Characteristics of Lead and Zinc Polymetallic Deposit and Wall Rock Alteration Zoning in Luziyuan, Yunnan

Lei Zeng; Ming Guo Deng; Chang Liang Lv; Wei Liu

doi:10.4028/www.scientific.net/AMR.734-737.52

Paper Titles

Analysis for the Global Distribution and Requirement of the Copper Resources
p.32

Application of 3D Apparent Physical Properties Inversion Method in an Iron Mine Area
p.37

Applications of Conventional Logs in Low Resistivity Contrast Tight Gas Reservoirs Identification
p.41

Characteristics of Coal and Gas Outburst within Gas Geological Units in Qidong Mine
p.45

Characteristics of Lead and Zinc Polymetallic Deposit and Wall Rock Alteration Zoning in Luziyuan, Yunnan
p.52

Estimation of In Situ Stresses by Using Hydraulic Fracturing and Welllogging Data in Shizhuangnan Coalbed Methane Field
p.56

Formation Age of the Qinling Complex and the early Paleozoic Tectonic Event
p.60

Framework of Sequence Stratigraphy Sedimentary System and Evolution of Yimin Formation in Yimin Depression
p.71

Geochemistry of Huyanshan Alkaline Complex, Shanxi Province, China: Evidences for the Sources of Magma
p.81

HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 734-737Characteristics of Lead and Zinc Polymetallic...

Characteristics of Lead and Zinc Polymetallic Deposit and Wall Rock Alteration Zoning in Luziyuan, Yunnan

Abstract:

The lead and zinc polymetallic deposit in LuziYuan is an ultra-large type skarn deposit. The ore body originated from the interlayer crushed zone between the second and thrid section of stratum marble and slate (schist) interbedding of upper Cambrian series Shahechang group, the wall rock alteration is intensice in the diggings, and the alteration zoning is obvious. Through field geological investigation and data analysis, based on the petrography of alterated rocks and combined with catalog information of drilling, the wall rock alteration in the diggings of LuziYuan is divided into four alteration zones,which are in sequence: carbonate-quartz-chloritization zone; carbonate-quartz-skarn lithification zone; skarn-lead zinc ore mineralization zone; and skarn-pyritization zone. The forming of ore body is related to alterations such as skarn lithification, silicification, marmarization, magnetite, etc.

You might also be interested in these eBooks

View Preview

Info:

Periodical:

Advanced Materials Research (Volumes 734-737)

Pages:

52-55

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.734-737.52

Citation:

Cite this paper

Online since:

August 2013

Authors:

Lei Zeng, Ming Guo Deng, Chang Liang Lv, Wei Liu

Keywords:

Characteristics of Mineralization, Lead Deposit, LuziYuan, Wall Rock Alteration Zoning, Yunnan, Zinc Deposit

Export:

RIS, BibTeX

Price:

Permissions CCC:

Request Permissions

Permissions PLS:

Request Permissions

Сopyright:

Citation:

References

[1] Wenwei Dong, Shaoling Chen. The Characteristics Genesis of Luziyuan Pb-Zn Deposit, Zhen Kang [J].Yunnan geological, 2007, 26(4):404-410(in Chinese).

Google Scholar

[2] Xiaofeng Yang, Gang Luo. A tentative analysis of the ore controlling factors of the Luziyuan lead -Zinc deposit in Zhenkang area, Yunnan [J]. Geological Bulletin of China, 2011, 30（7）; 1137 - 1146(in Chinese).

DOI: 10.4028/www.scientific.net/amr.734-737.26

Google Scholar

[3] Wenwei Dong.Metallogenic conditions and typical ore deposit metallogenic model, Zhen Kang [J].Yunnan geological, 2007, 26 (1): 56—61(In Chinese).

Google Scholar

[4] Qinglin Xia, Yongqing Chen, Yingxiang Lu, Chengxing Jiang, Hongguang Liu and Zhi cheng Lv. 2 005. Geochemistry, Fluid Inclusions and Stable Isotope Studies of Luziyuan Pb-Zn deposit, in Y- unnan province, southwestern China [J]. Earth Science Journal of China University of Geosciences, 30(2): 177-186 (in Chinese).

Google Scholar

[5] Feilin Zhu ,Yan Tao, Rui zhong Hu, , Ming yang Liao, Yinxi Wang, Yubang Li. 2011.For ming age of the Luziyuan Pb-Zn deposit in Zhenkang,Yunnan[J]. Bulletin of Mineral ogy, Petrology and Geochemistry, 30(1): 73- 79(In Chinese).

Google Scholar