Geology and Petrology of Ophiolites
A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".
Deadline for manuscript submissions: closed (11 September 2020) | Viewed by 12136
Special Issue Editor
Special Issue Information
Dear Colleagues,
Ophiolites represent fragments of the upper mantle and oceanic crust that were incorporated into continental margins during continent–continent and arc-continent collisions, ridge-trench interactions, and/or subduction-accretion events. Ophiolite units (peridotite, gabbro, subvolcanic, and volcanic complexes) have varying internal structures, geochemical affinities, and age ranges, and can become tectonically juxtaposed in collision zones. They originally formed in different geodynamic settings, including continental margins, mid-ocean ridges, and suprasubduction zones. Incorporated into subduction-accretion complexes of active margins and later into orogenic belts, ophiolites may be highly dismembered, may have diverse lithological assemblages, metamorphic grades, styles of deformation, and geochemical affinities. Although ophiolite structure, geochemical affinities, and emplacement mechanisms have been debated for several decades, new data on previously studied and newly found ophiolite complexes all over the world may provide better understanding of magmatic processes in oceanic settings and the evolution of orogenic belts.
This Special Issue accepts original research and reviews related to the geology, geochemistry, mineralogy, and ore potential of various types of ophiolites in orogenic belts of various ages.
Dr. Eugene Sklyarov
Guest Editor
Manuscript Submission Information
Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.
Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Minerals is an international peer-reviewed open access monthly journal published by MDPI.
Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.
Keywords
- Ophiolite
- Peridotite
- Gabbro
- Volcanic rocks
- Geochemistry
- Mineralogy
- Mechanism of emplacement