Rift and plate boundary evolution across two supercontinent cycles-Reference-Cited by-同舟云学术

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Rift and plate boundary evolution across two supercontinent cycles

Published:2019-02 Issue: Volume:173 Page:1-14
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Merdith Andrew S.,Williams Simon E.,Brune Sascha,Collins Alan S.,Müller R. Dietmar

Funder

Australian Research Council

Deep Energy Community of the Deep Carbon Observatory

Helmholtz Young Investigators Group CRYSTALS

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference140 articles.

1. Incompatible Ediacaran paleomagnetic directions suggest an equatorial geomagnetic dipole hypothesis;Abrajevitch;Earth Planet. Sci. Lett.,2010

2. U-Pb ages of metarhyolites of the Catoctin and Mount Rogers Formations, central and southern Appalachians: evidence for two pulses of Iapetan rifting;Aleinikoff;Am. J. Sci.,1995

3. Kinematic evolution of the Araçuaí-West Congo orogen in Brazil and Africa: nutcracker tectonics during the Neoproterozoic assembly of Gondwana;Alkmim;Precambrian Res.,2006

4. Genesis of the Tonian Imorona-Itsindro Magmatic Suite in Central Madagascar: Insights from U-Pb, oxygen and hafnium isotopes in zircon;Archibald;Precambrian Res.,2016

5. Tonian Arc Magmatism in Central Madagascar: the Petrogenesis of the Imorona-Itsindro Suite;Archibald;J. Geol.,2017

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