Appalachian-style multi-terrane Wilson cycle model for the assembly of South China: COMMENT
Résumé
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.
Domaines
TectoniqueOrigine | Publication financée par une institution |
---|
Loading...