Petrological and Rock Chemical Characteristics of Ore-Bearing Rock of Xinshan Area in Kafang, Gejiu, Yunnan

Article Preview

Abstract:

The paper studies on the geochemical characteristics of major element, trace element and REE of granite, marble and skarn in Xinshan Area in Kafang. The studies have shown that the granite in Xinshan Area is high-potassium calc-alkalic granite. The distribution plots of REE in different lithological rocks have obvious differences, but all three different lithological rocks have the characteristic of LREE enrichment. The ratio of LREE to HREE of Marble and skarn is larger, while that ratio of granite is smaller. The variation of LREE and HREE of Skarn is large, indicating that REE occurs significantly different in the migration process and the extent of wall rock material exchange.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 524-527)

Pages:

166-179

Citation:

Online since:

May 2012

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2012 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

[1] Zhuang Yongqiu, Wang Renzhong, Yang Shupei, etc. Gejiu tin-copper polymetallic deposits [M]. Beijing: Earthquake Press, 1996.1.

Google Scholar

[2] Fang Weixuan, Hu Ruizhong, Gao Zhenmin. On characteristics of the metallogenic systems of continental dynamics and metallogenic series as well as prospecting orientations at the southern margin of the Yangtze massif and its vicinities [J]. Acta Mineralogica Sinica, 2001, 21 (4): 561.

Google Scholar

[3] Jia Runxing, Fang Weixuan, He Ying, et al. Geochemical characteristics of trace elements for Tangziwa tin polymetal deposit, Gejiu, Yunnan [J]. Acta Mineralogica Sinica, 2004, 24 (2): 136-142

Google Scholar

[4] Huang Tingran. Gejiu native tin typical deposits Introduction [J]. Yunnan Geology, 1984, 3 (1): 36

Google Scholar

[5] Fang Weixuan, Hu Ruizhong, Xie Guiqing, et al. Tectonolithostratigraphic units of the Ailaoshan area in Yunnan, China and their implications of tectonic evolution [J]. Geotectonica Et Metallogenia, 2002, 26 (1): 337.

Google Scholar

[6] Tan Shucheng, Gao Jianguo, Yan Jianguo, etc. Research on primary halos vertical zoning in the ore deposit in Kafang ore field of the Gejiu ore district, Yunnan province as exemplified by the Longshujiao ore block [J]. Acta Mineralogica Sinica, 2001, 21 (4): 591 ~ 595

DOI: 10.1016/j.oregeorev.2012.03.004

Google Scholar

[7] Jia Runxing, Fang Weixuan, He Ying, etc. Geochemical characteristics of REE in tin-polymetal deposit, Gejiu, Yunnan [J]. Journal of the Chinese Rare Earth Society, 2005, 23 (2):228-234

Google Scholar

[8] Fang Weixuan, Jia Runxing. Characteristics of the alkaline picritic volcanic rocks in the Gejiu super large tin-copper depositand their Continental Dynamic implications [J]. Geotectonica Et Metallogenia. 2011, 35 (1): 138-149

Google Scholar

[9] Peng Zhangxiang. Gejiu tin mineralization model questionable [J]. Yunnan Geology, 1992, 11 (4): 362-368

Google Scholar

[10] Tao Yan, Ma Deyun, Gao Zhenmin. An insight into hydrothermal process of involved in the formation of Gejiu tin deposits as indicated by trace element geochemistry [J]. Geology - Geochemistry, 2002, 30 (2): 34 - 39

Google Scholar

[11] Zhang Hai, Fang Weixuan, Wei Ning, etc. Gejiu Kafang volcanic rocks REE geochemical characteristics [J]. Acta Mineralogica Sinica, 2009, (S1): 36-38

Google Scholar

[12] Philip R Whitney, James F Olmsted. Rare earth element meta-somatism in hydrothermal systems: the willsboro-lewiswollastonite ores [J]. New York, USA. Geochimica et Cosmochimica Acta. 1998, 62 (17): 2965

DOI: 10.1016/s0016-7037(98)00230-0

Google Scholar

[13] Yang Xueming, Yang Xiaoyong, Chen Tianhu, et al. Geochemical characteristics of a carbonatite dyke rich in rare earths from Bayan Obo, China [J]. Journal of the Chinese Rare Earth Society, 1999, 17 (4): 289

Google Scholar

[14] Xu Cheng, Liu Congqiang, Qi Liang, et al. Geochemistry of carbonatites in Maoniuping REE deposit, Sichuan Province, China [J]. Science in China (Series D), 2003, 46 (3): 246.

DOI: 10.1360/03yd9023

Google Scholar

[15] Sun SS, McDonough W F. Chemical and isotopic systematics of oceanic basalts: implications for mantlecomposition and pro-cesses. In: Saunders AD, Norry M J. magamatism in the ocean Basins [C]. London: Geological Society Special Publication , 1989, 313.

DOI: 10.1144/gsl.sp.1989.042.01.19

Google Scholar

[16] Maniar PD, Piccolli PM, Tectonic discrimination of granitoids. Geo1.Soc. Am.Butt, 1989, 101: 635 ~ 643.

Google Scholar

[17] Le Bas MJ, Le Maitre RW, Streckeisen A and Zanettin B. A chemical classification of Vocanic rocks basedon the total alkali-silica diagram. Journal of Petrology, 1986. 27: 745 ~ 750.

DOI: 10.1093/petrology/27.3.745

Google Scholar

[18] Peceerillo R and Taylor S R. Geochemistry of Eocene cale-alkaline volcanic rocks from the Kastamonu area, northern Turkey. Contrib. Minera1. Petro1. 1976, 58: 63 ~ 81.

DOI: 10.1007/bf00384745

Google Scholar

[19] Shi Changyi, Yan Mingcai, Chi Qinghua, China granite chemical element abundance [M]. Beijing: Geological Publishing House, 2008.

Google Scholar

[20] Yang Xueming, Yang Xiaoyong, Chen Shuangxi translation. Rock Geochemistry [M]. China University of Technology Press, (2000)

Google Scholar