上海地质
上海地質
상해지질
2010年
B11期
206~209
,共null页
铅锌多金属矿 东至断裂 控矿构造 控矿地层 地质特征 找矿方向
鉛鋅多金屬礦 東至斷裂 控礦構造 控礦地層 地質特徵 找礦方嚮
연자다금속광 동지단렬 공광구조 공광지층 지질특정 조광방향
lead-zinc polymetallic ore; Dongzhi rupture; ore-controlling structure; ore stratum; geological characteristics; prospecting
本文从控矿地层、控矿构造、矿体特征、热液蚀变等方面阐述了东至县兆吉口铅锌多金属矿成矿地质特征。通过对东至县兆吉口地区成矿地质条件综合分析，划分了兆吉口一叶家、杨树桥、万年灯、草鞋树、何村五片铅、锌、金、银、铜、钼远景区，为该区下步地质找矿指明了方向。
本文從控礦地層、控礦構造、礦體特徵、熱液蝕變等方麵闡述瞭東至縣兆吉口鉛鋅多金屬礦成礦地質特徵。通過對東至縣兆吉口地區成礦地質條件綜閤分析，劃分瞭兆吉口一葉傢、楊樹橋、萬年燈、草鞋樹、何村五片鉛、鋅、金、銀、銅、鉬遠景區，為該區下步地質找礦指明瞭方嚮。
본문종공광지층、공광구조、광체특정、열액식변등방면천술료동지현조길구연자다금속광성광지질특정。통과대동지현조길구지구성광지질조건종합분석，화분료조길구일협가、양수교、만년등、초혜수、하촌오편연、자、금、은、동、목원경구，위해구하보지질조광지명료방향。
The Lead-zinc polymetallic ore was discovered by General Nuclear prospecting techniques Research Institute of Anhui Province in a implementation of one project in 2006. This discovery is praised as an important breakthough for the ore-searching of southwest of Anhui Province. The following aspects such as ore formation, ore-controlling structures, ore characteristics, hydrothermal alteration and so on are concerned to expounding the mineralization features of this area. With a comprehensive analysis of the geological conditions of this area, this paper divide the area into five special scenic spots for five different metal ingredients, which specified the direction of geological prospecting.
