Title :

The Limpopo Magma-Rich Transform Margin, South Mozambique: 1. Insights From Deep-Structure Seismic Imaging

Author(s) :

Watremez, L. [Auteur]
Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
Leroy, S. [Auteur]
Institut des Sciences de la Terre de Paris [iSTeP]
d'Acremont, E. [Auteur]
Institut des Sciences de la Terre de Paris [iSTeP]
Roche, V. [Auteur]
Institut des Sciences de la Terre de Paris [iSTeP]
Evain, M. [Auteur]
Institut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
Leprêtre, A. [Auteur]
Institut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
Verrier, F. [Auteur]
Institut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
Aslanian, D. [Auteur]
Institut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
Dias, N. [Auteur]
Afilhado, A. [Auteur]
Schnürle, P. [Auteur]
Institut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
Castilla, R. [Auteur]
Despinois, F. [Auteur]
Moulin, M. [Auteur]
Institut Français de Recherche pour l'Exploitation de la Mer [IFREMER]

Journal title :

TECTONICS

Publisher :

American Geophysical Union (AGU)

Publication date :

2021

ISSN :

0278-7407

English keyword(s) :

magmatism
seismic refraction
transform margin
Mozambique

HAL domain(s) :

Planète et Univers [physics]
Planète et Univers [physics]/Sciences de la Terre

English abstract : [en]

A variety of structures results from the interplay of evolving far-field forces, plate kinematics, and magmatic activity during continental break-up. The east Limpopo transform margin, offshore northern Mozambique, formed ...
Show more >A variety of structures results from the interplay of evolving far-field forces, plate kinematics, and magmatic activity during continental break-up. The east Limpopo transform margin, offshore northern Mozambique, formed as Africa and Antarctica separated during the mid-Jurassic period break-up of the Gondwana supercontinent. The nature of the crust onshore has been discussed for decades in an effort to resolve issues with plate kinematic models. Two seismic refraction profiles with coincident multichannel seismic reflection profiles allow us to interpret the seismic velocity structures across the margin, both onshore and offshore. These seismic profiles allow us to (a) delineate the major regional crustal domains; (b) identify widespread indications of magmatic activity; and (c) map crustal structure and geometry of this magma-rich transform margin. Careful examination of the profiles allows us to make the following observations and interpretations: (a) on land, continental crust is overlain by a >10-km thick volcano-sedimentary wedge related to an early rifting stage, (b) offshore, thick oceanic crust formed due to intense magmatic activity, and between the two (c) a 50-60-km wide transform zone where the crustal structures are affected by intense magmatic activity and faulting. The prominent presence of intrusive and extrusive igneous units may be attributed to the combination of a deep-seated melting anomaly and a trans-tensional fault zone running through thinned lithosphere that allowed melt to reach the surface. A comparison of the crustal thinning along other transform margins shows a probable dependence with the thermal and/or tectonic history of the lithosphere.Show less >

Language :

Anglais

Peer reviewed article :

Oui

Audience :

Internationale

Popular science :

Non

Collections :

• Laboratoire d'Océanologie et de Géosciences (LOG) - UMR 8187

Source :

Harvested from HAL