ON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINS

Cross-spectral techniques have been used to analyze the relationship between free air gravity anomalies and topography of approx 100 profiles over the continental margins of E North America, SW Africa, and the Coral Sea/Lord Howe Rise. The resulting admittance functions for these margins have been i...

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Main Authors: Karner, G, Watts, A
Format: Journal article
Language:English
Published: 1982
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author Karner, G
Watts, A
author_facet Karner, G
Watts, A
author_sort Karner, G
collection OXFORD
description Cross-spectral techniques have been used to analyze the relationship between free air gravity anomalies and topography of approx 100 profiles over the continental margins of E North America, SW Africa, and the Coral Sea/Lord Howe Rise. The resulting admittance functions for these margins have been interpreted in terms of the flexure model of isostasy. The relatively young Coral Sea/Lord Howe rise margin is associated with the lowest value of the effective elastic thickness (Te<5km), while the relatively old E North American margin is associated with the highest value (10
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spelling oxford-uuid:2dca9db2-76fa-408f-a91d-c4be83b0c4a72022-03-26T12:45:09ZON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINSJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:2dca9db2-76fa-408f-a91d-c4be83b0c4a7EnglishSymplectic Elements at Oxford1982Karner, GWatts, ACross-spectral techniques have been used to analyze the relationship between free air gravity anomalies and topography of approx 100 profiles over the continental margins of E North America, SW Africa, and the Coral Sea/Lord Howe Rise. The resulting admittance functions for these margins have been interpreted in terms of the flexure model of isostasy. The relatively young Coral Sea/Lord Howe rise margin is associated with the lowest value of the effective elastic thickness (Te<5km), while the relatively old E North American margin is associated with the highest value (10
spellingShingle Karner, G
Watts, A
ON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINS
title ON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINS
title_full ON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINS
title_fullStr ON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINS
title_full_unstemmed ON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINS
title_short ON ISOSTASY AT ATLANTIC-TYPE CONTINENTAL MARGINS
title_sort on isostasy at atlantic type continental margins
work_keys_str_mv AT karnerg onisostasyatatlantictypecontinentalmargins
AT wattsa onisostasyatatlantictypecontinentalmargins