Mechanism of Paleo-Mesoproterozoic rifts related to breakup of Columbia supercontinent: A paleostress field modeling-Reference-Cited by-同舟云学术

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Mechanism of Paleo-Mesoproterozoic rifts related to breakup of Columbia supercontinent: A paleostress field modeling

Published:2017-06 Issue: Volume:107 Page:46-60
ISSN:0264-3707
Container-title:Journal of Geodynamics
language:en
Short-container-title:Journal of Geodynamics

Author:

Sun Shuai,Hou Guiting,Hari K.R.,Liu Shuwen,Guan Shuwei

Funder

National Natural Science Foundation of China

State Key Projects

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference121 articles.

1. Paleoproterozoic mafic dyke swarms from the Dharwar craton; paleomagnetic poles for India from 2.37 to 1.88Ga and rethinking the Columbia supercontinent;Belica;Precambrian Res.,2014

2. The stress regime associated with continental break-up;Bott;Geol. Soc. Lond. Spec. Publ.,1992

3. Asymmetric three-dimensional topography over mantle plumes;Burov;Nature,2014

4. Lithosphere, Mechanical Properties;Burov,2011

5. Effects of rock mechanical properties on local stress field of the Mahanadi basin, India-results from finite element modeling;Chatterjee;Geophys. Res. Lett.,2002

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2. Late Paleoproterozoic mafic-intermediate dykes from the southern margin of the North China Craton: Implication for magma source and Columbia reconstruction;Precambrian Research;2020-09

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