GEOCHEMICAL CHARACTER OF DISPERSED ELEMENT IN SPHALERITE FROM FULE Pb-Zn POLYMETAL DEPOSIT,YUNNAN PROVINCE
GEOCHEMICAL CHARACTER OF DISPERSED ELEMENT IN SPHALERITE FROM FULE Pb-Zn POLYMETAL DEPOSIT,YUNNAN PROVINCE
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发表时间:
2006
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通讯作者:
Si Rong-jun;Guo Xue‐xiang
中科院分区:
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作者:
Si Rong-jun;Guo Xue‐xiang
The dispersed elements have great economic value,and are widely applied to high and new-technology industries.However it is difficult for them to accumulate and form ore deposits because of their low assay and dispersivity in the crust.Four dispersed elements Cd,Se,Ge and Ga have economic value in Fule PbZn deposit which is localed in the southeast part of Sichan-Yunnan-Guihzou polymetallogenic district.The dispersed elements mainly occurred in sphalerites with average content of w(Cd) 16 183×10~(-6),w(Se) 163×10~(-6),w(Ge) 135×10~(-6) and w(Ga) 86×10~(-6) resectively,and with the content of Cd being the highest in China.The colour of sphalerite can be divided into dark-brown,red-brown and yellow-brown.Cd occurs mostly in dark colour sphalerite,Ge and Ga in light colour one,the content of Se does not change in different colour sphalerite.Mainly occurred as allomerism form,Cd,Ge,and Se occur in crystal lattice of sphalerite,where Cd and Ge occupy the position of Zn and Se occupies the position of S.Ga usually are adsorbed in lattice defect as microadsorption form,and the other enter sphalerite crystal lattice in place of Zn in sphalerite Cd-Zn are negative correlation,Ge-Zn are positive correlations,but Se-Zn are independent.The geochemical characters of the dispersed elements indicate that the deposit belongs to sedimentation-reformation type.