A polyorogenic model for the Paleoproterozoic Trans-North China Belt: Insights from an integrated structural, metamorphic and geochronological study. - Archive ouverte HAL Access content directly
Conference Papers Year : 2006

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

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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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Dates and versions

hal-00085504 , version 1 (09-08-2006)

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  • HAL Id : hal-00085504 , version 1

Cite

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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