The Limpopo magma‐rich transform margin, South Mozambique – Part 1: Insights from deep‐structure seismic imaging

Type Article
Date 2021-12
Language English
Author(s) Watremez L.ORCID1, Leroy S.ORCID2, D’acremont E.2, Roche V.ORCID2, Evain MikaelORCID3, Leprêtre A.3, Verrier Fanny3, Aslanian DanielORCID3, Dias N.ORCID4, 5, Afilhado A.4, 5, Schnurle PhilippeORCID3, Castilla R.6, Despinois F.7, Moulin MarylineORCID3
Affiliation(s) 1 : Univ. Lille CNRS Univ. Littoral Côte d’Opale IRD UMR 8187 – LOG – Laboratoire d’Océanologie et de Géosciences F‐59000 Lille ,France
2 : Sorbonne Université CNRS Institut des Sciences de la Terre de Paris UMR 7193 ISTeP Paris,France
3 : IFREMER REM/GM/LGS Centre de Brest Plouzané, France
4 : Instituto Dom Luis (IDL) Faculdade das Ciências Universidade de Lisboa Campo Grande1749‐016 Lisboa, Portugal
5 : Instituto Superior de Engenharia de Lisboa Instituto Politécnico de Lisboa 1959‐007 Lisboa, Portugal
6 : Géo‐Energie Zürich,Switzerland
7 : TotalEnergies SE R&D Sustainability Pau, France
Source Tectonics (0278-7407) (American Geophysical Union (AGU)), 2021-12 , Vol. 40 , N. 12 , P. e2021TC006915 (29p.)
DOI 10.1029/2021TC006915
WOS© Times Cited 2
Keyword(s) transform margin, Mozambique, magmatism, seismic refraction
Abstract

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 (1) delineate the major regional crustal domains; (2) identify widespread indications of magmatic activity; and (3) 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: (1) on land, continental crust is overlain by a >10 km thick volcano-sedimentary wedge related to an early rifting stage, (2) offshore, thick oceanic crust formed due to intense magmatic activity, and between the two (3) 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 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.

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Watremez L., Leroy S., D’acremont E., Roche V., Evain Mikael, Leprêtre A., Verrier Fanny, Aslanian Daniel, Dias N., Afilhado A., Schnurle Philippe, Castilla R., Despinois F., Moulin Maryline (2021). The Limpopo magma‐rich transform margin, South Mozambique – Part 1: Insights from deep‐structure seismic imaging. Tectonics, 40(12), e2021TC006915 (29p.). Publisher's official version : https://doi.org/10.1029/2021TC006915 , Open Access version : https://archimer.ifremer.fr/doc/00737/84860/