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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 1 Michel Faure 1 Wei Lin 2 Patrick Monié 3 Olivier Bruguier 4 Nicole Le Breton 1
1 ISTO - Institut des Sciences de la Terre d'Orléans
2 SKL - State Key Laboratory of Lithospheric Evolution
3 LDL - Laboratoire Dynamique de la Lithosphère
4 ISTEEM - Institut des Sciences de la Terre, de l'Environnement et de l'Espace de Montpellier
Abstract : 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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https://hal-insu.archives-ouvertes.fr/hal-00085504
Contributor : Nathalie Pothier <>
Submitted on : Wednesday, August 9, 2006 - 9:25:34 AM
Last modification on : Wednesday, August 14, 2019 - 8:32:01 PM
Long-term archiving on: : Tuesday, April 6, 2010 - 12:06:25 AM

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Pierre Trap, Michel Faure, Wei Lin, Patrick Monié, Olivier Bruguier, et al.. A polyorogenic model for the Paleoproterozoic Trans-North China Belt: Insights from an integrated structural, metamorphic and geochronological study.. Geophysical Research Abstracts, 2006, Baltimore, United States. ⟨hal-00085504⟩

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