Kazan Federal University Digital Repository

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

Show simple item record

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


Files in this item

This item appears in the following Collection(s)

  • Публикации сотрудников КФУ Scopus [22633]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

Show simple item record

Search DSpace


Advanced Search

Browse

My Account