中文摘要:通过铅，硫、氢、氧同位素以及不同层位、岩石金丰度的大量统计，成矿与构造、岩浆岩关系研究，表明金的成矿作用具有多来源、多成因、多阶段的特点，金矿有明显的层控性，晚太古代西垌堆组绿岩是金的矿源层。区域东西向复武背斜和南北向韧性剪切带分别控制了成矿区和矿田，矿床、矿体的分布。金矿主要形成在燕山期中温，中深成条件下的脆-韧性变形环境。
Abstract:Large quantities of analyses and statistics of gold abundance in different strata and rocks combined with lead isotope data suggest that greenstone of Late Archean Xigudui Formation is the source bed of gold deposits. The regional EW-trending anticlinorium and the SN-trending ductile shear zones control the distribution of metallogenic provinces and that of ore fields, ore deposits and orebodies respectively. 47% of known gold deposits and ore (mineralization) spots are distributed within or near Tancheng-Lujiang faulted zone, and auriferous quartz veins with economic significance all occur in subsidiary SN-trending ductile shear zones, 1~2 km from the major fault. From Tancheng-Lujiang faulted zone outwards, in conformity with the falling ore-forming temperature and pressure, grain sizes of native gold become smaller, fineness, δ34S values and Co/Ni as well as Se/Te ratios of pyrite decrease, and Au/Ag ratio tends to increase. Strain analysis shows that gold deposits and spots are mostly located in areas where ε=0.6-0.9, while mineralization is rather weak in areas with Zs larger than l or smaller than 0.5. This coincides with the conclusion drawn from the research that gold of wall rocks within the ductile shear zone is most abundant in the moderate shear strain (Y) area, suggesting the mobilization and migration of gold in the strong deformation part and precipitation and enrichment of gold in the moderate strain part. Gold metallization shows polystage, polysource and polygenetic characteristics; nevertheless, the major ore-forming process took place in Yanshanian period in a brittle-ductile deformation environment of intermediate structural layer, with ore-forming temperature 438-132℃, pressure 5.45×107～6.53×107 Pa and depth l.98~2.37 km.
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涂荫玖, 陈成涛.1993.蚌埠-五河地区绿岩带金矿地质特征及控矿因素[J].矿床地质,12(1):38~47.1993.Geological Characteristics And Ore-Control Factors Of Gold Deposits In The Greenstone Belt Of Bengbu-Wuhe Area[J].Mineral Deposits12(1):38~47
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