Conference papers
A polyorogenic model for the Paleoproterozoic Trans-North China Belt: Insights from an integrated structural, metamorphic and geochronological study.
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.
https://hal-insu.archives-ouvertes.fr/hal-00085504
Contributor : Nathalie POTHIER Connect in order to contact the contributor
Submitted on : Wednesday, August 9, 2006 - 9:25:34 AM
Last modification on : Tuesday, August 2, 2022 - 3:50:23 AM
Long-term archiving on: : Tuesday, April 6, 2010 - 12:06:25 AM
Contributor : Nathalie POTHIER Connect in order to contact the contributor
Submitted on : Wednesday, August 9, 2006 - 9:25:34 AM
Last modification on : Tuesday, August 2, 2022 - 3:50:23 AM
Long-term archiving on: : Tuesday, April 6, 2010 - 12:06:25 AM