Origin and history of development of the Bransfield Straight (based on DSS data interpretation)

Essential difference in the structure of the earth’s crust of the northwestern continental margins of the Trinity peninsula (suboceanic) and Graham Coast (subcontinental) has been shown on the base of DSS data analysis. In agreement with similarity of geomorphologic elements on both sides of Bransfi...

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Main Authors: Yu.V. Kozlenko, M. V. Kozlenko
Format: Article
Language:English
Published: Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine 2012-04-01
Series:Геофизический журнал
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/116613
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author Yu.V. Kozlenko
M. V. Kozlenko
author_facet Yu.V. Kozlenko
M. V. Kozlenko
author_sort Yu.V. Kozlenko
collection DOAJ
description Essential difference in the structure of the earth’s crust of the northwestern continental margins of the Trinity peninsula (suboceanic) and Graham Coast (subcontinental) has been shown on the base of DSS data analysis. In agreement with similarity of geomorphologic elements on both sides of Bransfield Trough it has been shown that the Antarctic Peninsula and South-Shetland islands could be a single structure that was a reason to come to conclusion on the probable origin of the straight as a result of spreading motion apart of the bottom as a result of riftogenesis. Using GPS observations data it was calculated that the opening of the Bransfield Straight could begin within the interval of 26-37 mil years ago, i.e. in the Late Paleogene - Early Neogene. A scheme of the history of the Bransfield Straight development has been proposed on the base of seismic models interpretation.
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publishDate 2012-04-01
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spelling doaj-art-d47cfa5d3f754ae98a9a1dbc0b94e7dc2025-06-27T10:14:38ZengSubbotin Institute of Geophysics of the National Academy of Sciences of UkraineГеофизический журнал0203-31002524-10522012-04-0134210.24028/gzh.0203-3100.v34i2.2012.116613Origin and history of development of the Bransfield Straight (based on DSS data interpretation)Yu.V. Kozlenko0M. V. Kozlenko1Institute of Geophysics of the National Academy of Sciences of UkraineInstitute of Geophysics of the National Academy of Sciences of UkraineEssential difference in the structure of the earth’s crust of the northwestern continental margins of the Trinity peninsula (suboceanic) and Graham Coast (subcontinental) has been shown on the base of DSS data analysis. In agreement with similarity of geomorphologic elements on both sides of Bransfield Trough it has been shown that the Antarctic Peninsula and South-Shetland islands could be a single structure that was a reason to come to conclusion on the probable origin of the straight as a result of spreading motion apart of the bottom as a result of riftogenesis. Using GPS observations data it was calculated that the opening of the Bransfield Straight could begin within the interval of 26-37 mil years ago, i.e. in the Late Paleogene - Early Neogene. A scheme of the history of the Bransfield Straight development has been proposed on the base of seismic models interpretation.https://journals.uran.ua/geofizicheskiy/article/view/116613
spellingShingle Yu.V. Kozlenko
M. V. Kozlenko
Origin and history of development of the Bransfield Straight (based on DSS data interpretation)
Геофизический журнал
title Origin and history of development of the Bransfield Straight (based on DSS data interpretation)
title_full Origin and history of development of the Bransfield Straight (based on DSS data interpretation)
title_fullStr Origin and history of development of the Bransfield Straight (based on DSS data interpretation)
title_full_unstemmed Origin and history of development of the Bransfield Straight (based on DSS data interpretation)
title_short Origin and history of development of the Bransfield Straight (based on DSS data interpretation)
title_sort origin and history of development of the bransfield straight based on dss data interpretation
url https://journals.uran.ua/geofizicheskiy/article/view/116613
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