Mantle exhumation and sequence of magmatic events in the Magnaghi-Vavilov Basin (Central Tyrrhenian, Italy): New constraints from geological and geophysical observations
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- 作者：M. Prada<sup>asup><sup> ; sup><sup>1sup> ; C.R. Ranero<sup>bsup><sup> ; sup><sup>cranero@icm.csic.es" class="auth_mail" title="E-mail the corresponding authorsup> ; V. Sallarè ; s<sup>asup> ; N. Zitellini<sup>csup> ; I. Grevemeyer<sup>dsup>
- 关键词：Back-arc basin formation ; Serpentinisation ; Mantle exhumation ; MOR-type magmatism ; Tyrrhenian Basin
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：15 October 2016
- 年：2016
- 卷：689
- 期：Complete
- 页码：133-142
- 全文大小：3806 K
文摘
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A serpentinised peridotite basement is strongly supported by S-waves analysis
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Depth dependent serpentinisation resembles to that observed at magma-poor margins.
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Mantle exhumation was preceded by MOR-type magmatism and later intraplate volcanism.