Early post-breakup kinematic adjustments of continental-oceanic transform fault zones: Cape Range, Coromandal and Romanche transform margin case study

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F22%3A10249198" target="_blank" >RIV/61989100:27350/22:10249198 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.lyellcollection.org/doi/pdf/10.1144/SP524-2021-110?download=true" target="_blank" >https://www.lyellcollection.org/doi/pdf/10.1144/SP524-2021-110?download=true</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1144/SP524-2021-110" target="_blank" >10.1144/SP524-2021-110</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Early post-breakup kinematic adjustments of continental-oceanic transform fault zones: Cape Range, Coromandal and Romanche transform margin case study

Popis výsledku v původním jazyce

A comparison of transform margins that started their evolution as continental transforms shows differences in their tectonic style, which can be attributed to the variable kinematic adjustments they underwent during the post-breakup continental-oceanic stage of their development. The Cape Range transform fault zone (Western Australia) retained its strike-slip character during its entire continental-oceanic stage, as documented by the transform-perpendicular system of spreading related magnetic stripe anomalies. The Coromandal transform fault zone (Eastern India) adjusted its kinematics to a transtensional one during its continental-oceanic stage, as indicated by the transform-oblique system of magnetic stripe anomalies and extensional component of movement indicated by a narrow zone of crustal thinning. The Romanche transform fault zone adjusted its kinematics to transpressional, as documented by the changing geometries of magnetic stripe anomalies and transpressional folding during its continental-oceanic development stage.

Název v anglickém jazyce

Early post-breakup kinematic adjustments of continental-oceanic transform fault zones: Cape Range, Coromandal and Romanche transform margin case study

Popis výsledku anglicky

A comparison of transform margins that started their evolution as continental transforms shows differences in their tectonic style, which can be attributed to the variable kinematic adjustments they underwent during the post-breakup continental-oceanic stage of their development. The Cape Range transform fault zone (Western Australia) retained its strike-slip character during its entire continental-oceanic stage, as documented by the transform-perpendicular system of spreading related magnetic stripe anomalies. The Coromandal transform fault zone (Eastern India) adjusted its kinematics to a transtensional one during its continental-oceanic stage, as indicated by the transform-oblique system of magnetic stripe anomalies and extensional component of movement indicated by a narrow zone of crustal thinning. The Romanche transform fault zone adjusted its kinematics to transpressional, as documented by the changing geometries of magnetic stripe anomalies and transpressional folding during its continental-oceanic development stage.

Druh

C - Kapitola v odborné knize

CEP obor

—

OECD FORD obor

10500 - Earth and related environmental sciences

Projekt

—

Návaznosti

N - Vyzkumna aktivita podporovana z neverejnych zdroju

Rok uplatnění

2022

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název knihy nebo sborníku

Geological Society Special Publication. Volume 524

ISBN

978-1-78620-571-1

Počet stran výsledku

27

Strana od-do

70-97

Počet stran knihy

256

Název nakladatele

Geological Society of London

Místo vydání

Londýn

Kód UT WoS kapitoly

—