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Global tectonic settings and deep mantle control on Hg and Au-Hg deposits Read chapter Read first chapter

2005 | OriginalPaper | Chapter

Numerical simulations of heat and mass transfer for the Tongchang porphyry copper deposit, Dexing, Jiangxi province, China

Authors : Jiankang Li, Dehui Zhang, Denghong Wang

Published in: Mineral Deposit Research: Meeting the Global Challenge

Publisher: Springer Berlin Heidelberg

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Numerical simulations of heat and mass transfer have been used to investigate the genesis of the Tongchang porphyry copper deposit, China. Early stages of hydrothermal activity are predicted to have been dominated magmatic-derived fluids, with fluid flow centred on granodiorite contact zones. During the middle period of hydrothermal activity, there was potential for mixing of magmatic water and groundwater. Late stage hydrothermal activity is predicted to have been dominated by groundwater convection.

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previous chapter Mass-balance analysis of mineralized skarn systems: Implications for replacement processes, carbonate mobility, and permeability evolution
next chapter Magmatic Ni-Cu-PGE deposits in the Qilian-Longshou mountains, Northwest China — part of a Proterozoic large igneous province
Metadata
Title
Numerical simulations of heat and mass transfer for the Tongchang porphyry copper deposit, Dexing, Jiangxi province, China
Authors
Jiankang Li
Dehui Zhang
Denghong Wang
Copyright Year
2005
Publisher
Springer Berlin Heidelberg
Book
Mineral Deposit Research: Meeting the Global Challenge

Print ISBN: 978-3-540-27945-7

Electronic ISBN: 978-3-540-27946-4

Copyright Year: 2005

DOI
https://doi.org/10.1007/3-540-27946-6_111