地球化学
地毬化學
지구화학
GEOCHIMICA
2014年
6期
602-618
,共17页
林振文%秦艳%岳素伟%周振菊%王立新%余康伟
林振文%秦豔%嶽素偉%週振菊%王立新%餘康偉
림진문%진염%악소위%주진국%왕립신%여강위
造山型金矿%蚀变分带%元素迁移%铧厂沟金矿%陕西省
造山型金礦%蝕變分帶%元素遷移%鏵廠溝金礦%陝西省
조산형금광%식변분대%원소천이%화엄구금광%합서성
orogenic gold deposit%alteration zoning%element migration%the Huachanggou gold deposit%Shaanxi Province
陕西省铧厂沟金矿床位于勉略缝合带以南,矿体受控于近东西向逆冲断层和韧脆性剪切带。本文以细碧岩矿带为例,系统研究了围岩蚀变分带及蚀变矿物组合,总结了矿床的蚀变分带模式。围岩蚀变以穿切细碧岩透镜体的剪切带为中心向外依次可划分为黄铁绢英岩化带、绢云碳酸盐化带和绿泥赤铁矿化带。蚀变矿物组合分别为黄铁矿+铁白云石+铬云母+绢云母+钠长石+石英+方解石、铁白云石+绢云母+钠长石+石英±黄铁矿、(铁)绿泥石+钠长石+铁白云石+赤铁矿+钛铁氧化物+石英±绿帘石。蚀变岩石组分迁移分析表明,在围岩蚀变过程中, SiO2、Na2O、Fe2O3T、MgO与Y等组分发生不同程度的迁出, K2O、CaO、Ba、Rb、Sr、Cr、Cu、Pb和挥发组分等迁入,并以黄铁绢英岩化带最为显著。金在成矿流体中以Au(HS)–2络合物迁移,成矿流体与富铁细碧岩之间的反应是金沉淀重要机制。
陝西省鏵廠溝金礦床位于勉略縫閤帶以南,礦體受控于近東西嚮逆遲斷層和韌脆性剪切帶。本文以細碧巖礦帶為例,繫統研究瞭圍巖蝕變分帶及蝕變礦物組閤,總結瞭礦床的蝕變分帶模式。圍巖蝕變以穿切細碧巖透鏡體的剪切帶為中心嚮外依次可劃分為黃鐵絹英巖化帶、絹雲碳痠鹽化帶和綠泥赤鐵礦化帶。蝕變礦物組閤分彆為黃鐵礦+鐵白雲石+鉻雲母+絹雲母+鈉長石+石英+方解石、鐵白雲石+絹雲母+鈉長石+石英±黃鐵礦、(鐵)綠泥石+鈉長石+鐵白雲石+赤鐵礦+鈦鐵氧化物+石英±綠簾石。蝕變巖石組分遷移分析錶明,在圍巖蝕變過程中, SiO2、Na2O、Fe2O3T、MgO與Y等組分髮生不同程度的遷齣, K2O、CaO、Ba、Rb、Sr、Cr、Cu、Pb和揮髮組分等遷入,併以黃鐵絹英巖化帶最為顯著。金在成礦流體中以Au(HS)–2絡閤物遷移,成礦流體與富鐵細碧巖之間的反應是金沉澱重要機製。
합서성화엄구금광상위우면략봉합대이남,광체수공우근동서향역충단층화인취성전절대。본문이세벽암광대위례,계통연구료위암식변분대급식변광물조합,총결료광상적식변분대모식。위암식변이천절세벽암투경체적전절대위중심향외의차가화분위황철견영암화대、견운탄산염화대화록니적철광화대。식변광물조합분별위황철광+철백운석+락운모+견운모+납장석+석영+방해석、철백운석+견운모+납장석+석영±황철광、(철)록니석+납장석+철백운석+적철광+태철양화물+석영±록렴석。식변암석조분천이분석표명,재위암식변과정중, SiO2、Na2O、Fe2O3T、MgO여Y등조분발생불동정도적천출, K2O、CaO、Ba、Rb、Sr、Cr、Cu、Pb화휘발조분등천입,병이황철견영암화대최위현저。금재성광류체중이Au(HS)–2락합물천이,성광류체여부철세벽암지간적반응시금침정중요궤제。
The Huachanggou gold deposit in Shaanxi province is located to the south of Mianlue suture zone. The ore bodies are mainly controlled by EW trending reverse faults and ductile-brittle shear zones. Based on detailed study of alteration mineral association in the main ore zone that hosted in the spilite tectonic lens, an alteration zoning model has been established. The wall rock alteration can be divided into three alteration zones outward from the shear center: pyrite - phyllic alteration zone, sericite - carbonate alteration zone, chlorite - hematite alteration zone. The alteration mineral associations are pyrite + ankerite + fuchsite + sericite + albite + quartz +calcite, ankerite+sericite+albite+quartz ± pyrite, and chlorite+albite+ankerite+hematite+ilmenite oxide+quartz ± epidote, respectively. The elements migration analysis showed that SiO2, Na2O, Fe2O3T, MgO and Y occur to move out in varying degrees, while K2O, CaO, Ba, Rb, Sr, Cr, Cu, Pb and volatile components move in during alteration. The most intensive migration occurred in the pyrite phyllic alteration zone. Gold is mainly transported as Au(HS)–2 complex in the hydrothermal fluids. It seems that fluid-rock interaction between ore-forming fluid and Fe-rich spilite plays an important role in gold precipitation.