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Seafloor topography and tectonic elements of the Western Indian Ocean

Seafloor topography and tectonic elements of the Western Indian Ocean
Seafloor topography and tectonic elements of the Western Indian Ocean
The break-up of Gondwanaland and dispersal of several of its component continental fragments, which eventually formed the margins of the Indian Ocean, have produced an ocean basin of enormous variety, both in relief and in origin of seafloor features. The western half of the Indian Ocean alone contains every type of tectonic plate boundary, both active and fossil, and, along with some of the deepest fracture zones, the most complex mid-ocean ridge configurations and some of the thickest sedimentary sequences in the world's ocean basins. This ocean is one of the most diverse on the face of the globe. We explore the evolution of the morphology of the Indian Ocean floor, and discuss the effect of its variations, maxima and minima, on the interconnectivity of the ocean's water masses.
Indian Ocean, bathymetry, tectonic tvolution
1364-503X
15-24
Parson, L.M.
8985a003-911e-402e-a858-3ecbd09d6771
Evans, A.J.
4492478c-e994-42bf-b943-97844eda8230
Parson, L.M.
8985a003-911e-402e-a858-3ecbd09d6771
Evans, A.J.
4492478c-e994-42bf-b943-97844eda8230

Parson, L.M. and Evans, A.J. (2005) Seafloor topography and tectonic elements of the Western Indian Ocean. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 363 (1826), 15-24. (doi:10.1098/rsta.2004.1472).

Record type: Article

Abstract

The break-up of Gondwanaland and dispersal of several of its component continental fragments, which eventually formed the margins of the Indian Ocean, have produced an ocean basin of enormous variety, both in relief and in origin of seafloor features. The western half of the Indian Ocean alone contains every type of tectonic plate boundary, both active and fossil, and, along with some of the deepest fracture zones, the most complex mid-ocean ridge configurations and some of the thickest sedimentary sequences in the world's ocean basins. This ocean is one of the most diverse on the face of the globe. We explore the evolution of the morphology of the Indian Ocean floor, and discuss the effect of its variations, maxima and minima, on the interconnectivity of the ocean's water masses.

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Published date: 2005
Keywords: Indian Ocean, bathymetry, tectonic tvolution
Organisations: National Oceanography Centre,Southampton

Identifiers

Local EPrints ID: 14867
URI: http://eprints.soton.ac.uk/id/eprint/14867
ISSN: 1364-503X
PURE UUID: 66239379-b3e1-4e0e-b972-c217fe09e2ab

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Date deposited: 07 Mar 2005
Last modified: 15 Mar 2024 05:32

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Author: L.M. Parson
Author: A.J. Evans

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