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
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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