Petrology, Thermochronology and Structural Evolution of Metamorphic-Core Complex
A special issue of Minerals (ISSN 2075-163X).
Deadline for manuscript submissions: closed (31 May 2022) | Viewed by 728
Special Issue Editors
Interests: tectonics; structural geology; exhumation processes; metamorphic core complexes; syn-extensional granitoid intrusives; sedimentary basins; active tectonics
Interests: granites geochemistry; igneous petrology; isotope geochemistry; mineral chemistry; rare earth element mineralization; soil characterization
Special Issues, Collections and Topics in MDPI journals
Interests: tectonics; thermochronology; geochronology; provenance studies; exhumation; structural geology; metamorphic petrology and petrochronology
Special Issue Information
Dear Colleagues,
Metamorphic core complexes (MCCs) are crustal-scale dome-shaped structures associated with the extensional or diapiric structural exhumation of mid- to lower-crustal rocks on continental and oceanic settings. These rocks have been exhumed through the brittle–ductile transition by a crustal-scale normal-sense brittle–ductile shear zones and/or discrete brittle detachment faults and structurally juxtaposed against upper-crustal rocks with markedly different tectonothermal and/or metamorphic histories. While the initiation and geometric evolution of MCCs remain controversial, they have been documented in a plethora of continental and oceanic tectonic settings, ranging from syn- and post-orogenic in nature in collisional belts, back-arc, rifted and hyperextended continental margins, to oceanic spreading centers. Lower-plate rocks in metamorphic core complexes are often characterized by intense ductile and brittle deformation, progressive exhumation, metamorphism, and magmatism. Brittle faulting, magmatism, and the dynamic thermal evolution in metamorphic core complex can also lead to hydrothermal fluid circulation and ore deposit formation. Novel and integrated approaches, including field-based, analytical, numerical, and analogue models, are shedding new light on the geometric, mechanical, temporal, and thermal evolution of MCCs. The main subjects of this Special Issue include but are not limited to:
- Geometric and structural evolution of the MCC footwall and hanging wall;
- Petrological and hydrothermal or metasomatic evolution MCCs;
- Mechanical and thermal evolution of MCCs;
- Pressure–Temperature evolution of footwall and hanging wall rocks;
- Syn- and post-tectonic magmatism and MCCs;
- Ore formation and deposition in MCCs and detachments.
We look forward to receiving your contributions.
Dr. Konstantinos Soukis
Dr. Christina Stouraiti
Prof. Dr. Daniel Stockli
Guest Editors
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Keywords
- metamorphic core complex
- detachment
- mylonite
- low-T thermochronology
- syn-extensional intrusives
- fluid circulation
- ore formation
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