Luminescence dating of Late Pleistocene faults as evidence of uplift and active tectonics in Sardinia, W Mediterranean

dc.contributor.author	Casini L.
dc.contributor.author	Andreucci S.
dc.contributor.author	Sechi D.
dc.contributor.author	Huang C.Y.
dc.contributor.author	Shen C.C.
dc.contributor.author	Pascucci V.
dc.date.accessioned	2021-02-25T20:35:50Z
dc.date.available	2021-02-25T20:35:50Z
dc.date.issued	2020
dc.identifier.issn	0954-4879
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/161936
dc.description.abstract	© 2020 John Wiley & Sons Ltd Precise dating of the activity of Late Pleistocene to Holocene neo-tectonic structures is crucial to quantify the rate of deformation in low-seismicity regions. Sardinia is a relatively stable continental fragment set in the middle of the tectonically active Western Mediterranean belt. This paper provides evidences of significant uplift of northwest Sardinia that support an ongoing tectonic activity since the Marine Isotopic Stage 7 (MIS 7; ca. 220 ka). In particular, it documents for the first time Late Pleistocene to Holocene tectonics based on luminescence dating of travertine sealing a major NNE-SSW fault.
dc.relation.ispartofseries	Terra Nova
dc.title	Luminescence dating of Late Pleistocene faults as evidence of uplift and active tectonics in Sardinia, W Mediterranean
dc.type	Article
dc.relation.ispartofseries-issue	4
dc.relation.ispartofseries-volume	32
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	261
dc.source.id	SCOPUS09544879-2020-32-4-SID85081681257

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Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.