Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)

The upwelling mantle within the Banda Sea is modeled using computer visualization techniques. The Banda Sea is considered a triple junction of the Pacific, Australian, and Eurasian Plates within the plate tectonic hypothesis. Evaluation of mantle depths from gravity and seismic studies indicates upw...

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Main Authors: Bruce A. Leybourne, Michael B. Adams
Format: Article
Language:English
Published: International Institute of Informatics and Cybernetics 2020-08-01
Series:Journal of Systemics, Cybernetics and Informatics
Subjects:
Online Access:http://www.iiisci.org/Journal/CV$/sci/pdfs/IP093LL20.pdf
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spelling doaj-47654ee1dbe14739be129c90204f70e22021-03-27T18:09:50ZengInternational Institute of Informatics and CyberneticsJournal of Systemics, Cybernetics and Informatics1690-45242020-08-0118497106Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)Bruce A. LeybourneMichael B. AdamsThe upwelling mantle within the Banda Sea is modeled using computer visualization techniques. The Banda Sea is considered a triple junction of the Pacific, Australian, and Eurasian Plates within the plate tectonic hypothesis. Evaluation of mantle depths from gravity and seismic studies indicates upwelling of mantle from approximately 30-40 km under the continental shelf of Australia to 21 km in the Banda Arc. From here the mantle rises to 14 km within the Weber Deep and finally reaches a depth of 7 km in the North Banda Sea. Seismic epicenter data delineate spatial boundaries of flow regimes and define magmatic migration routes. Epicenter magnitudes are visualized in 3 dimensions by color-coding. Topographic and bathymetric data from in-house sources define geographic position and geomorphology of the model domain, while altimetry data delineate the gravity field associated with a component of mantle dynamics using contour lines or interpolated color fields. Conceptual animation portrays upwelling and divergence of mantle flow structures (geostreams) underlying the tectonic trends of the region and the resulting counterflow within the volcanic arcs based on the surge tectonic hypothesis. This animation uses a series of color-coded arrows and particle systems to represent these flow structures in motion. Induced micro-gravity oscillations in the triple junction may be caused by planetary gravity waves. This phenomenon is explored to determine the coupling effects with the atmospheric pressure flux of the southern oscillation, which modulates El Nino.http://www.iiisci.org/Journal/CV$/sci/pdfs/IP093LL20.pdf surge tectonic vortexbanda seaensotriple junctionmantle dynamics
collection DOAJ
language English
format Article
sources DOAJ
author Bruce A. Leybourne
Michael B. Adams
spellingShingle Bruce A. Leybourne
Michael B. Adams
Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)
Journal of Systemics, Cybernetics and Informatics
surge tectonic vortex
banda sea
enso
triple junction
mantle dynamics
author_facet Bruce A. Leybourne
Michael B. Adams
author_sort Bruce A. Leybourne
title Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)
title_short Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)
title_full Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)
title_fullStr Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)
title_full_unstemmed Modeling Mantle Dynamics in the Banda Sea Triple Junction – Exploring a Possible Link to El Niño Southern Oscillation (Revisited)
title_sort modeling mantle dynamics in the banda sea triple junction – exploring a possible link to el niño southern oscillation (revisited)
publisher International Institute of Informatics and Cybernetics
series Journal of Systemics, Cybernetics and Informatics
issn 1690-4524
publishDate 2020-08-01
description The upwelling mantle within the Banda Sea is modeled using computer visualization techniques. The Banda Sea is considered a triple junction of the Pacific, Australian, and Eurasian Plates within the plate tectonic hypothesis. Evaluation of mantle depths from gravity and seismic studies indicates upwelling of mantle from approximately 30-40 km under the continental shelf of Australia to 21 km in the Banda Arc. From here the mantle rises to 14 km within the Weber Deep and finally reaches a depth of 7 km in the North Banda Sea. Seismic epicenter data delineate spatial boundaries of flow regimes and define magmatic migration routes. Epicenter magnitudes are visualized in 3 dimensions by color-coding. Topographic and bathymetric data from in-house sources define geographic position and geomorphology of the model domain, while altimetry data delineate the gravity field associated with a component of mantle dynamics using contour lines or interpolated color fields. Conceptual animation portrays upwelling and divergence of mantle flow structures (geostreams) underlying the tectonic trends of the region and the resulting counterflow within the volcanic arcs based on the surge tectonic hypothesis. This animation uses a series of color-coded arrows and particle systems to represent these flow structures in motion. Induced micro-gravity oscillations in the triple junction may be caused by planetary gravity waves. This phenomenon is explored to determine the coupling effects with the atmospheric pressure flux of the southern oscillation, which modulates El Nino.
topic surge tectonic vortex
banda sea
enso
triple junction
mantle dynamics
url http://www.iiisci.org/Journal/CV$/sci/pdfs/IP093LL20.pdf
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AT michaelbadams modelingmantledynamicsinthebandaseatriplejunctionexploringapossiblelinktoelninosouthernoscillationrevisited
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