上海地质
上海地質
상해지질
2010年
B11期
157~161
,共null页
钼矿床 地质特征 矿床成因 找矿标志 邵武观音山
鉬礦床 地質特徵 礦床成因 找礦標誌 邵武觀音山
목광상 지질특정 광상성인 조광표지 소무관음산
molybdenum deposit; geological characteristics; genesis of mineral deposit; prospecting indications and guides; Shaowu city
邵武观音山钼矿体产于早二叠世栖霞组（P1q）中，矿体呈层状、似层状，容矿岩石为透辉石石榴子石矽卡岩，成矿作用在时间、空间上与燕山期岩浆活动密切相关，属热液交代矽卡岩型钼矿床。
邵武觀音山鉬礦體產于早二疊世棲霞組（P1q）中，礦體呈層狀、似層狀，容礦巖石為透輝石石榴子石矽卡巖，成礦作用在時間、空間上與燕山期巖漿活動密切相關，屬熱液交代矽卡巖型鉬礦床。
소무관음산목광체산우조이첩세서하조（P1q）중，광체정층상、사층상，용광암석위투휘석석류자석석잡암，성광작용재시간、공간상여연산기암장활동밀절상관，속열액교대석잡암형목광상。
The Guanyinshan molybdenum deposit in Shaowu,Fujian Province exists in the limestone of Early Permian Qixia Formation. The orebody is in a stratiform and parabedded occurrence.The host rock is the diopside garnet skarn.The ore-forming process has a close relation with the Yanshanian magmatic activity in time and space.It belongs to the molybdenum deposit of the hydrothermal metasomatic skarn type.
