The pyroclastic breccias from Cabezo Negro de Tallante (SE Spain). Is there any relation with carbonatitic magmatism?

Autor: Innocenzi F.[1], Ronca S.[1], Agostini S.[2], Brandano M.[1], Caracausi A.[3], Lustrino M.[1

Publikováno v: Lithos (Oslo. Print) 392-393 (2021): 1–21. doi:10.1016/j.lithos.2021.106140
info:cnr-pdr/source/autori:Innocenzi F.[1], Ronca S.[1], Agostini S.[2], Brandano M.[1], Caracausi A.[3], Lustrino M.[1,4]/titolo:The pyroclastic breccias from Cabezo Negro de Tallante (SE Spain): Is there any relation with carbonatitic magmatism?/doi:10.1016%2Fj.lithos.2021.106140/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:21/intervallo_pagine:1–21/volume:392-393

The small Plio-Quaternary volcanic centre of Cabezo Negro de Tallante in SE Spain includes a thick deposit of polymictic pyroclastic tuff-breccia, whose fragments are agglutinated by a carbonate-rich component. This feature is also observed in other

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eebf3a35a6a335e9fe87c6b005ac6afd
http://hdl.handle.net/11573/1541979