A polyorogenic model for the Paleoproterozoic Trans-North China Belt: Insights from an integrated structural, metamorphic and geochronological study.

Pierre Trap; Michel Faure; Wei Lin; Patrick Monié; Olivier Bruguier; Nicole Le Breton

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A polyorogenic model for the Paleoproterozoic Trans-North China Belt: Insights from an integrated structural, metamorphic and geochronological study.

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A polyorogenic model for the Paleoproterozoic Trans-North China Belt: Insights from an integrated structural, metamorphic and geochronological study.

Pierre Trap, Michel Faure, Wei Lin, Patrick Monié, Olivier Bruguier et Nicole Le Breton

Geophysical Research Abstracts (Baltimore, United States, 2006)

2006

Résumé

In the North China Craton, the Paleoproterozoic Trans-North China Belt (TNCB) is a nearly north-south trending zone, of 1200 km long and 300 km wide, that separates two Archean blocks. Previous tectonic models assumed that the TNCB is the result of a 1850 Ma collision between the two Archean eastern and western blocks with an intervening 2500 Ma magmatic arc.

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Titre: A polyorogenic model for the Paleoproterozoic Trans-North China Belt: Insights from an integrated structural, metamorphic and geochronological study.
Créateurs - sans rôle: Pierre Trap - Institut des Sciences de la Terre d'Orléans
Michel Faure - Institut des Sciences de la Terre d'Orléans
Wei Lin - State Key Laboratory of Lithospheric Evolution
Patrick Monié - Laboratoire Dynamique de la Lithosphère
Olivier Bruguier - Institut des Sciences de la Terre
Nicole Le Breton - Institut des Sciences de la Terre d'Orléans
Colloque: Geophysical Research Abstracts (Baltimore, United States, 2006)
Identifiants: 9947911909311
Unité académique: Université de Montpellier
Langue: English
Type de ressource: Conference proceeding
Champs locaux: hal-00085504