Fluid origin and evolution of Cu-Pb-Zn mineralization in rhyolite breccias in the Lón area, southeastern Iceland-Reference-Cited by-同舟云学术

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Fluid origin and evolution of Cu-Pb-Zn mineralization in rhyolite breccias in the Lón area, southeastern Iceland

Published:2018-01 Issue: Volume:349 Page:177-191
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Kremer Christopher H.,Bird Dennis K.

Funder

Stanford University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference74 articles.

1. The fluid geochemistry of Icelandic high temperature geothermal areas;Ármannsson;Appl. Geochem.,2016

2. Geothermal systems in Iceland: structure and conceptual models—I. High-temperature areas;Arnórsson;Geothermics,1995

3. Summary of sulfeur isotope standards;Ault,1963

4. Modelling of temperature conditions near the bottom of well IDDP-1 in Krafla, Northeast Iceland;Axelsson;Geothermics,2014

5. Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: evidence for magmatic digestion and erosion of Pleistocene hyaloclastites;Bindeman;Geochim. Cosmochim. Acta,2008

Cited by 1 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Chlorine isotope ratios record magmatic brine assimilation during rhyolite genesis;Geochemical Perspectives Letters;2021-01

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