Use this URL to cite or link to this record in EThOS: https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.792613
Title: Kinematic and paleobathymetric evolution of the South Atlantic basin
Author: Perez Diaz, Lucia
ISNI:       0000 0004 8499 3328
Awarding Body: Royal Holloway, University of London
Current Institution: Royal Holloway, University of London
Date of Award: 2017
Availability of Full Text:
Access from EThOS:
Access from Institution:
Abstract:
The opening of the South Atlantic ocean is one of the most extensively researched problems in plate kinematics. An accurate representation of the plate motions that led to the growth of this ocean basin is crucial to understanding the dynamics of its margins, the formation of petroleum systems and the driving mechanisms behind present and past water circulation patterns. General agreement exists about ocean opening being the result of the diachronous separation of two major plates (South American and African), having involved a certain degree of intracontinental deformation. However, for a fuller understanding, the bathymetric evolution also needs to be considered. I model oceanic growth as depicted by seafloor spreading data (fracture zone traces and magnetic anomalies). I present the results of this model as an animated tectonic reconstruction. Spreading started at 138 Ma, with movement along intracontinental accommodation zones leading to the assembly of South America by 123 Ma and Africa by 106 Ma. The model also provides an explanation for the inception and evolution of the Malvinas plate and its connection with the formation of a LIP south of the Falkland-Agulhas Fracture Zone. I challenge the view of narrow deformation belts as the sole sites of stress accommodation during continental separation and discuss the implications of the kinematic model in terms of the distribution of intracontinental strain. Subsequently, I use a high-resolution seafloor age grid, derived from the plate kinematic model presented, to model the subsidence of oceanic lithosphere as a function of its age by applying plate-cooling theory. Then, I refine this thermal surface to account for other factors that affect bathymetry at smaller scales or amplitudes, both within the ocean and the continent-ocean transition zones (here sedimentation, variable crustal thickness and mantle fluctuations). Despite of the uncertainties that this workflow introduces in the resulting model, which I describe and quantify, the paleobathymetric reconstructions are a big step forward (both in resolution and accuracy) from previous attempts at modelling the changes in seafloor depth through time in the South Atlantic. The final products are a series of paleobathymetric reconstructions of the South Atlantic, which, together with the plate kinematic model provide a complete picture of its evolution from Cretaceous times to present.
Supervisor: Not available Sponsor: Not available
Qualification Name: Thesis (Ph.D.) Qualification Level: Doctoral
EThOS ID: uk.bl.ethos.792613  DOI: Not available
Keywords: geodynamics ; plate tectonics ; plate kinematics ; south atlantic ; paleobathymetry ; computer modelling ; geology ; earth sciences ; Geodynamic modelling ; geophysics ; passive margins ; extended continental margins
Share: