Re-Os isotopic analysis of the Kalatongke Cu-Ni sulfide deposit, northern Xinjiang, NW China, and its geological implication

Abstract

The Kalatongke is a large Cu-Ni deposit in the southern part of the Altay orogenic belt, northwestern China. Rhenium and osmium isotopic analyses of Ni-and Cu-bearing sulfide minerals from the deposit have been used to determine the timing of mineralization, the source of osmium, and, by inference, the source of ore metals. Sulfide ore samples have osmium and rhenium concentrations varying in the ranges of 0.29 - 3.07 ppb, and 6.605 - 61.10ppb, respectively. Analyses of these data yield a six-point isochron with an age of 305 ± 15Ma. The age implies that the Cu-Ni sulfide deposit and other related magmatic deposits in the same area formed between the latest Carboniferous and Early Permian post-collisional extension in the Altay Shan. An initial 187Os/ 188Os ratio of 0.352 ± 0.044 (MSWD=2.1) and the δ 34S of -3.5‰ to + 3.0‰ for the ores, as well as initial 87Sr/ 86Sr ratios of metalliterous intrusions that vary from 0.70375 to 0.70504, suggest a magmatic source for the ores, with the melts being dominated by mantle contributions. The data also indicate that the Kalatongke Ni-Cu deposit, like many other copper, gold, and nickel deposits within central Asia, is related to post-collisional extensional processes.

喀拉通克銅鎳硫化物礦石的Re-Os同位素測年結果為305±15(2σ)Ma。該數據表明產于阿爾泰山南緣的銅鎳硫化物礦床形成于晚石炭世一早二疊世,與區內廣泛發育的造山型金礦和淺成低溫熱液型金礦基本為同一時期。其等時線~187Os/~188Os初始比值為0．35±0．04,γ_Os仉值平均為183,表明在成礦過程及巖漿侵位期間有少量地殼物質加入成礦系統中。