黄金
黃金
황금
GOLD JOURNAL
2014年
3期
21-25
,共5页
地质特征%找矿标志%硅化蚀变岩型金矿床%金英金矿床%松江河金矿床%吉林东部
地質特徵%找礦標誌%硅化蝕變巖型金礦床%金英金礦床%鬆江河金礦床%吉林東部
지질특정%조광표지%규화식변암형금광상%금영금광상%송강하금광상%길림동부
geological characteristics%prospecting indicator%silicification altered rock gold deposit%Jinying Gold Deposit%Songjianghe Gold Deposit%east Jilin Province
通过对吉林省内金英金矿床与松江河金矿床2个硅化蚀变岩型金矿床地质特征的“类比求同”,总结出该类型矿床共同特点为:都与大型区域性断裂构造有关,控矿构造为大型区域性断裂构造的次级断裂构造,赋矿层位为元古代地层中的特定“界面”;矿体品位与黄铁矿等金属硫化物无关,矿体与围岩界线不明显,金呈独立矿物出现且成色较高,围岩蚀变以硅化为主,并见有碳酸盐化、高岭土化、重晶石化等,呈现出中低温矿物组合特点。该类矿床地质特征的对比分析对寻找类似矿床具有重要意义。
通過對吉林省內金英金礦床與鬆江河金礦床2箇硅化蝕變巖型金礦床地質特徵的“類比求同”,總結齣該類型礦床共同特點為:都與大型區域性斷裂構造有關,控礦構造為大型區域性斷裂構造的次級斷裂構造,賦礦層位為元古代地層中的特定“界麵”;礦體品位與黃鐵礦等金屬硫化物無關,礦體與圍巖界線不明顯,金呈獨立礦物齣現且成色較高,圍巖蝕變以硅化為主,併見有碳痠鹽化、高嶺土化、重晶石化等,呈現齣中低溫礦物組閤特點。該類礦床地質特徵的對比分析對尋找類似礦床具有重要意義。
통과대길림성내금영금광상여송강하금광상2개규화식변암형금광상지질특정적“류비구동”,총결출해류형광상공동특점위:도여대형구역성단렬구조유관,공광구조위대형구역성단렬구조적차급단렬구조,부광층위위원고대지층중적특정“계면”;광체품위여황철광등금속류화물무관,광체여위암계선불명현,금정독립광물출현차성색교고,위암식변이규화위주,병견유탄산염화、고령토화、중정석화등,정현출중저온광물조합특점。해류광상지질특정적대비분석대심조유사광상구유중요의의。
Analogy is made between the characterisitics of Jinying Gold Deposit and Songjianghe Gold Deposit , two silicification altered rock gold deposits .It is concluded that the same type deposit has such common characteristics as close relation to large scale regional fracture structures ,ore-controlling structures being secondary ones to large scale regional fracture structures ,occurrence being specific plane among Proterozoic layers ,grade of orebodies having noth-ing to do with metal sulfide like pyrites ,blur in the boundary between orebodies and surrounding rocks ,gold displaying higher grades as independent minerals ,silicification dominating the alteration of surrounding rocks while carbonation , kaolinization ,baratization coexisting ,a characteristic of medium-low temperature mineral association .The analogical a-nalysis among this type of deposits'characteristics bears significance of finding similar deposits .