Geological features and tectonic setting of porphyry copper deposits rounding the Balkhash region, Central Kazakhstan, Central Asia
Geological features and tectonic setting of porphyry copper deposits rounding the Balkhash region, Central Kazakhstan, Central Asia
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发表时间:
2008
影响因子:
1.8
通讯作者:
Guangming Li;Qin Kz;Li Jx
中科院分区:
文献类型:
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作者:
Guangming Li;Qin Kz;Li Jx
Central Kazakhstan located in the center of the Central Asia Orogenic Belt(CAOB),is one of the largest porphyry copper deposit metallogenic domains,wherein hosts tens of large and superlm'ge ore deposits.In the area,three major subtypes of porphyry copper deposits have been recognized:porphyry Cu-Au deposits,porphyry Cu deposits and porphyry Cu-Mo deposits,mostly associated with contemporaneous volcanic rocks.Established alteration zonation consists of alkaline and acidic alterations.δ~(34)S(CDT) values of sulfides from porphyry copper deposits range from-7.1% to 4.2%,showing a deep source.Pb isotope analyses reveal that ore-forming materials were generated from lower crust and upper mantle.In the central Kazakhstan multistage tectonic evolutions were followed by formation of multistage porphyry copper deposits.Early Paleozoic porphyry copper deposits have been formed during early stages of island arcs evolution,but late Paleozoic porphyry copper deposits are confined in the Devonian volcano-plutonic belts,and then Carboniferous-Permian volcano-plutonic belts.From northwest to southeast towards the central Kazakhstan,ore-forming ages of porphyry copper deposits are successively younger.Whereas study on porphyry copper deposits in the region throughout tens years, some key problems yet remain uncertain,e.g.high-precise age-dating on intrusive stocks and mineralizations for the major porphyry copper deposits,temparol-spatial distribution framwork and geodynamic settings.The linkage and comprehensive correlation between Balkhash porphyry copper belt and adjacent Chinese western Jungar and western Tienshan is of great significance for further exploration.