Lead isotopic systematics of Urals massive sulphide deposits

被引:2
|
作者
Orgeval, Jean-Jacques [1 ]
Guerrot, Catherine [1 ]
Tessalina, Svetlana G. [1 ]
Bourdon, Bernard [1 ]
Zaykov, Victor [1 ]
Buley, Claudia [1 ]
Bushmann, Berndt [1 ]
Herrington, Richard [1 ]
Taylor, Rex [1 ]
机构
[1] Bur Rech Geol & Minieres, F-45060 Orleans, France
关键词
lead isotopes; Urals; massive sulphide deposits;
D O I
10.1007/3-540-27946-6_170
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The isotopic composition of lead from a total of 53 samples of galena from 18 VHMS deposits shows a range between 17.437 and 18.111 for Pb-206/Pb-204; 15.484 and 15.630 for Pb-207/Pb-204 and 37.201 - 38.027 for Pb-208/204. The results show a systematic trend with the leads of the Sibay, Barsuchiy Log and Djusa deposits being most radiogenic by comparison with those of Bakr-Tau and Oktiabrskoe which are the least radiogenic deposits. The Bakr-Tau and Oktiabrskoe deposits occur within most primitive fore-arc rocks at the lower part of the Baymak-Buribay formation, which contain lavas of boninitic affinity. The Sibay, Barsuchiy Log and Djusa deposits are found in intra- and back-arc setting and are hosted by a sequence of bimodal tholeiites. The deposits in "arc" settings such as the Balta-Tau, Gai and Alexandrinka deposits occupy an intermediate position. This trend is explained in term of mixing between mantle wedge and continental blocks.
引用
收藏
页码:667 / 670
页数:4
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