%0 Journal Article
%T Sm-Nd and Rb-Sr isotopical ages of magnetite-chlorite formation gold deposit in the volcanic rock area of Late Paleozoic Era, East Tianshan
%A Jinsheng Ji
%A Huaqin Li
%A Lianchang Zhang
%A Xingke Yang
%A Chengyou Feng
%J Chinese Science Bulletin
%@ 1861-9541
%D 1999
%I 
%R 10.1007/BF02886163
%X Through studying geo-geochemical characteristics and determining Sm-Nd and Rb-Sr isotopical ages in the Kanggur magnetite-chlorite formation gold deposit, some conclusions can be achieved: Sm-Nd isochron age is (290.4 ¡À 7)Ma, Rb-Sr isochron age is (282.3 ¡À 5)Ma, mineralization is Late Hercynian and the formation of this gold deposit is related to the macroscopic Huangshan-Qiugemingtashi ductile shear zone which is produced as a result of collision between the Tarim plate and the Junggar plate.
%K gold deposit
%K Sm-Nd isotope
%K Rb-Sr isotope
%K Kanggurtage
%U http://link.springer.com/article/10.1007/BF02886163