Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data

Magnetic data from the northeastern Indian Ocean reveal east-west trending magnetic lineations 28 through 34, an abandoned spreading center (ASC) and part of the Cretaceous Magnetic Quiet Zone (CMQZ), which are used to reconstruct past tectonic processes involved in the evolution of the ocean. Offse...

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Main Authors: Krishna, K.S., Rao, D.G.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2000
Subjects:
Online Access:http://drs.nio.org/drs/handle/2264/1673
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spelling ftnio:oai:dsr.nio.org:2264/1673 2023-05-15T13:59:28+02:00 Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data Krishna, K.S. Rao, D.G. 2000 http://drs.nio.org/drs/handle/2264/1673 en eng Elsevier Copyright [2000]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository. palaeomagnetism plate tectonics seismic reflection profiles spreading centres fracture zones hotspots Journal Article 2000 ftnio 2012-08-25T20:05:46Z Magnetic data from the northeastern Indian Ocean reveal east-west trending magnetic lineations 28 through 34, an abandoned spreading center (ASC) and part of the Cretaceous Magnetic Quiet Zone (CMQZ), which are used to reconstruct past tectonic processes involved in the evolution of the ocean. Offsets in the magnetic lineations outline the existence of four N-S trending fracture zones: 80 degrees E, Indira, 84.5 degrees E, and 86 degrees E. The 84.5 degrees E Fracture Zone (FZ) acts as a boundary separating oceanic crust with different magnetic isochron patterns. The pairs of magnetic lineations 30 through 32n.2 between the 86 degrees E FZ and the Ninetyeast Ridge reveal an ASC of about 65 Ma age; parallel to approx. equal to 0.5 degrees S latitude. the structure of the ASC is well-identified in seismic reflection data as an undulating basement topographic rise covered by up to 2 km of Bengal Fan sediments. The spreading center might have initiated its activity along with other spreading centers of the Wharton Ridge and India-Antarctica Ridge, after the first major plate reorganization of the Indian Ocean (about 95 plus or minus 5 Ma), but ceased shortly after formation of anomaly 30 (about 65 Ma). Then it jumped southward between anomalies 32n.2 and 33. The jump captured the oceanic crust of anomalies 30 through 32n.2 that initially formed on the Antarctica plate, but were later transferred to the Indian plate. The spreading centers in the vicinity of the Ninetyeast Ridge jumped several times southward, to maintain a close proximity to the Kerguelen hotspot Article in Journal/Newspaper Antarc* Antarctica National Institute of Oceanography, India: Digital Repository Service (DRS@nio) Kerguelen Indian Wharton ENVELOPE(157.817,157.817,-81.050,-81.050)
institution Open Polar
collection National Institute of Oceanography, India: Digital Repository Service (DRS@nio)
op_collection_id ftnio
language English
topic palaeomagnetism
plate tectonics
seismic reflection profiles
spreading centres
fracture zones
hotspots
spellingShingle palaeomagnetism
plate tectonics
seismic reflection profiles
spreading centres
fracture zones
hotspots
Krishna, K.S.
Rao, D.G.
Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data
topic_facet palaeomagnetism
plate tectonics
seismic reflection profiles
spreading centres
fracture zones
hotspots
description Magnetic data from the northeastern Indian Ocean reveal east-west trending magnetic lineations 28 through 34, an abandoned spreading center (ASC) and part of the Cretaceous Magnetic Quiet Zone (CMQZ), which are used to reconstruct past tectonic processes involved in the evolution of the ocean. Offsets in the magnetic lineations outline the existence of four N-S trending fracture zones: 80 degrees E, Indira, 84.5 degrees E, and 86 degrees E. The 84.5 degrees E Fracture Zone (FZ) acts as a boundary separating oceanic crust with different magnetic isochron patterns. The pairs of magnetic lineations 30 through 32n.2 between the 86 degrees E FZ and the Ninetyeast Ridge reveal an ASC of about 65 Ma age; parallel to approx. equal to 0.5 degrees S latitude. the structure of the ASC is well-identified in seismic reflection data as an undulating basement topographic rise covered by up to 2 km of Bengal Fan sediments. The spreading center might have initiated its activity along with other spreading centers of the Wharton Ridge and India-Antarctica Ridge, after the first major plate reorganization of the Indian Ocean (about 95 plus or minus 5 Ma), but ceased shortly after formation of anomaly 30 (about 65 Ma). Then it jumped southward between anomalies 32n.2 and 33. The jump captured the oceanic crust of anomalies 30 through 32n.2 that initially formed on the Antarctica plate, but were later transferred to the Indian plate. The spreading centers in the vicinity of the Ninetyeast Ridge jumped several times southward, to maintain a close proximity to the Kerguelen hotspot
format Article in Journal/Newspaper
author Krishna, K.S.
Rao, D.G.
author_facet Krishna, K.S.
Rao, D.G.
author_sort Krishna, K.S.
title Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data
title_short Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data
title_full Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data
title_fullStr Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data
title_full_unstemmed Abandoned Paleocene spreading center in the northeastern Indian Ocean: evidence from magnetic and seismic reflection data
title_sort abandoned paleocene spreading center in the northeastern indian ocean: evidence from magnetic and seismic reflection data
publisher Elsevier
publishDate 2000
url http://drs.nio.org/drs/handle/2264/1673
long_lat ENVELOPE(157.817,157.817,-81.050,-81.050)
geographic Kerguelen
Indian
Wharton
geographic_facet Kerguelen
Indian
Wharton
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_rights Copyright [2000]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
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