A simple magma-driven thermal balance model for the formation of volcanogenic massive sulphides
- 28 October 2002
- journal article
- Published by Elsevier
- Vol. 76 (1-2) , 123-134
- https://doi.org/10.1016/0012-821x(85)90153-0
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Flow rates in the axial hot springs of the East Pacific Rise (21°N): Implications for the heat budget and the formation of massive sulfide depositsEarth and Planetary Science Letters, 1984
- Chemistry of solutions from the 13°N East Pacific Rise hydrothermal siteEarth and Planetary Science Letters, 1984
- Constraints on the structure of the East Pacific Rise from seismic refraction dataJournal of Geophysical Research, 1982
- Black smokers fuelled by freezing magmaNature, 1982
- Chemistry of hot springs on the East Pacific Rise and their effluent dispersalNature, 1982
- East Pacific rise at 21°N: The volcanic, tectonic, and hydrothermal processes of the central axisEarth and Planetary Science Letters, 1981
- Hydrothermal activity at mid-ocean ridge axesNature, 1981
- Hydrothermal heat flux of the “black smoker” vents on the East Pacific RiseEarth and Planetary Science Letters, 1980
- Seismic evidence for a narrow zone of partial melting underlying the East Pacific Rise at 21°NGSA Bulletin, 1977
- Geology, geochemistry, and genesis of Cyprus sulfide depositsEconomic Geology, 1973