TY  - JOUR
AU  - Brendan Murphy, J.
AU  - Gutiérrez Alonso, Gabriel
AU  - Nance, R. Damian
AU  - Fernández Suárez, Javier
AU  - Duncan Keppie, James
AU  - Quesada Ochoa, Cecilio
AU  - Strachan, Robin A.
AU  - Dostal, Jarda
PY  - 2006
DO  - 10.1130/G22068.1
SN  - 0091-7613, ESSN: 1943-2682
UR  - https://hdl.handle.net/20.500.14352/52738
T2  - Geology
AB  - The Rheic Ocean is widely believed to have formed in the Late Cambrian–Early Ordovician as a result of the drift of peri-Gondwanan terranes, such as Avalonia and Carolina, from the northern margin of Gondwana, and to have been consumed in the Devonian...
LA  - eng
M2  - 325
PB  - Geological Society of America
KW  - Pangea
KW  - Rheic Ocean
KW  - Neoproterozoic suture
KW  - Sm-Nd data
KW  - terranes
TI  - Origin of the Rheic Ocean: Rifting along a Neoproterozoic suture?
TY  - journal article
VL  - 34
ER  -