地质与勘探
地質與勘探
지질여감탐
GEOLOGY AND PROSPECTING
2001年
2期
23-27
,共5页
孙忠实%冯本智%邓军%翟裕生
孫忠實%馮本智%鄧軍%翟裕生
손충실%풍본지%산군%적유생
动力系统%碰撞%叠加%金矿床%吉林
動力繫統%踫撞%疊加%金礦床%吉林
동력계통%팽당%첩가%금광상%길림
动力系统是金成矿作用研究的关键,它控制金矿床产生的始终。运用成矿动力系统思想把夹皮沟区地壳演化和金成矿分为三大阶段和三大构造带。(1)太古—元古宙克拉通隆—滑动力系统边缘矿化带,太古宙克拉通隆起、元古宙沉积物拉伸滑断,成矿动力系统在克拉通周边形成韧性剪切带,金受到初步富集;(2)海西俯冲动力系统南缘矿化带,西伯利亚板块与中朝板块间大陆拉张和碰撞,正反动力系统产生超壳断裂和金矿化;(3)中生代叠加构造岩浆动力系统成矿带,中生代太平洋板块俯冲、郯庐断裂滑移及区域NNE与NW向共轭控矿等多级动力系统叠加、岩浆活动和幔源流体上升及金元素进一步富集等夹皮沟金矿床最终形成。成矿预测范围由原变质岩区进入夹皮沟断裂带上及两侧附近中生代花岗岩区。
動力繫統是金成礦作用研究的關鍵,它控製金礦床產生的始終。運用成礦動力繫統思想把夾皮溝區地殼縯化和金成礦分為三大階段和三大構造帶。(1)太古—元古宙剋拉通隆—滑動力繫統邊緣礦化帶,太古宙剋拉通隆起、元古宙沉積物拉伸滑斷,成礦動力繫統在剋拉通週邊形成韌性剪切帶,金受到初步富集;(2)海西俯遲動力繫統南緣礦化帶,西伯利亞闆塊與中朝闆塊間大陸拉張和踫撞,正反動力繫統產生超殼斷裂和金礦化;(3)中生代疊加構造巖漿動力繫統成礦帶,中生代太平洋闆塊俯遲、郯廬斷裂滑移及區域NNE與NW嚮共軛控礦等多級動力繫統疊加、巖漿活動和幔源流體上升及金元素進一步富集等夾皮溝金礦床最終形成。成礦預測範圍由原變質巖區進入夾皮溝斷裂帶上及兩側附近中生代花崗巖區。
동력계통시금성광작용연구적관건,타공제금광상산생적시종。운용성광동력계통사상파협피구구지각연화화금성광분위삼대계단화삼대구조대。(1)태고—원고주극랍통륭—활동력계통변연광화대,태고주극랍통륭기、원고주침적물랍신활단,성광동력계통재극랍통주변형성인성전절대,금수도초보부집;(2)해서부충동력계통남연광화대,서백리아판괴여중조판괴간대륙랍장화팽당,정반동력계통산생초각단렬화금광화;(3)중생대첩가구조암장동력계통성광대,중생대태평양판괴부충、담려단렬활이급구역NNE여NW향공액공광등다급동력계통첩가、암장활동화만원류체상승급금원소진일보부집등협피구금광상최종형성。성광예측범위유원변질암구진입협피구단렬대상급량측부근중생대화강암구。
Dynamic system is the sdudying key in gold metallization. Itcontrols gold deposit forming all the time. Earth evolution and gold metallization in Jiapigou area are divided into three stages and three kinds of tectonic belts with the help of metallogenic dynamic system theory. The first one is the marginal gold mineralizing belt of rising-slipping dynamic system in the Archean-Proterozoic craton. A pair of dynamic system between uplifting Archean craton and extending or slipping Proterozoic sediments formed gold mineralizing ductile shear belts of the craton margin and then gold enriched initially. Dynamic system of the hercynian subduction is the second kind of the south margin mineralizing belt. Continental rift and collision took place between Siberia plate and Chinese-Korea plate. The positive-negative dynamic system formed over earth crust-fault and gold mineralizes.The Mesozoic superimposing tectono-magmatic dynamic system forms the third kind of metallogenic belt. The Mesozoic Pacific plate subduction, TanLu fault slipping , NNE and NW striked conjugate ore-controlling structure form poly-level dynamic system superimposing. Magma activities and mantle origin fluid go up. Gold further enrich. Finally form Jiapigou gold deposit.The limits of metallogenic prognosis are that original metamorphic rock's area enter Jiapigou fault belt and the Mesozoic granite area by both sides of Jiapigou fault.