Reply to comment on ‘The challenge in restoring magma-rich rifted margins: The example of the Mozambique-Antarctica conjugate margins’ (Gondwana Research, 2021, 95 29–44)

Author:

Tomasi Simon,Kusznir Nick,Manatschal Gianreto,Despinois Frank

Publisher

Elsevier BV

Subject

Geology

Reference15 articles.

1. Aslanian D., Moulin M., 2012. Paleogeographic consequences of conservational models in the South Atlantic Ocean, In: Mohriak, W.U., Danforth, A., Post, P.J., Brown, D.E., Tari, G.C., Nemcok, M. and Sinha, S.T. (eds). Conjugate Divergent Margins. Geological Society, London, Special Publications, 369, http://dx.doi.org/10.1144/SP369.5.

2. Geology and hydrocarbon potential of the East African continental margin: a review;Davison;Pet. Geosci.,2018

3. Deep structure of the Santos Basin-São Paulo Plateau System;Evain;SE Brazil: Journal of Geophysical Research, Solid Earth,2015

4. Karner, G.D., C. Johnson, J. Shoffner, M. Lawson, M. Sullivan, J. Sitgreaves, J. McHarge, J. Stewart and P. Figueredo, 2021. Tectono-magmatic development of the Santos and Campos basins, offshore Brazil. In Mello, Yilmaz and Katz (Eds), The supergiant lower Cretaceous pre-salt petroleum systems of the Santos Basin. AAPG Memoir 124, 215-256.

5. Leroy S., V. Roche, F. Guillocheau, P. Dietrich, S. Revillon, L. Watremez, C. Robin, F. Despinois, W. Vetel. 2020. Magma-rich transform margins: example from the Limpopo transform fault zone between Mozambique and Antarctica. EGU General Assembly, 2020. Vienna. EGU2020-10508

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