地球化学
地毬化學
지구화학
GEOCHIMICA
2008年
4期
329-343
,共15页
裘愉卓%涂光炽%Byron R. BERGER
裘愉卓%塗光熾%Byron R. BERGER
구유탁%도광치%Byron R. BERGER
浅成低温热液%金矿床%中国
淺成低溫熱液%金礦床%中國
천성저온열액%금광상%중국
epithermal gold deposits%China
浅成低温热液金矿床在中国传统上称为陆相火山岩型金矿床,主要发现在中国东部,后来在北疆地区也有新的发现.根据产出的大地构造背景,它们集中分布在3个带,并分属于3个成矿时期.它们包括:(1)新生代台湾东部岛弧带;(2)晚古生代北疆岛弧带;(3)中生代沿中朝克拉通北界的大陆边缘带;(4)中生代中国东南沿海地区的大陆边缘带.绝大多数矿床是低硫化型的,只有3个是高硫化型的,另有1个是与碱性岩系有关的Au-Te型矿床.除了中国最大的金矿床金瓜石矿床外,迄今为止中国大陆上的浅成低温热液金矿床总的来说只有较小的经济重要性.在中国东部发现的浅成低温热液金矿床的总储量,与区内广泛分布的中生代陆相火山岩十分巨大的体积极不相称.较古老的成矿年龄,中国东部的中生代和北疆的晚古生代,是中国大陆浅成低温热液金矿床的一个鲜明的特点.根据中国的成矿条件和保存条件的分析,以及与美国西部和俄国东部的对比,提出了中国浅成低温热液金矿床成矿潜力的一个初步评估.北疆可能有较大的寻找浅成低温热液金矿床的潜在重要性.
淺成低溫熱液金礦床在中國傳統上稱為陸相火山巖型金礦床,主要髮現在中國東部,後來在北疆地區也有新的髮現.根據產齣的大地構造揹景,它們集中分佈在3箇帶,併分屬于3箇成礦時期.它們包括:(1)新生代檯灣東部島弧帶;(2)晚古生代北疆島弧帶;(3)中生代沿中朝剋拉通北界的大陸邊緣帶;(4)中生代中國東南沿海地區的大陸邊緣帶.絕大多數礦床是低硫化型的,隻有3箇是高硫化型的,另有1箇是與堿性巖繫有關的Au-Te型礦床.除瞭中國最大的金礦床金瓜石礦床外,迄今為止中國大陸上的淺成低溫熱液金礦床總的來說隻有較小的經濟重要性.在中國東部髮現的淺成低溫熱液金礦床的總儲量,與區內廣汎分佈的中生代陸相火山巖十分巨大的體積極不相稱.較古老的成礦年齡,中國東部的中生代和北疆的晚古生代,是中國大陸淺成低溫熱液金礦床的一箇鮮明的特點.根據中國的成礦條件和保存條件的分析,以及與美國西部和俄國東部的對比,提齣瞭中國淺成低溫熱液金礦床成礦潛力的一箇初步評估.北疆可能有較大的尋找淺成低溫熱液金礦床的潛在重要性.
천성저온열액금광상재중국전통상칭위륙상화산암형금광상,주요발현재중국동부,후래재북강지구야유신적발현.근거산출적대지구조배경,타문집중분포재3개대,병분속우3개성광시기.타문포괄:(1)신생대태만동부도호대;(2)만고생대북강도호대;(3)중생대연중조극랍통북계적대륙변연대;(4)중생대중국동남연해지구적대륙변연대.절대다수광상시저류화형적,지유3개시고류화형적,령유1개시여감성암계유관적Au-Te형광상.제료중국최대적금광상금과석광상외,흘금위지중국대륙상적천성저온열액금광상총적래설지유교소적경제중요성.재중국동부발현적천성저온열액금광상적총저량,여구내엄범분포적중생대륙상화산암십분거대적체적겁불상칭.교고로적성광년령,중국동부적중생대화북강적만고생대,시중국대륙천성저온열액금광상적일개선명적특점.근거중국적성광조건화보존조건적분석,이급여미국서부화아국동부적대비,제출료중국천성저온열액금광상성광잠력적일개초보평고.북강가능유교대적심조천성저온열액금광상적잠재중요성.
Epithermal gold deposits have been found mainly in eastern China and recently in the northern Xinjiang Region.They are grouped into four bolts based on their tectonic settings and belong to three mineralization episodes. They include:(1) the Cenozoic eastern Taiwan island are belt; (2) the Late Paleozoic North Xinjiang island arc bolt; (3) the Mesozoic continental margin bolt along the northern border of the Sino-Korean Craton; and (4) the Mesozoic continental margin belt of SE China coastal area. Most of the reviewed deposits are of low snlfidation type, three are of high sulfidation type, and one is of Au-Te type related to alkaline rock series. Except the Chinkuashih deposit, the largest gold deposit in China, the epithermal gold deposits in general are of less economic importance at present in the mainland of China. The total reserve of epithennal gold deposits discovered in eastern China is not compared with the huge volume of widespread subaerial volcanic rocks of Mesozoic age. Relatively old mineralization age, Mesozoic in eastern China and Late Paleozoic in North Xinjiang, is an apparent feature of epithermal gold deposits in the mainland of China. Based on the analyses of metallogenic condition and preservation in China, and the comparison with western USA and eastern Russia, a preliminary assessment on the potential of epithermal gold deposits of China has been presented. Northern Xinjiang may be potentially significant for finding epithermal gold deposits.