supported by the Czech Science Foundation,Czechia(grant number 19-27682X to K.S.)。
The processes leading to the assembly of the Rodinia supercontinent through Grenvillian collisional orogeny are relatively well known.In contrast,accretionary orogenic processes occurring at the supercontinent periphe...
Final support for this study was jointly provided by the National Natural Science Foundation of China (Grant Nos.41802056,41972058,42030307);the China Postdoctoral Science Foundation (Grant2018M633554);the MOST Special Fund from the State Key Laboratory of Continental Dynamics (Grant 201210133);Young Talent fund of University Association for Science and Technology in Shaanxi,China (Grant20200703);China Geological Survey (Grant DD20190376).
The North Qaidam orogenic belt(NQOB) is generally considered to be an early Paleozoic ultrahigh pressure metamorphic belt,but increasing reports of the Neoproterozoic magmatic and metamorphic events indicate that the ...
Financial support over the last years was through Spanish MEC and MICINN grants CGL2005-02065/BTE and CGL2009-07984;UCM-Santander grant GR58/08;Argentinian grant 1728 AR PICT 1009
The role played by Paleoproterozoic cratons in southern South America from the Mesopro- terozoic to the Early Cambrian is reconsidered here. This period involved protracted continental amal- gamation that led to forma...