Journal articles
Appalachian-style multi-terrane Wilson cycle model for the assembly of South China: COMMENT
Abstract : Lin et al. (2018) propose a model of Proterozoic-Mesozoic evolution of the South China block (SCB) involving West and East Cathaysia
separated by the Northwest Fujian fault. They assume a northeastward translation of East Cathaysia after an Early Paleozoic orogeny due to the
collision of West Cathaysia with a “proposed terrane”. This model ignores most of the available, robust field data.
Cited literature [11 references]
https://hal-insu.archives-ouvertes.fr/insu-01818014
Contributor : Nathalie Pothier Connect in order to contact the contributor
Submitted on : Sunday, December 16, 2018 - 8:48:16 AM
Last modification on : Monday, January 24, 2022 - 4:42:03 PM
Long-term archiving on: : Sunday, March 17, 2019 - 12:11:12 PM
Contributor : Nathalie Pothier Connect in order to contact the contributor
Submitted on : Sunday, December 16, 2018 - 8:48:16 AM
Last modification on : Monday, January 24, 2022 - 4:42:03 PM
Long-term archiving on: : Sunday, March 17, 2019 - 12:11:12 PM
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