Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions

Abstract Segmented magmatic arcs create arc‐parallel variable loads and influence associated foreland basins through flexural isostasy along strike, in addition to standard subduction‐perpendicular foredeep/forebulge/backbulge models. Segmentation occurs in both continental and island arcs (Aleutian...

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Published in:Terra Nova
Main Author: Martin, Keith
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1111/ter.12672
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12672
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spelling crwiley:10.1111/ter.12672 2024-04-07T07:53:44+00:00 Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions Martin, Keith 2023 http://dx.doi.org/10.1111/ter.12672 https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12672 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Terra Nova volume 35, issue 6, page 451-470 ISSN 0954-4879 1365-3121 Geology journal-article 2023 crwiley https://doi.org/10.1111/ter.12672 2024-03-14T00:40:42Z Abstract Segmented magmatic arcs create arc‐parallel variable loads and influence associated foreland basins through flexural isostasy along strike, in addition to standard subduction‐perpendicular foredeep/forebulge/backbulge models. Segmentation occurs in both continental and island arcs (Aleutians, Calabria, Japan, Kuril/Kamchatka, Lesser Antilles, Solomon Islands and Sumatra/Java). Some segments have variable gravity anomalies and elastic thicknesses ( T e ). In standard theory, the load created by an orogenic belt/magmatic arc depresses the lithosphere modelled as a thin elastic plate floating on a fluid mantle substrate, leading to an arc‐perpendicular foredeep, forebulge and backbulge. Arc‐parallel topographic and gravitational features should influence loading along strike in a similar way, resulting in a checkerboard pattern of foredeeps, forebulges and backbulges in both pro‐arc and retro‐arc foreland basins. This pattern exercises profound controls on sediment and facies distribution in a here‐to‐fore un‐envisaged manner, with implications for resource exploration in foreland basins. Article in Journal/Newspaper Kamchatka Wiley Online Library Terra Nova 35 6 451 470
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
topic Geology
spellingShingle Geology
Martin, Keith
Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions
topic_facet Geology
description Abstract Segmented magmatic arcs create arc‐parallel variable loads and influence associated foreland basins through flexural isostasy along strike, in addition to standard subduction‐perpendicular foredeep/forebulge/backbulge models. Segmentation occurs in both continental and island arcs (Aleutians, Calabria, Japan, Kuril/Kamchatka, Lesser Antilles, Solomon Islands and Sumatra/Java). Some segments have variable gravity anomalies and elastic thicknesses ( T e ). In standard theory, the load created by an orogenic belt/magmatic arc depresses the lithosphere modelled as a thin elastic plate floating on a fluid mantle substrate, leading to an arc‐perpendicular foredeep, forebulge and backbulge. Arc‐parallel topographic and gravitational features should influence loading along strike in a similar way, resulting in a checkerboard pattern of foredeeps, forebulges and backbulges in both pro‐arc and retro‐arc foreland basins. This pattern exercises profound controls on sediment and facies distribution in a here‐to‐fore un‐envisaged manner, with implications for resource exploration in foreland basins.
format Article in Journal/Newspaper
author Martin, Keith
author_facet Martin, Keith
author_sort Martin, Keith
title Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions
title_short Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions
title_full Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions
title_fullStr Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions
title_full_unstemmed Continental and island arc segmentation: Implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions
title_sort continental and island arc segmentation: implications for retro‐arc and pro‐arc foreland basin and backarc basin geometries and sediment distributions
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1111/ter.12672
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12672
genre Kamchatka
genre_facet Kamchatka
op_source Terra Nova
volume 35, issue 6, page 451-470
ISSN 0954-4879 1365-3121
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/ter.12672
container_title Terra Nova
container_volume 35
container_issue 6
container_start_page 451
op_container_end_page 470
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