Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)

The Kallintiri area (SW Byala Reka–Kechros Dome, Rhodope) hosts a polymetallic (critical, base, and precious metals) ore deposit, tectonically controlled by the late Eocene–Oligocene, top-to-SW Kallintiri Detachment System. The earliest structure associated with the Kallintiri Detachment is a ductil...

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Main Authors: Konstantinos Soukis, Christos Kanellopoulos, Panagiotis Voudouris, Constantinos Mavrogonatos, Ilias Lazos, Sotiris Sboras, Alexandre Tarantola, Daniel Koehn, Robert Moritz
Format: Article
Language:English
Published: MDPI AG 2025-02-01
Series:Geosciences
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Online Access:https://www.mdpi.com/2076-3263/15/2/46
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author Konstantinos Soukis
Christos Kanellopoulos
Panagiotis Voudouris
Constantinos Mavrogonatos
Ilias Lazos
Sotiris Sboras
Alexandre Tarantola
Daniel Koehn
Robert Moritz
author_facet Konstantinos Soukis
Christos Kanellopoulos
Panagiotis Voudouris
Constantinos Mavrogonatos
Ilias Lazos
Sotiris Sboras
Alexandre Tarantola
Daniel Koehn
Robert Moritz
author_sort Konstantinos Soukis
collection DOAJ
description The Kallintiri area (SW Byala Reka–Kechros Dome, Rhodope) hosts a polymetallic (critical, base, and precious metals) ore deposit, tectonically controlled by the late Eocene–Oligocene, top-to-SW Kallintiri Detachment System. The earliest structure associated with the Kallintiri Detachment is a ductile shear zone at the interface between the high-grade footwall gneisses of the Lower and Intermediate Rhodope Terranes. The detachment zone encompasses the uppermost part of the gneisses and the ultramylonitic Makri Unit marble. The marble is bound by a brittle–ductile shear zone at the base and a knife-sharp, low-angle normal fault at the roof, exhibiting considerable brecciation and ultracataclasite development. The hanging wall includes the Makri Unit phyllites and the overlying mid–late-Eocene–Oligocene supra-detachment sediments, which show syn-depositional slump structures and brittle deformation with low- and high-angle faulting and non-cohesive cataclasites. Extensive hydrothermal fluid circulation along the detachment zone and through NW tension gashes and high-angle faults led to pronounced silicification and ore deposition. Field observations and mineralogical and geochemical analyses revealed two primary types of ore mineralization spatially and temporally associated with different structures. Base and precious metals-rich ores are associated with the detachment, while Sb ore deposition is localized mostly within the NW-trending tension gashes and high-angle faults.
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spelling doaj-art-93fe47ed8e8d4938aed80e6a9cfc05bc2025-08-20T03:12:14ZengMDPI AGGeosciences2076-32632025-02-011524610.3390/geosciences15020046Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)Konstantinos Soukis0Christos Kanellopoulos1Panagiotis Voudouris2Constantinos Mavrogonatos3Ilias Lazos4Sotiris Sboras5Alexandre Tarantola6Daniel Koehn7Robert Moritz8Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou, 15784 Athens, GreeceHellenic Survey of Geology and Mineral Exploration (HSGME), 1 Spirou Loui Str., Olympic Villa, Acharnae, 13677 Attiki, GreeceFaculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou, 15784 Athens, GreeceDepartment of Earth Sciences, University of Pisa, Via Santa Maria, 53, 56126 Pisa, ItalyInstitute of Geodynamics, National Observatory of Athens, Lofos Nymphon, Thesio, 11810 Athens, GreeceInstitute of Geodynamics, National Observatory of Athens, Lofos Nymphon, Thesio, 11810 Athens, GreeceGeoRessources UMR 7359, Faculté des Sciences et Technologies, Université de Lorraine, Boulevard des Aiguillettes, F-54506 Vandoeuvre-lès-Nancy, FranceGeoZentrum Nordbayern, Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU), Schlossgarten 5, 91054 Erlangen, GermanyHellenic Survey of Geology and Mineral Exploration (HSGME), 1 Spirou Loui Str., Olympic Villa, Acharnae, 13677 Attiki, GreeceThe Kallintiri area (SW Byala Reka–Kechros Dome, Rhodope) hosts a polymetallic (critical, base, and precious metals) ore deposit, tectonically controlled by the late Eocene–Oligocene, top-to-SW Kallintiri Detachment System. The earliest structure associated with the Kallintiri Detachment is a ductile shear zone at the interface between the high-grade footwall gneisses of the Lower and Intermediate Rhodope Terranes. The detachment zone encompasses the uppermost part of the gneisses and the ultramylonitic Makri Unit marble. The marble is bound by a brittle–ductile shear zone at the base and a knife-sharp, low-angle normal fault at the roof, exhibiting considerable brecciation and ultracataclasite development. The hanging wall includes the Makri Unit phyllites and the overlying mid–late-Eocene–Oligocene supra-detachment sediments, which show syn-depositional slump structures and brittle deformation with low- and high-angle faulting and non-cohesive cataclasites. Extensive hydrothermal fluid circulation along the detachment zone and through NW tension gashes and high-angle faults led to pronounced silicification and ore deposition. Field observations and mineralogical and geochemical analyses revealed two primary types of ore mineralization spatially and temporally associated with different structures. Base and precious metals-rich ores are associated with the detachment, while Sb ore deposition is localized mostly within the NW-trending tension gashes and high-angle faults.https://www.mdpi.com/2076-3263/15/2/46detachmentpolymetallic ore depositantimonymetamorphic core complexexhumationultramylonite
spellingShingle Konstantinos Soukis
Christos Kanellopoulos
Panagiotis Voudouris
Constantinos Mavrogonatos
Ilias Lazos
Sotiris Sboras
Alexandre Tarantola
Daniel Koehn
Robert Moritz
Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)
Geosciences
detachment
polymetallic ore deposit
antimony
metamorphic core complex
exhumation
ultramylonite
title Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)
title_full Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)
title_fullStr Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)
title_full_unstemmed Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)
title_short Investigating the Structure of Detachment Faulting and Its Role in Ore Formation: The Kallintiri Detachment System and the Associated Polymetallic Ore Deposit (Rhodope, NE Greece)
title_sort investigating the structure of detachment faulting and its role in ore formation the kallintiri detachment system and the associated polymetallic ore deposit rhodope ne greece
topic detachment
polymetallic ore deposit
antimony
metamorphic core complex
exhumation
ultramylonite
url https://www.mdpi.com/2076-3263/15/2/46
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