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EnglishThis paper presents the results of a geological mapping project across the eastern Simbruini Mts. and the higher Roveto Valley (Central Apennines). The study area belongs to the Latium-Abruzzi Domain, which is characterized by a Cretaceous and Miocene carbonate platform succession followed by a thick upper Miocene terrigenous succession. A unique feature of the study area is the existence of a thick clastic unit, the brecce della Renga fm.'; this unit was produced by the dismantling of the margins of a large pre-orogenic extensional structural high, which rose within the foredeep basin starting in the early Tortonian. Following the Messinian-Pliocene Apennine chain building phase, the area was subjected to post-orogenic Quaternary extension, related to the opening of the Tyrrhenian sea. A geological map on the 1:20,000 scale illustrates the main stratigraphic and structural features of the area.
Geology of the eastern slopes of the Simbruini Mts. between Verrecchie and Capistrello (Central Apennines – Abruzzo, Italy) / Fabbi, Simone. - In: JOURNAL OF MAPS. - ISSN 1744-5647. - 14:2(2018), pp. 435-446. [10.1080/17445647.2018.1483843]
| Titolo: | Geology of the eastern slopes of the Simbruini Mts. between Verrecchie and Capistrello (Central Apennines – Abruzzo, Italy) | |
| Autori: | ||
| Data di pubblicazione: | 2018 | |
| Rivista: | ||
| Citazione: | Geology of the eastern slopes of the Simbruini Mts. between Verrecchie and Capistrello (Central Apennines – Abruzzo, Italy) / Fabbi, Simone. - In: JOURNAL OF MAPS. - ISSN 1744-5647. - 14:2(2018), pp. 435-446. [10.1080/17445647.2018.1483843] | |
| Handle: | http://hdl.handle.net/11573/1172786 | |
| Appartiene alla tipologia: | 01a Articolo in rivista |
File allegati a questo prodotto
| File | Note | Tipologia | Licenza | |
|---|---|---|---|---|
| Fabbi_Geology_2018.pdf | Versione editoriale (versione pubblicata con il layout dell'editore) |  | Open Access Visualizza/Apri |
http://hdl.handle.net/11573/1172786
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