Back-arc underplating provided crustal accretion affecting topography and sedimentation in the Adria microplate

Објеката

Тип
Рад у часопису
Верзија рада
објављена верзија
Језик
енглески
Креатор
Paolo Mancinelli, Vittorio Scisciani, Cristina Pauselli, Gérard M. Stampfli, Fabio Speranza, Ivana Vasiljević
Извор
Marine and Petroleum Geology
Издавач
Elsevier Ltd.
Датум издавања
2021
Сажетак
Supported by evidence of deep crustal sources for the observed magnetic anomalies in Central Italy and by outcropping gabbros in the Croatian archipelago, we model the observed gravity and magnetic anomalies in the Central Adriatic Sea and surroundings. We suggest that the major magnetic anomalies in the area are related to a wide underplating and propose that this volume represents the first stage of the back-arc Adria continental breakup in Early Permian times. During the Palaeotethys-Adria collision, underplating has controlled topography and palaeogeographic domains resulting in the observed asymmetrical sedimentary evolution since the Triassic across the Adria microplate. Finally, we propose that the Palaeotethys-Adria boundary in the Early Permian was similar to the current Pacific-Okhotsk plate boundary.
том
136, February 2022, 105470
Број
136
број страница
12
doi
10.1016/j.marpetgeo.2021.105470
issn
0264-8172
Subject
Underplating, akrecija kore, Magnetske anomalije, Jadranska ploča
Underplating, Crustal accretion, Magnetic anomalies, Adria plate
Шира категорија рада
M20
Ужа категорија рада
М21
Права
Затворени приступ
Лиценца
All rights reserved
Формат
.pdf
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Ивана Васиљевић
Radovi istraživača

Paolo Mancinelli, Vittorio Scisciani, Cristina Pauselli, Gérard M. Stampfli, Fabio Speranza, Ivana Vasiljević. "Back-arc underplating provided crustal accretion affecting topography and sedimentation in the Adria microplate" in Marine and Petroleum Geology, Elsevier Ltd. (2021). https://doi.org/10.1016/j.marpetgeo.2021.105470

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