The geological setting of Matra ore deposit (France): insights from lithostratigraphy and polyphase deformation history

Arsenic sulfide mineralization in Matra mine (southern Alpine Corsica) is hosted by two tectonic units belonging to the Schistes Lustrés Complex. Country rocks include a Jurassic ophiolitic sequence and related sedimentary covers, which were metamorphosed. Geological mapping and thin section analysi...

Full description

Saved in:
Bibliographic Details
Main Authors: Danis Ionut Filimon, Giacomo Vannucci, Alessandro La Rosa, Vincenzo Zarone, Maria Di Rosa
Format: Article
Language:English
Published: Taylor & Francis Group 2024-12-01
Series:Journal of Maps
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/17445647.2024.2394502
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Arsenic sulfide mineralization in Matra mine (southern Alpine Corsica) is hosted by two tectonic units belonging to the Schistes Lustrés Complex. Country rocks include a Jurassic ophiolitic sequence and related sedimentary covers, which were metamorphosed. Geological mapping and thin section analysis were used to understand lithostratigraphy and the tectononic-metamorphic history. The polyphase deformation history includes four phases of ductile deformation during the Late Cretaceous–Early Oligocene Alpine orogeny, with associated high-pressure–low-temperature metamorphism culminating in eclogite facies. The post-Alpine phase includes an N–S extensional fault system that controls the movement of ore fluids.
ISSN:1744-5647