A Geophysical-Geochemical Approach to the Study of the Paleogene Julian—Slovenian Basin 'Megabeds' (Southern Alps—Northwestern Dinarides, Italy/Slovenia)

التفاصيل البيبلوغرافية
العنوان: A Geophysical-Geochemical Approach to the Study of the Paleogene Julian—Slovenian Basin 'Megabeds' (Southern Alps—Northwestern Dinarides, Italy/Slovenia)
المؤلفون: Ž. Pogačnik, Gian Andrea Pini, Giorgio Tunis, Andrea Festa, Kim Senger, Kei Ogata
المساهمون: Ogata, K., Pogacnik, Z., Tunis, G., Pini, G. A., Festa, A., Senger, K., Geology and Geochemistry
المصدر: Geosciences
Volume 9
Issue 4
Geosciences, Vol 9, Iss 4, p 155 (2019)
Geosciences (Switzerland), 9(4):155, 1-17. MDPI
Ogata, K, Pogačnik, Ž, Tunis, G, Pini, G A, Festa, A & Senger, K 2019, ' A geophysical-geochemical approach to the study of the paleogene julian-slovenian basin “megabeds” (Southern alps-northwestern dinarides, Italy/Slovenia) ', Geosciences (Switzerland), vol. 9, no. 4, 155, pp. 1-17 . https://doi.org/10.3390/geosciences9040155
سنة النشر: 2019
مصطلحات موضوعية: 010504 meteorology & atmospheric sciences, Carbonate platform, Carbonate Mass Transport Deposits, Megabreccias, Geoelectric Profiling, Geochemical Fingerprinting, Mass-Transport Deposits, Outer Dinarides, Seismic-Reflection, Sedimentation, Architecture, Turbidite, Mudstones, Chemistry, Slovenia, carbonate mass transport deposits, megabreccias, geoelectric profiling, geochemical fingerprinting, Mudstone, Geochemistry, Fluorescence spectrometry, 010502 geochemistry & geophysics, 01 natural sciences, Soft-sediment deformation structures, Sedimentary depositional environment, geochemical fingerprinting, Carbonate mass transport deposit, Marl, SDG 14 - Life Below Water, Outer Dinaride, megabreccias, 0105 earth and related environmental sciences, lcsh:QE1-996.5, carbonate mass transport deposits, Megabreccia, lcsh:Geology, Carbonate Mass Transport Deposit, Clastic rock, Mass-Transport Deposit, Carbonate mass transport deposits, General Earth and Planetary Sciences, Sedimentary rock, geoelectric profiling, Paleogene
الوصف: The Paleogene &ldquo
megabeds&rdquo
of the Julian-Slovenian Basin are regional, basin-wide deposits, produced by catastrophic carbonate platform collapses. They record the emplacement of a bipartite slide mass behaving as a cohesive blocky/debris flow in the lower part, and as a grain to turbulent flow in the upper part. Several types of primary (sedimentary) soft sediment deformation structures testify fluid overpressure conditions during emplacement. Such structures are identified within a brecciated, fine grained matrix that encloses and intrudes slide blocks and clasts, characterized by NE-, NW- and SW-directed paleo-transport directions, indicating a depositional setting close to the basin margins. Here we present an updated review of some representative megabeds, exposed in the open-pit quarry outcrops of Anhovo (SW Slovenia). In particular, we here discuss new interpretations based on X-ray fluorescence spectrometry (XRF), thermo-gravimetry (TG) and electric resistivity tomography (ERT). Our results indicate that basal marly clasts of the megabeds are markedly different from the uppermost draping marls, suggesting two different coeval sources. The relationships with the underlying successions are strongly erosive, with deep localized scouring of the substrate and amalgamations between different megabeds, and the depositional units inside individual megabeds, supporting the geochemical differences.
وصف الملف: ELETTRONICO; application/pdf
اللغة: English
تدمد: 2076-3263
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1500b4670bf7104bd347ebe076f9c697
http://hdl.handle.net/2318/1696355
حقوق: OPEN
رقم الأكسشن: edsair.doi.dedup.....1500b4670bf7104bd347ebe076f9c697
قاعدة البيانات: OpenAIRE