A trans-Iapetus transform fault control for the evolution of the Rheic Ocean: Implications for an early Paleozoic transition of accretionary tectonics: Reply

Author:

Wu Lei12,Murphy J. Brendan3ORCID,Collins William J.4,Waldron John W.F.5,Li Zheng-Xiang4,Pisarevsky Sergei A.46,Halverson Galen P.1

Affiliation:

1. 1Department of Earth & Planetary Sciences, McGill University, 3450 Rue University, Montréal, Québec H3A 0E8, Canada

2. 2Department of Physics, University of Alberta, Edmonton, Alberta T6G 2E1, Canada

3. 3Department of Earth and Environmental Sciences, St. Francis Xavier University, Antigonish, Nova Scotia B2G 2W5, Canada

4. 4Earth Dynamics Research Group, The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, Western Australia 6845, Australia

5. 5Department of Earth & Atmospheric Sciences, University of Alberta, Edmonton, Alberta 26G 2E3, Canada

6. 6Institute of the Earth's Crust, Siberian Branch of the Russian Academy of Sciences, ul. Lermontova 128, Irkutsk 664033, Russia

Publisher

Geological Society of America

Reference19 articles.

1. The Paxton Group in southeastern New England: U.S. Geological Survey Bulletin 1814;Barosh,1988

2. OVERVIEW: Neoproterozoic-Paleozoic geography and tectonics: Review, hypothesis, environmental speculation;Dalziel;Geological Society of America Bulletin,1997

3. The Virgilina deformation, a late Precambrian to Early Cambrian (?) orogenic event in the central Piedmont of Virginia and North Carolina;Glover;American Journal of Science,1973

4. The Virgilina deformation: Implications of stratigraphic correlation in the Carolina slate belt: Carolina Geological Society Field Trip Guide;Harris,1985

5. The regional extent of the ca. 600 Ma Virgilina deformation: Implications for stratigraphic correlation in the Carolina terrane;Harris;Geological Society of America Bulletin,1988

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