主要蚀变为硅化、钾化、黄铁矿化、绢云母化。
Silicification, potassic alteration, pyritization and sericitization are main alterations for the gold deposit.
矿化表现为“硅化、白云石化、黄铁矿化”组合。
The gold mineralization is represented by the association of silicification, dolomitization and pyritization.
蚀变类型主要有硅化、绢云母化、钾化、黄铁矿化。
The alteration are mainly silicification, sericitization, k feldspathization and pyritization.
伴生的金矿化局部较好，可能与铜矿化阶段的黄铁矿化有关。
The associated gold mineralization is locally well-developed and may be related to pyritization during the stage of Cu mineralization.
认为含矿岩系的物源主要来自海底火山喷发作用形成的黄铁矿化矿源层。
According to the study of the mineral evolving, origin analysis etc., it is considered that the source of minerals etc mainly comes from the pyritization sources of the submarine volcano eruption.
蚀变是区内的找矿标志之一，金矿的形成与硅化、褐铁矿化、黄铁矿化等蚀变有关。
The development of gold deposit in this area is connected with alteration, such as silicification, ferritization, pyritization.
火山演化从早期到中晚期分别形成铁矿层、火山成因块状硫化物矿床和黄铁矿化层。
Early to late stage volcanic evolution resulted in the formation of iron formations, sulfide deposits and pyrite mineralization beds.
绢云母化、硅化、钾长石化、黑云母化、黄铁矿化、赤铁矿化及水合多水高岭石化等。
Wall rock alterations include sericitization, silicification, potassic feldspathization, biotitization, pyritization, hematitization and hydrous kaolinization.
夏杖子金矿严格受构造破碎带控制，围岩蚀变主要为钾长石化、黄铁矿化、硅化和碳酸盐化。
Xiazhangzi gold deposit is strictly controlled by structural fracture zone, and the wall rock alterations are mainly of K feldsparization, pyritization, silication and carbonation.
金的载体矿物主要为石英和黄铁矿，但随着不同矿化阶段和矿化环境常形成多样的矿石类型。
Thegold-bearing mineral mainly consist of quartz and pyrite, but many sorts of ore formed in different mineral periods and environment.
黄铁矿是金矿中最常见的金属矿物，它不仅与金的矿化有着密切联系，而且还是主要的载金矿物。
Pyrite is the most common metal mineral in gold deposits. It not only has a close relationship with the gold mineralization, but also is the main gold-carrier.
金的矿化与富集以富含黄铁矿、贫其他多金属硫化物为特征。
The mineralization and enrichment of gold are characterized by the rich pyrite and poor other polymetallic sulfide.
矿石主要类型为石英脉型，矿石有益组分为辉钼矿，形成于石英-黄铁矿-辉钼矿-黄铜矿早期矿化阶段。
Ore types are mostly quartz veins. The useful component is molybdenite formed in the quartz-pyrite-molybdenite-chalcopyrite of early mineralization stage.
金矿化以含金黄铁矿为特征，产出于盖县组变质砂岩段厚层状变质砂岩、薄层状变质砂岩和石墨化片岩的互层带中， 矿体产状与地层一致；
The gold metallogeny is characterized by auriferous pyrite and occurred in the alternating layer of heavy-layer metasandstone, flaggy metasandstone and graphitization schist.
金矿化以含金黄铁矿为特征，产出于盖县组变质砂岩段厚层状变质砂岩、薄层状变质砂岩和石墨化片岩的互层带中， 矿体产状与地层一致；
The gold metallogeny is characterized by auriferous pyrite and occurred in the alternating layer of heavy-layer metasandstone, flaggy metasandstone and graphitization schist.
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