[an error occurred while processing this directive] ������� 2012, 31(2) 281-289 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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Ore geochemical characteristics and genesis of Xikuangshan type Fe --Cu deposit in Lanniping--Baixila copper mine of Dongchuan
LIU Wei-Ming-1, 2, LIU Ji-Shun-1, LIU Wen-Heng-1, YANG Li-Gong-1, ZHOU Yu-Guo-3, DONG Xin-1
1. School of Geosciences and Info-Physics��Central South University��Changsha 410083��China; 2. Faculty of Resources and Environmental Engineering��Jiangxi University of Science and Technology�� Ganzhou 341000��Jiangxi��China; 3. School of Resources Environment and Earth Science��Yunnan University��Kunming 650051��China; 4. Gansu Non-ferrous Metal Geological Exploration Bureau��Lanzhou 730000��China
Abstract:

On the basis of the correlation of Yinmin Formation from Lanniping --Baixila copper mine area��the authors confirmed the existence of Xikuangshan type deposit in the studied area��and designed mineral exploration engineering in favorable sectors�� Analysis and comparation of geochemical characteristics of the exposed orebody revealed that ( K2O + Na2O) contents and K2O/Na2O ratio of ores are similar to in Yinmin mine area�� REE contents are ( 55. 94 �� 367. 72) × 10-6��( La /Yb) N = 5. 09 �� 67. 57 with strong enrichment of LREE and positive Eu anomaly�� The REE characteristics are similar to hydrothermal solution of modern ocean floor��which shows that oreforming fluid was in deep high-temperature with deoxidation nature��

Keywords: Yinmin Formation   Xikuangshan type Fe-Cu deposit   prospecting potential   Lanniping   Baixila   Dongchuan  
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