具有多样性;矿石与容矿岩石(地层、岩浆岩)稀土元素配分曲线颇为相似,总体呈右倾型,具Eu负异常。表明成矿与容矿岩石(地层、岩浆岩)具有一定的成因联系。成矿物质来源于壳源及壳幔混合。地幔流体可能参与了矿床成矿作用。成矿环境表现为早期还原,晚期由还原向氧化转化。
對比研究瞭棘子溝金礦區內不同類型礦石與成礦有關的巖漿巖及地層的稀土元素地毬化學特徵,藉以示蹤成礦物質來源。研究錶明,礦床不同類型礦石的稀土元素配分麯線既有相似又有差彆,反映成礦物質具有多樣性;礦石與容礦巖石(地層、巖漿巖)稀土元素配分麯線頗為相似,總體呈右傾型,具Eu負異常。錶明成礦與容礦巖石(地層、巖漿巖)具有一定的成因聯繫。成礦物質來源于殼源及殼幔混閤。地幔流體可能參與瞭礦床成礦作用。成礦環境錶現為早期還原,晚期由還原嚮氧化轉化。
대비연구료조자구금광구내불동류형광석여성광유관적암장암급지층적희토원소지구화학특정,차이시종성광물질래원。연구표명,광상불동류형광석적희토원소배분곡선기유상사우유차별,반영성광물질구유다양성;광석여용광암석(지층、암장암)희토원소배분곡선파위상사,총체정우경형,구Eu부이상。표명성광여용광암석(지층、암장암)구유일정적성인련계。성광물질래원우각원급각만혼합。지만류체가능삼여료광상성광작용。성광배경표현위조기환원,만기유환원향양화전화。
Comparative study on different kinds of ores , metallogenic magmatic rocks and geological features of REE in strata of Zaozigou gold deposit was conducted to trace the source of ore-forming minerals .Research shows that REE curves of different ores in the deposit are similar while distinct meaning complex ore -forming minerals .Ores and host rocks ( strata and magmatic rocks ) curves take on similar forms ,generally the rightwards type and Eu negative a-nomaly .This indicates metallogenesis and host rocks are related .The ore-forming minerals came from crust source and mixture of crust and mantle .Mantle fluids may have participated in the mineralization .The early ore-forming settings are reduction and later transmitted from reduction to oxidation .