Proceedings of the 2015 Asia-Pacific Energy Equipment Engineering Research Conference

C, H, O, S, Pb Isotope Geochemistry and the Implications of Qixiashan Pb-Zn-Ag Polymetallic Deposit in Jiangsu Province

Authors
Mingchao Zhang, Yongsheng Li, Xiaofei Yu, Wenbin Jia
Corresponding Author
Mingchao Zhang
Available Online June 2015.
DOI
10.2991/ap3er-15.2015.50How to use a DOI?
Keywords
isotope geochemistry; source of ore-forming materials; Pb-Zn-Ag polymetallic deposit; Qixiashan; Nanjing
Abstract

Qixiashan Pb-Zn-Ag polymetallic deposit in Jiangsu Province is located in the Yangtze continental block-the Lower Yangtze block zone-central of the Lower Yangtze foreland basin, and is a large polymetallic deposit dominated by Pb and Zn. We have carried out the C and O isotope tests of calcite at the main mineralization stage, H and O isotope tests of quartz at the main mineralization stage, as well as S and Pb isotope analyses and testing of typical sulfide ores in the deposit. The results showed that the 13CV-PDB=-1‰~1.2‰, 18OV-SMOW=14.1‰~21.6‰ of calcite in limestones, 13CV-PDB=-4.9‰~1.9‰, 18OV-SMOW=9.1‰~19.6‰ of calcite in ores. This indicates that carbon largely derived from magma at the main mineralization stage of the deposit, and part of the carbon might come from dissolution of marine carbonate. Quart at main mineralization stage showed D=-81.8‰~-67‰ and 18O=-0.38‰~6.25‰, indicating that ore-forming fluid was mainly magmatic water. And with the progress of mineralization, the mineralization feature of magmatic and meteoric water mixing was revealed. Sulfur isotope ranged in a narrow area from -4.4‰ to 3.6‰ at the main mineralization stage, showing that the main source of sulfur was the magma, and mixed with sedimentary sulfur from the surrounding rocks. The test results for Pb isotopes at main mineralization stage were 206Pb/204Pb=17.62~17.82, 207Pb/204Pb=15.51~15.72, 208Pb/204Pb=37.91~38.59, indicating the lead was not from a single source of the crust or mantle, and it should be a combination of lead from the upper mantle and the crust brought by magmatic activities.

Copyright
© 2015, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

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Volume Title
Proceedings of the 2015 Asia-Pacific Energy Equipment Engineering Research Conference
Series
Advances in Engineering Research
Publication Date
June 2015
ISBN
10.2991/ap3er-15.2015.50
ISSN
2352-5401
DOI
10.2991/ap3er-15.2015.50How to use a DOI?
Copyright
© 2015, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

Cite this article

TY  - CONF
AU  - Mingchao Zhang
AU  - Yongsheng Li
AU  - Xiaofei Yu
AU  - Wenbin Jia
PY  - 2015/06
DA  - 2015/06
TI  - C, H, O, S, Pb Isotope Geochemistry and the Implications of Qixiashan Pb-Zn-Ag Polymetallic Deposit in Jiangsu Province
BT  - Proceedings of the 2015 Asia-Pacific Energy Equipment Engineering Research Conference
PB  - Atlantis Press
SP  - 214
EP  - 218
SN  - 2352-5401
UR  - https://doi.org/10.2991/ap3er-15.2015.50
DO  - 10.2991/ap3er-15.2015.50
ID  - Zhang2015/06
ER  -