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  • 1
    Keywords: Aufsatzsammlung ; Meeresspiegelschwankung ; Quartär
    Type of Medium: Book
    Pages: 257 S. , Ill., graph. Darst., Kt.
    Series Statement: Quaternary international 232
    Language: English
    Note: Literaturangaben
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  • 2
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    PANGAEA
    In:  Supplement to: Antonioli, Fabrizio; Lo Presti, Valeria; Rovere, Alessio; Ferranti, Luigi; Anzidei, Marco; Furlani, Stefano; Mastronuzzi, Giuseppe; Orru, Paolo E; Scicchitano, Giovanni; Sannino, Gianmaria; Spampinato, Cecilia R; Pagliarulo, Rossella; Deiana, Giacomo; de Sabata, Eleonora; Sansò, Paolo; Vacchi, Matteo; Vecchio, Antonio (2015): Tidal notches in Mediterranean Sea: a comprehensive analysis. Quaternary Science Reviews, 119, 66-84, https://doi.org/10.1016/j.quascirev.2015.03.016
    Publication Date: 2023-01-21
    Description: Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology. Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development. Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2023-01-21
    Keywords: Erosion rate; Lithology/composition/facies; Location; Reference/source
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
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  • 4
    Publication Date: 2023-04-13
    Keywords: Badisco; Badisco_notch_64; Badisco_notch_65; Badisco_notch_66; Balzi_Rossi_Ventimiglia_notch_3; Balzi Rossi Ventimiglia; Biddiriscottai; Biddiriscottai_notch_8; Bottom depth of biological rim; Buggerru; Buggerru_notch_21; Buggerru_notch_22; Cala_Domestica_notch_19; Cala_Domestica_notch_20; Cala_Fuili_notch_9; Cala_Mosca_notch_11; Cala_Mosca_notch_12; Cala Domestica; Cala Fuili; Cala Mosca; Calamosche; Calamosche_notch_48; Capo_Caccia_notch_5; Capo Caccia; Capri; Capri_notch_27; Cefalu; Cefalu_notch_40; Cefalu_notch_41; Ciolo; Ciolo_notch_62; Circeo; Circeo_notch_25; Colonia_de_Sant_Jordie_Palma_notch_1; Colonia de Sant Jordie Palma; Comino; Comino_notch_51; Comment; Depth of cliff toe; Direction; Dubrovnik; Dubrovnik_notch_71; ELEVATION; Event label; Favignana_Cala_rossa_notch_30; Favignana Cala rossa; Gaeta; Gaeta_notch_26; Gavathas; Gavathas_notch_73; Giovinazzo; Giovinazzo_notch_69; Gozo; Gozo_eroded_mushroom_notch_50; Gozo_notch_49; Gozo eroded mushroom; Lampedusa; Lampedusa_Cala_Calandra_notch_53; Lampedusa_notch_54; Lampedusa_notch_55; Lampedusa Cala Calandra; Latitude of event; Levanzo; Levanzo_harbour_notch_32; Levanzo_notch_31; Levanzo harbour; Lithology/composition/facies; Location; Longitude of event; Macari; Macari_notch_34; Malta; Malta_notch_52; Marettimo_Castello_notch_29; Marettimo_harbour_notch_28; Marettimo Castello; Marettimo harbour; Marina_di_Pulsano_notch_56; Marina di Pulsano; Marseille_Fausse_Monnaie_notch_2; Marseille Fausse Monnaie; Marzamemi; Marzamemi_notch_47; Masua; Masua_notch_13; Masua_notch_14; Masua_notch_15; Mongerbino; Mongerbino_notch_39; Montenegro; Montenegro_notch_72; MULT; Multiple investigations; Noli_Malpasso_notch_4; Noli Malpasso; Notch depth; Notch width; Palermo_harbour_notch_38; Palermo_Mondello_notch_37; Palermo harbour; Palermo Mondello; Pan_di_zucchero_notch_16; Pan_di_zucchero_notch_17; Pan_di_zucchero_notch_18; Pan di zucchero; Polignano_Modugno_notch_67; Polignano_San_Vito_notch_68; Polignano Modugno; Polignano San Vito; Porto_Conte_notch_6; Porto_Conte_notch_7; Porto Conte; Range; San_Vito_Castelluzzo_notch_33; Santa_Maria_di_Leuca_notch_60; Santa_Maria_di_Leuca_notch_61; Santa Maria di Leuca; San Vito Castelluzzo; Scopello; Scopello_notch_36; Sella_del_Diavolo_notch_10; Sella del Diavolo; Serra_Cicora_notch_58; Serra_Cicora_notch_59; Serra Cicora; Siracusa; Siracusa_notch_42; Siracusa_notch_43; Siracusa_notch_44; Siracusa_notch_45; Siracusa_notch_46; Site; Species; Talamone; Talamone_notch_24; Tharros; Tharros_notch_23; Thickness; Torre_Colimena_notch_57; Torre Colimena; Tremiti; Tremiti_notch_70; Type; Uncertainty; Variation bottom depth of biological rim; Variation of notch width; Waves energy, flux; Width; Zingaro; Zingaro_notch_35; Zinzulusa; Zinzulusa_notch_63
    Type: Dataset
    Format: text/tab-separated-values, 1569 data points
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  • 5
    Publication Date: 2024-03-02
    Description: AMS 14C ages of the speleothem samples from Cola cave. The "dead carbon portion" DCP-corrected 14C ages were calculated based on two different values of dead carbon incorporated in the speleothem (5%, and 10%). The 14C ages were converted to calendar year (calibrated age) using the IntCal13 calibration curve (Reimer et al., 2013). The mean preferred calibrated age is the average of the median probability calculated from the two DCP values. The 1sigma range for the preferred calibrated age represents the largest age interval.
    Keywords: 14C; Age, 14C AMS; Age, 14C calibrated, IntCal13 (Reimer et al., 2013); Age, dated; Age, error; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; COLA; dating; Dead carbon portion (DCP)-corrected; Italy; Laboratory code/label; Sample code/label; Speleothem sample; Spleothems; SPS
    Type: Dataset
    Format: text/tab-separated-values, 68 data points
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  • 6
    Publication Date: 2024-03-02
    Description: Uranium-series measurements of the speleothem samples from the Cola cave. The concentrations of 238U and 232Th were determined using the enriched 236U and 229Th isotopes, respectively. delta234Um = {[(234U/238U)sample/(234U/238U)eq] − 1} ×1000, where (234U/238U)sample is the measured atomic ratio and (234U/238U)eq is the atomic ratio at secular equilibrium.
    Keywords: Age, dated; Age, error; Age, Uranium-Thorium; COLA; dating; Italy; Laboratory code/label; Multi-collector ICP-MS (MC-ICP-MS), Neptune Plus, Thermo; Sample code/label; Speleothem sample; Spleothems; SPS; Thorium-230/Thorium-232 activity ratio; Thorium-230/Thorium-232 activity ratio, error; Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 activity ratio, error; Thorium-232; Thorium-232, error; U/Th; Uranium-238; Uranium-238, error; δ234 Uranium
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 7
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Foreland contraction and hinterland extension in the Southern Apennines orogen of Italy produced a complex spatial and temporal pattern of vertical and horizontal displacement. Remarkably, Late Miocene to mid-Pleistocene foreland migration of the contractional front at ∼16 mm yr−1 was not accompanied by uplift and the frontal thrust belt remained at or below sea level. Only following a mid-Pleistocene reduction in horizontal displacement did the frontal thrust belt and foreland begin uplift at ∼0.5 mm yr−1, a rate that increased to ∼1 mm yr−1 after 125 ka. Although the extensional hinterland experienced net subsidence during formation of the Tyrrhenian basin, an extensional transition zone adjacent to the frontal thrust belt records sustained uplift at ∼0.3 mm yr−1. The interaction of preexisting crustal structure and deep tectonic processes resulted in time-integrated displacement rates suggesting steady-state deformation for periods of 106 years. Displacement rate changes were abrupt and occurred over intervals of 105 years or less.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2021-01-22
    Description: Integration of archaeoseismic observations, geological and geophysical surveys and a critical review of historical written sources contributed to shed light on the effects of the 847 earthquake AD that struck a large area of Southern-Central Italy. New archaeoseismic evidence of a strong earthquake comes from two Medieval archaeological sites along the Volturno Valley, between Campania and Molise regions, which occurred around the middle of the ninth century AD. Evidence includes the tilting of pillars in the Basilica of Santa Maria near Alvignano (northern Campania) and a collapsed masonry wall in the Abbey of San Vincenzo al Volturno near Isernia (northern Molise). At Alvignano, a site so far unrecorded in seismic catalogues for the 847 earthquake, geoelectrical and georadar investigations were used to explore the subsoil and study local site conditions, which could have influenced coseismic ground motion. Integrated interpretation of geophysical surveys and borehole logs document the presence of altered pyroclastic deposits, which certainly enhanced site effects at Alvignano. Analysis of damage descriptions and of archaeological reports indicate that the 847 seismic event documented by historical sources damaged a wide area between Latium, Campania and Molise, with destruction of the town of Isernia. Although historical sources did not explicitly mention damage in Rome, seismic effects attributed to the 847 event are recorded in the archaeological and seismological literature. Because the damaged area for this medieval earthquake is loosely defined due to the scanty documentation, the present study represents an important contribution to better define the shaking area and provide new hints on the extent and location of the possible seismogenic source.
    Description: Published
    Description: 228301
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2021-05-12
    Description: 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.
    Description: Published
    Description: 106812
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: Marine terraces ; Aeolian ridges ; Luminescence dating ; Pleistocene ; Frontal thrust belt ; Fold growth ; Southwestern Sicily ; Mediterranean sea ; 04.04. Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2021-05-12
    Description: Speleoseismological research carried out in the Central Apennines (Italy) contributed to understanding the behavior of active normal faults that are potentially able to generate Mw 6.5–7 earthquakes documented by paleoseismology and by historical and instrumental seismology. Radiometric (U‐Th, AMS‐14C, and bulk‐14C) dating of predeformation and postdeformation layers from collapsed speleothems found in Cola Cave indicates that at least three speleoseismic events occurred in the cave during the last ~12.5 ka and were ostensibly caused by seismic slip on one or more of the active faults located in the region surrounding the cave. We modeled the collapse of a tall (173 cm high) stalagmite to find a causative association of this event with one among the potential seismogenic sources. We defined the uniform hazard spectrum (UHS) for each seismogenic source at the site, and we used the calculated spectra in a deterministic approach to study the behavior of the speleothem, through a numerical finite element modeling (FEM). Although our analysis suggests the “Liri” fault as the most likely source responsible for the ground shaking recorded in the cave, the “Fucino” fault system, responsible for a Mw 7 earthquake in 1915, cannot be excluded as a potential source of speleoseismic damage. Results of this work provide new constraints on the seismotectonic history of this sector of Central Apennines and highlight the performance of integrated speleoseismological, seismic hazard, and numerical studies.
    Description: Published
    Description: e2020TC006289
    Description: 6T. Studi di pericolosità sismica e da maremoto
    Description: JCR Journal
    Keywords: Speleoseismology ; Central Apennines ; seismic hazard ; finite element modeling ; 04.04. Geology ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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