دورية أكاديمية

Late Quaternary coastal uplift of southwestern Sicily, central Mediterranean sea

التفاصيل البيبلوغرافية
العنوان: Late Quaternary coastal uplift of southwestern Sicily, central Mediterranean sea
المؤلفون: Ferranti L., Burrato P., Sechi D., Andreucci S., Pepe F., Pascucci V.
المصدر: SCOPUS02773791-2021-255-SID85100442006
سنة النشر: 2021
المجموعة: Kazan Federal University Digital Repository
مصطلحات موضوعية: Aeolian ridges, Fold growth, Frontal thrust belt, Luminescence dating, Marine terraces, Mediterranean sea, Pleistocene, Southwestern sicily
الوصف: Mapping and luminescence aging of raised marine terraces and aeolian ridges along an ∼90 km coastal stretch in southwestern Sicily provide the first quantitative assessment of vertical tectonic deformation in this region, which spans the frontal part of an active thrust belt. We recognized a staircase of eleven terraces and nine related aeolian ridges. The elevation profile of terraces parallel to the coast shows a >90 km long bell-shaped pattern, onto which shorter-wavelength (∼10 km long) undulations are superimposed. Luminescence ages from terraced beach deposits and aeolian sediments constrain the position of paleoshorelines formed during MIS 5e, 7a and 7c, with a maximum uplift rate of ∼0.75 mm/a, and indicate a late Middle-Late Pleistocene (80–400 ka) age for the sequence of terraces. The elevation of Lower Pleistocene morpho-depositional markers points that uplift may have occurred at similar rates at the beginning of the Early Pleistocene, but almost zeroed between ∼1.5 and 0.4 Ma before the recent renewal. The uneven elevation of Middle-Upper Pleistocene paleoshorelines observed moving along the coast documents that uplift embeds both a regional and a local component. The regional, symmetric bell-shaped uplift is related to involvement in the thrust belt of thicker crustal portions of the northern African continental margin. The short-wavelength undulations represent the local component and correspond to actively growing bedrock folds. The present study contributes to unravel the different spatial and temporal scales of deformation processes at a collisional margin.
نوع الوثيقة: article in journal/newspaper
اللغة: unknown
تدمد: 0277-3791
العلاقة: Quaternary Science Reviews; 255; http://dspace.kpfu.ru/xmlui/bitstream/net/169006/-1/SCOPUS02773791-2021-255-SID85100442006-p1.pdfTest; https://dspace.kpfu.ru/xmlui/handle/net/169006Test
الإتاحة: https://dspace.kpfu.ru/xmlui/handle/net/169006Test
رقم الانضمام: edsbas.288A75B7
قاعدة البيانات: BASE