地质通报
地質通報
지질통보
GEOLOGICAL BULLETIN OF CHINA
2014年
12期
1890-1908
,共19页
韦少港%董国臣%莫宣学%申俊峰%张翔%薄海军%任龙
韋少港%董國臣%莫宣學%申俊峰%張翔%薄海軍%任龍
위소항%동국신%막선학%신준봉%장상%박해군%임룡
自然重砂%金矿%组合规律%找矿意义
自然重砂%金礦%組閤規律%找礦意義
자연중사%금광%조합규률%조광의의
natural heavy mineral%gold deposit%heavy mineral assemblage%ore prospecting
对云南、海南、江西、湖北、河南、新疆、浙江、山东、辽宁等27个省185个典型金矿床的自然重砂矿物进行统计分析,发现自然重砂矿物对金矿具有良好的响应,自然金、黄铁矿、方铅矿、黄铜矿、白铅矿、辰砂等对寻找金矿具有指示意义。不同成因类型的金矿床反映出的自然重砂矿物组合不同,斑岩型金矿床的标型指示矿物组合为自然金+黄铁矿+方铅矿+重晶石+闪锌矿+白铅矿+金红石,卡林型—类卡林型金矿床的标型指示矿物组合为自然金+黄铁矿+方铅矿+辉锑矿+毒砂+雄(雌)黄,而造山型+矽卡岩型+热液型+构造蚀变岩型金矿床的标型指示矿物组合为自然金+黄铁矿+方铅矿+辰砂。不同区域的金矿床反映出的自然重砂矿物组合也各有差异,闪锌矿为南方各省金矿床的特征矿物,辰砂和白钨矿为北方地区金矿床的特征矿物,重晶石和白铅矿为西部地区金矿的特征矿物。综合研究认为,自然重砂具有直接找矿和指导找矿的作用,按照特定成因类型和区域金矿床所建立的自然重砂矿物组合对建立矿床找矿模型具有重要的意义。
對雲南、海南、江西、湖北、河南、新疆、浙江、山東、遼寧等27箇省185箇典型金礦床的自然重砂礦物進行統計分析,髮現自然重砂礦物對金礦具有良好的響應,自然金、黃鐵礦、方鉛礦、黃銅礦、白鉛礦、辰砂等對尋找金礦具有指示意義。不同成因類型的金礦床反映齣的自然重砂礦物組閤不同,斑巖型金礦床的標型指示礦物組閤為自然金+黃鐵礦+方鉛礦+重晶石+閃鋅礦+白鉛礦+金紅石,卡林型—類卡林型金礦床的標型指示礦物組閤為自然金+黃鐵礦+方鉛礦+輝銻礦+毒砂+雄(雌)黃,而造山型+矽卡巖型+熱液型+構造蝕變巖型金礦床的標型指示礦物組閤為自然金+黃鐵礦+方鉛礦+辰砂。不同區域的金礦床反映齣的自然重砂礦物組閤也各有差異,閃鋅礦為南方各省金礦床的特徵礦物,辰砂和白鎢礦為北方地區金礦床的特徵礦物,重晶石和白鉛礦為西部地區金礦的特徵礦物。綜閤研究認為,自然重砂具有直接找礦和指導找礦的作用,按照特定成因類型和區域金礦床所建立的自然重砂礦物組閤對建立礦床找礦模型具有重要的意義。
대운남、해남、강서、호북、하남、신강、절강、산동、료녕등27개성185개전형금광상적자연중사광물진행통계분석,발현자연중사광물대금광구유량호적향응,자연금、황철광、방연광、황동광、백연광、신사등대심조금광구유지시의의。불동성인류형적금광상반영출적자연중사광물조합불동,반암형금광상적표형지시광물조합위자연금+황철광+방연광+중정석+섬자광+백연광+금홍석,잡림형—류잡림형금광상적표형지시광물조합위자연금+황철광+방연광+휘제광+독사+웅(자)황,이조산형+석잡암형+열액형+구조식변암형금광상적표형지시광물조합위자연금+황철광+방연광+신사。불동구역적금광상반영출적자연중사광물조합야각유차이,섬자광위남방각성금광상적특정광물,신사화백오광위북방지구금광상적특정광물,중정석화백연광위서부지구금광적특정광물。종합연구인위,자연중사구유직접조광화지도조광적작용,안조특정성인류형화구역금광상소건립적자연중사광물조합대건립광상조광모형구유중요적의의。
Assemblages of natural heavy minerals from 185 gold deposits in China were analyzed, and the results show that the assem?blages of natural heavy minerals display relatively close relationships with the genetic types of gold deposits. Various mineral assemblag?es of native gold, pyrite, galena, chalcopyrite, cerusite and cinnabar can be used as indicators for ore-prospecting. Typomorphic min?eral assemblages are varied in different genetic types of gold deposits and different regions in China. The typical heavy minerals in the porphyry gold deposit exhibit native gold+pyrite+galena+sphalerite+barite+cerusite+rutil assemblage, whereas native gold+pyrite + galena + stibnite + arsenopyrite +realgar/orpiment constitute the typical heavy mineral assemblage in Carlin gold deposits. Nevertheless, the heavy minerals in orogenic+skarn+hydrothermal+altered rock gold deposits are simple and characterized by the native gold + pyrite + galena + cinnabar assemblage. Natural heavy mineral assemblages in gold deposits of different areas of China are varied. Sphalerite is the characteristic mineral in gold deposits of southern China, cinnabar and scheelite are characteristic minerals in gold deposits of northern China, and barite and cerusite are characteristic minerals in western China. It is considered that natural heavy mineral assemblages play an important role in the prospecting for gold deposits and the formulation of natural placer prospect?ing models for different genetic types of gold deposits in various parts of China.