Archean Terrane Docking Upper Crust Collision Tectonics

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- The northern NVZ and southern volcanic zones SVZ of the Abitibi greenstone belt are separated by the major E-trending Destor-Porcupine-Manneville fault zone DPMFZ . The DPMFZ is interpreted to be the locus of Archean terrane docking between the older diffuse volcanic arc of the NVZ 2730-2710 .Archean terrane docking: upper crust collision tectonics,. Abitibi greenstone belt, Quebec, Canada 1 a . W.U. Mueller , , R. Daigneault a, J.K. Mortensen b, E.H. Chown c a Sciences de la Term, Univ. du Quibec gt Chicoutimi, Quebec, G7H 2B1, Canada h Department of Geological Sciences, University of British Columbia, ..le: Archean terrane docking: upper crust collision tectonics, Abitibi greenstone belt, Quebec, Canada. Authors: Mueller, W. U.; Daigneault, R.; Mortensen, J. K.; Chown, E. H Affiliation: AA Sciences de la Terre, Univ. du Quebec a Chicoutimi, Quebec, G7H 2B1, Canada , AB Sciences de la Terre, Univ. du Quebec a .The northern NVZ and southern volcanic zones SVZ of the Abitibi greenstone belt are separated by the major E-trending Destor-Porcupine-Manneville fault zone DPMFZ . The DPMFZ is interpreted to be the locus of Archean terrane docking between the older diffuse volcanic arc of the NVZ 2730-2710 Ma and the .

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