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Titlebook: Neogenic Evolution of the Mediterranean Region; Geodynamics, Tectoni Enzo Mantovani,Marcello Viti,Caterina Tamburelli Book 2024 The Editor(

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發(fā)表于 2025-3-21 17:20:49 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Neogenic Evolution of the Mediterranean Region
副標(biāo)題Geodynamics, Tectoni
編輯Enzo Mantovani,Marcello Viti,Caterina Tamburelli
視頻videohttp://file.papertrans.cn/663/662553/662553.mp4
概述Serves as an overview of tectonics in the Mediterranean.Discusses implications of plate tectonics.Provides alternative interpretations
圖書封面Titlebook: Neogenic Evolution of the Mediterranean Region; Geodynamics, Tectoni Enzo Mantovani,Marcello Viti,Caterina Tamburelli Book 2024 The Editor(
描述.This book deals with a controversially discussed topic about the Mediterranean tectonic evolution, underlying the basic role of extrusion processes. Alternative interpretations of Mediterranean back-arc basins are discussed to complete the picture. The kinematics of the confining plates is discussed as well. Understanding the geodynamics that determined the evolution of the Mediterranean area may have important implications for other regions of the world. The recognition of the ongoing tectonic processes may help to identify possible regularities in the distribution of major earthquakes, allowing a better estimate of the long-period seismic hazard..
出版日期Book 2024
關(guān)鍵詞Plate kinematics; Trench-Arc-Back Arc systems; Major earthquakes in the central Mediterranean; Nubia-Eu
版次1
doihttps://doi.org/10.1007/978-3-031-62150-5
isbn_softcover978-3-031-62152-9
isbn_ebook978-3-031-62150-5
copyrightThe Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl
The information of publication is updating

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發(fā)表于 2025-3-21 21:37:47 | 只看該作者
Neogenic Evolution,erved tectonic events in the Mediterranean region. The basic concept underlying the proposed view is that the tectonic evolution of the study area, with particular regard to the generation of trench-arc-back arc systems, was mainly controlled by the lateral escape of buoyant structures, driven by th
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Magmatism and Tectonics in the Central Mediterranean,n of the Neogene magmatic activity in the central Mediterranean region. In particular, the available evidence strongly supports the hypothesis that the uprise of magmas through the upper crust is considerably facilitated (or even conditioned) by the formation of transtensional fault systems. The pre
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Enzo Mantovani,Marcello Viti,Daniele Babbucci,Caterina Tamburelli
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發(fā)表于 2025-3-23 06:53:52 | 只看該作者
Enzo Mantovani,Marcello Viti,Daniele Babbucci,Caterina Tamburelli
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