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The Montagne Noire Variscan gneiss dome (southern French Massif Central) has been extensively studied, but interpretations of geochronology data remain highly debated. In tribute to Jean-Louis Paquette\u2019s work, we first present the results of the last 10 yr of reflection on our knowledge of the Montagne Noire dome, highlighting the various contributions of LA-ICPMS U-Th-Pb geochronology. Then, based on new structural, petrological and U-Th-Pb data obtained in the southeastern part of the Montagne Noire Axial Zone (MNAZ), in \u201cLes Gorges d\u2019H\u00e9ric\u201d valley, we provide new insight into the structure and strain partitioning in this region and propose the existence of a crustal-scale dextral shear zone that we name the \u201cGorges d\u2019H\u00e9ric Shear Zone\u201d (GHSZ). The LA-ICPMS U-Th-Pb age on monazite, obtained on a pegmatite cross-cutting vertical structures on the southern margin of the GHSZ, constrains the end of ductile deformation at\n                    <jats:italic>ca.<\/jats:italic>\n                    295 Ma in that part of the shear zone. Further north, a localized deformation corridor is accompanied by significant fluid circulation recorded in retrogressed metamafic lenses. Petrographic observations reveal a complex mineralogical evolution characterised by the formation of garnet, amphibole, orthopyroxene, and secondary spinel, interpreted as the product of fluid-driven mineral reactions. Potassium metasomatism is responsible for the development of syn-kinematic biotite. The final retrograde stage is marked by the development of amphibole\u2009+\u2009chlorite assemblages and late serpentinization reactions. U-Th-Pb results obtained on zircon grains highlight a long and complex geological history. Three age populations have been identified and associated with: (1) the magmatic protolith emplacement likely to be linked to early Paleozoic event(s), (2) the existence of a\n                    <jats:italic>ca.<\/jats:italic>\n                    315 Ma event interpreted as a high-grade metamorphic imprint and (3) a last corresponding to most of the zircon U-Pb data gives a concordia age of 280.6\u2009\u00b1\u20092.5 Ma, interpreted as the age of zircon (re)crystallization during localized deformation and aqueous fluid circulation along the GHSZ, probably related to the well-known early Permian regional volcanic episode. Within the GHSZ, the geochronological dataset spans the period from 320 Ma to 280 Ma, suggesting that this is a significant structure.\n                  <\/jats:p>","DOI":"10.1051\/bsgf\/2025012","type":"journal-article","created":{"date-parts":[[2025,4,24]],"date-time":"2025-04-24T14:42:38Z","timestamp":1745505758000},"page":"23","source":"Crossref","is-referenced-by-count":2,"title":["Permian fluid circulation and deformation along a crustal-scale shear zone in the Montagne Noire gneiss dome (southern French Massif Central)"],"prefix":"10.1051","volume":"196","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-3621-0213","authenticated-orcid":false,"given":"Fran\u00e7oise","family":"Roger","sequence":"first","affiliation":[{"name":"Geosciences Montpellier, Campus Triolet, Universit\u00e9 de Montpellier, CNRS","place":["France"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Pierre","family":"Trap","sequence":"additional","affiliation":[{"name":"UMR 6249 Chrono-environnement, Universit\u00e9 de Bourgogne-Franche-Comt\u00e9","place":["France"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Christian","family":"Teyssier","sequence":"additional","affiliation":[{"name":"Department of Earth and Environment Sciences, University of Minnesota \u2212 Twin Cities","place":["USA"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Donna L.","family":"Whitney","sequence":"additional","affiliation":[{"name":"Department of Earth and Environment Sciences, University of Minnesota \u2212 Twin Cities","place":["USA"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Jean-Louis","family":"Paquette","sequence":"additional","affiliation":[{"name":"Laboratoire Magmas et Volcans (CNRS-UMR 6524), Campus Universitaire des C\u00e9zeaux","place":["France"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Cl\u00e9mentine","family":"Hamelin","sequence":"additional","affiliation":[{"name":"Department of Earth and Environment Sciences, University of Minnesota \u2212 Twin Cities","place":["USA"]},{"name":"Geology department, College of William and Mary","place":["USA"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Jean-Patrick","family":"Respaut","sequence":"additional","affiliation":[{"name":"Geosciences Montpellier, Campus Triolet, Universit\u00e9 de Montpellier, CNRS","place":["France"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"No\u00ebllie","family":"Co\u00ebffier","sequence":"additional","affiliation":[{"name":"UMR 6249 Chrono-environnement, Universit\u00e9 de Bourgogne-Franche-Comt\u00e9","place":["France"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Jonas","family":"Vanardois","sequence":"additional","affiliation":[{"name":"Department of Earth and Environment Sciences, University of Minnesota \u2212 Twin Cities","place":["USA"]},{"name":"Institute of Earth Sciences, University of Lausanne","place":["Switzerland"]}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Patrice F.","family":"Rey","sequence":"additional","affiliation":[{"name":"School of Geosciences, University of Sydney","place":["Australia"]}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"250","published-online":{"date-parts":[[2025,12,3]]},"reference":[{"key":"R1","doi-asserted-by":"crossref","first-page":"62","DOI":"10.1029\/97TC02342","volume":"17","author":"Aerden","year":"1998","journal-title":"Tectonics"},{"key":"R2","doi-asserted-by":"crossref","first-page":"1321","DOI":"10.1016\/S0191-8141(99)00098-X","volume":"21","author":"Aerden","year":"1999","journal-title":"J Struct Geol"},{"key":"R3","unstructured":"Alabouvette B, Demange M, Gu\u00e9rang\u00e9-Lozes J, Ambert P. 2003. 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