Petrology and Geochemistry of Igneous Rocks Linked to Volcanogenic Massive Sulphides
A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".
Deadline for manuscript submissions: closed (20 May 2021) | Viewed by 5398
Special Issue Editors
Interests: petrology and geochemistry of igneous rocks, including granitoids and volcanic rocks; mineralization associated to magmatism; palaeovolcanology; major- and trace element geochemistry; hydrothermal alteration related to mineralization; isotopic geochemistry; U-Pb dating of igneous and hydrothermal rocks
Special Issues, Collections and Topics in MDPI journals
Interests: petrology and geochemistry of altered volcanic rocks; isotopic geochemistry; U-Pb dating of igneous rocks; palaeovolcanology; physical volcanology
Special Issues, Collections and Topics in MDPI journals
Interests: petrology and geochemistry of igneous rocks; including granitoids and volcanic rocks; mineralization associated to magmatism; palaeovolcanology; major- and trace element geochemistry; hydrothermal alteration related to mineralization; isotopic geochemistry; U-Pb dating of igneous and hydrothermal rocks
Special Issues, Collections and Topics in MDPI journals
Special Issue Information
Dear Colleagues,
Volcanogenic massive sulphide (VMS) deposits are accumulations of sulphide minerals that precipitate from hydrothermal fluids at or below the seafloor in a wide range of geological environments. Today, VMS maintain a high economic interest.
As VMS deposits are linked to igneous rocks both in space and time, much attention has previously been paid to the mutual relations of magmatism and VMS mineralization, aiming at the determination of those features of the igneous rocks that could be useful as a proxy of VMS. Accordingly, research has been focused in recent years both on volcanology and on petrology/geochemistry, including isotope geology.
In spite of a number of significant advances, and due to the highly variable characteristics of VMS deposits and their related magmatic rocks (including contrasts in geological setting, magma generation, thermal flow, and hydrothermal circulation), their mutual relationships are still only partly understood.
The goal of this Special Issue of Minerals is to show an updated perspective of this important matter, in order to improve both our theoretical knowledge on this link and our exploration tools applied to VMS exploration. We warmly encourage researchers in these fields to join us in this challenging effort.
Prof. Dr. Emilio Pascual
Dr. Teodosio Donaire
Dr. Manuel Toscano
Guest Editors
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Keywords
- VMS deposits
- magmatism
- petrology
- (paleo)volcanology
- geochemistry
- isotope geology