大地构造与成矿学
大地構造與成礦學
대지구조여성광학
GETECTONICA ET METALLOGENIA
2015年
1期
128-138
,共11页
周栋%包志伟%姚军明%曾令君%赵太平
週棟%包誌偉%姚軍明%曾令君%趙太平
주동%포지위%요군명%증령군%조태평
八宝山铁铜多金属矿床%斑岩成矿体系%黄铁矿%氧化还原环境%卢氏
八寶山鐵銅多金屬礦床%斑巖成礦體繫%黃鐵礦%氧化還原環境%盧氏
팔보산철동다금속광상%반암성광체계%황철광%양화환원배경%로씨
Babaoshan iron and copper polymetallic deposit%porphyry metallogenic system%pyrite%oxidation and reduction%Lushi county
豫西卢氏八宝山铁铜多金属矿床是华北克拉通南缘中生代斑岩成矿体系中以铁矿化为主的矿床,其中南矿带和西矿带广泛发育黄铁矿。电子探针成分显示,黄铁矿的主要元素S和Fe的总和超过90%,但同一种黄铁矿表面不同位置微量元素Cu和As的含量存在突变。这种突变说明,来源于同一岩浆热液系统的富液相流体与上升的富气相流体的混合作用是引起黄铁矿沉淀的主要机制。黄铁矿中的As有两种赋存价态As3+和As1–,代表了八宝山斑岩矿床中形成黄铁矿的岩浆流体可能经历了先氧化后还原的环境(As3+指示氧化环境, As1–指示还原环境),说明八宝山矿区具有斑岩铜矿的成矿潜力。
豫西盧氏八寶山鐵銅多金屬礦床是華北剋拉通南緣中生代斑巖成礦體繫中以鐵礦化為主的礦床,其中南礦帶和西礦帶廣汎髮育黃鐵礦。電子探針成分顯示,黃鐵礦的主要元素S和Fe的總和超過90%,但同一種黃鐵礦錶麵不同位置微量元素Cu和As的含量存在突變。這種突變說明,來源于同一巖漿熱液繫統的富液相流體與上升的富氣相流體的混閤作用是引起黃鐵礦沉澱的主要機製。黃鐵礦中的As有兩種賦存價態As3+和As1–,代錶瞭八寶山斑巖礦床中形成黃鐵礦的巖漿流體可能經歷瞭先氧化後還原的環境(As3+指示氧化環境, As1–指示還原環境),說明八寶山礦區具有斑巖銅礦的成礦潛力。
예서로씨팔보산철동다금속광상시화북극랍통남연중생대반암성광체계중이철광화위주적광상,기중남광대화서광대엄범발육황철광。전자탐침성분현시,황철광적주요원소S화Fe적총화초과90%,단동일충황철광표면불동위치미량원소Cu화As적함량존재돌변。저충돌변설명,래원우동일암장열액계통적부액상류체여상승적부기상류체적혼합작용시인기황철광침정적주요궤제。황철광중적As유량충부존개태As3+화As1–,대표료팔보산반암광상중형성황철광적암장류체가능경력료선양화후환원적배경(As3+지시양화배경, As1–지시환원배경),설명팔보산광구구유반암동광적성광잠력。
The Babaoshan iron and copper polymetallic deposit, which is located in Lushi county Henan province, is unique for its iron-predominated ore mineralization among all the Mesozoic porphyry metallogenic systems in the southern margin of the North China Craton. Pyrite is ubiquitous in the southern and western parts of the deposit. Their EMPA analyses indicated the contents of S and Fe are more than 90% in total, the contents of Cu and As of the pyrites vary considerably even within the same grain. The abrupt change suggests mixing of ore-forming fluid and upward magmatic vapors from the same magmatic-hydrothermal system is the major force to induce pyrite deposition. That As exist in two valence states, As3+ and As1–, revealed that the Babaoshan pyrite-forming fluid was oxidative originally and changed to be reductive subsequently. The oxygen fugacity fluctuation is a positive factor to the formation of the Babaoshan porphyry copper deposit.