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  • 1
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    (Table T4) Core porosity, density, and velocity of ODP Site 178-1101 (2001)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 178-1101; COMPCORE; Composite Core; Density; DEPTH, sediment/rock; interpolated; Joides Resolution; Leg178; Ocean Drilling Program; ODP; Porosity; South Pacific Ocean; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 319 data points
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    DATA PANGAEA
  • 2
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    (Table T2) Core and downhole logs of porosity, density, and velocity of ODP Site 178-1095 (2001)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 178-1095; COMPCORE; Composite Core; Density; DEPTH, sediment/rock; interpolated; Joides Resolution; Leg178; Ocean Drilling Program; ODP; Porosity; South Pacific Ocean; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1293 data points
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    DATA PANGAEA
  • 3
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    (Table T3) Core and downhole logs of porosity, density, and velocity of ODP Site 178-1096 (2001)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 178-1096; COMPCORE; Composite Core; Density; DEPTH, sediment/rock; interpolated; Joides Resolution; Leg178; Ocean Drilling Program; ODP; Porosity; South Pacific Ocean; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1170 data points
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    DATA PANGAEA
  • 4
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    Opal content of the lowermost part of sediment core 178-1095B (2003)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 178-1095B; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg178; Ocean Drilling Program; ODP; Opal, auto analysis (Müller & Schneider, 1993); Opal, biogenic silica; Sample code/label; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
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    DATA PANGAEA
  • 5
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    Physical properties of ODP Leg 178 sites (2001)
    PANGAEA
    In:  Supplement to: Volpi, Valentina; Camerlenghi, Angelo; Moerz, Tobias; Corubolo, P; Rebesco, Michele; Tinivella, Umberta (2001): Data report: Physical properties relevant to seismic stratigraphic studies, continental rise Sites 1095, 1096, and 1101, ODP Leg 178, Antarctic Peninsula. In: Barker, PF; Camerlenghi, A; Acton, GD; Ramsay, ATS (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 178, 1-36, https://doi.org/10.2973/odp.proc.sr.178.228.2001
    Details
    Publication Date: 2024-01-09
    Description: We have reanalyzed the porosity, bulk density, and seismic velocity information collected from continental rise Sites 1095, 1096, and 1101 during the drilling of Ocean Drilling Program (ODP) Leg 178 (Fig. F1). The purpose is to provide a comprehensive composite digital set of data readily available for future studies aimed at well-seismic correlation. The work originates from the occurrence of overlapping sets of physical parameters and acoustic velocity collected by different methods (downhole logging, core logging, laboratory determination, and derivation from seismic data) and from different holes at the same site. These data do not always provide the same information because of difficulties encountered at each specific hole or methodological differences. In addition, a basic correlation between these parameters and onsite multichannel seismic (MCS) data is presented.
    Keywords: 178-1095; 178-1096; 178-1101; COMPCORE; Composite Core; Joides Resolution; Leg178; Ocean Drilling Program; ODP; South Pacific Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
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    DATA PANGAEA
  • 6
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    New evidence of active transtensional deformation in apulia foreland (n-ionian sea). (2019)
    Details
    Publication Date: 2019-12-05
    Description: The response of continental forelands to subduction and oblique collision is a widely investigated topic in geodynamics. The deformation occurring within a foreland shared by two opposite-verging chains, however, is not very common and poorly understood. The Apulia block, at the southern end of the Adria microplate, Central Mediterranean, represents one of these latter cases, being the common foreland of the Dinarides and Apennines orogens. In its southern part, the Apulian foreland has preserved the Mesozoic paleomargin at the transition with the old oceanic Ionian crust that conversely underwent subduction under the Calabrian and Hellenic arcs. For these reasons, Apulia represents an interesting and rare case of study where double orogens and subduction have interacted with the foreland block. As described by various authors, the almost symmetrical bending of the Apulia foreland due the opposite load of the adjacent chains, produced a system of NW-SE trending normal faults. The precise age and the role of these faults have not been yet determined due to the lack of available information. In this contribution we investigated the internal deformation of the Apulia foreland using geophysical data at various resolutions and scales over a wide area. We used multichannel seismic profiles, part of which are provided in the collaborative framework between Spectrum Geo and INGV, recorded up to 12 s and provide a consistent imaging of the upper crustal setting of the Apulia foreland. High-resolution multichannel seismic profiles, multibeam high-resolution bathymetry and CHIRP profiles recently acquired by R/V OGS Explora provide constraints on the recent activity of the major fault systems identified. The analysis of this multiscale dataset highlights the presence and the role of a major NW-SE oriented active fault system which obliquely cuts the Apulia foreland. The presence of this fault system has already been hypothesized based on sparse seismic profiles, but its lateral continuity has never been documented. From the seismic viewpoint, this structure lies in a relatively silent area. Nonetheless, it hosts the 1743 Southern Apulia Mw 6.8 earthquake which widely damaged the Salento (S-Italy) and Ionian Islands (Greece) regions and whose source is still a matter of debate. This new geophysical dataset allowed us to reconstruct the 3D geometry of this fault system, whose architecture suggests a transtensive kinematics, and to analyse the syn-tectonic basins associated with the major faults which recorded the Late Quaternary to Holocene deformation. This work is being developed in the frame of the project “FASTMIT”, funded by the Italian Ministry of University and Research.
    Description: Unpublished
    Description: La Valletta, Malta
    Description: 2TR. Ricostruzione e modellazione della struttura crostale
    Keywords: Active Tectonics ; Marine Geology ; 04.04. Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 7
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    Active Extension in a Foreland Trapped Between Two Contractional Chains: The South Apulia Fault System (SAFS) (2020)
    Wiley
    Details
    Publication Date: 2020-07-08
    Description: The response of continental forelands to subduction and collision is a widely investigated topic in geodynamics. The deformation occurring within a foreland shared by two opposite‐verging chains, however, is uncommon and poorly understood. The Apulia Swell in the southern end of the Adria microplate (Africa‐Europe plate boundary, central Mediterranean Sea) represents one of these cases, as it is the common foreland of the SW verging Albanides‐Hellenides and the NE verging Southern Apennines merging into the SSE verging Calabrian Arc. We investigated the internal deformation of the Apulia Swell using multiscale geophysical data: multichannel seismic profiles recording up to 12‐s two‐way time (TWT) for a consistent image of the upper crust; high‐resolution multichannel seismic profiles, high‐resolution multibeam bathymetry, and CHIRP profiles acquired by R/V OGS Explora to constrain the Quaternary geological record. The results of our analyses characterize the geometry of the South Apulia Fault System (SAFS), a 100‐km‐long and 12‐km‐wide structure attesting an extensional (and possibly transtensional) response of the foreland to the two contractional fronts. The SAFS consists of two NW‐SE right‐stepping master faults and several secondary structures. The SAFS activity spans from the Early Pleistocene through the Holocene, as testified by the bathymetric and high‐resolution seismic data, with long‐term slip rates in the range of 0.2–0.4 mm/yr. Considering the position within an area with few or none other active faults in the surroundings, the dimension, and the activity rates, the SAFS can be a candidate causative fault of the 20 February 1743, M 6.7, earthquake.
    Description: Italian Ministry for Education, University, and Research (MIUR), Premiale 2014 D. M. 291 03/05/2016.
    Description: Published
    Description: e2020TC006116
    Description: 2T. Deformazione crostale attiva
    Description: 2TR. Ricostruzione e modellazione della struttura crostale
    Description: JCR Journal
    Keywords: active tectonics ; apulia ; south apulia fault system ; 1743 earthquake ; marine geology ; stable continental region ; ionian sea ; active faults ; subsurface geology ; seismic interpretation ; 04.04. Geology ; 04.07. Tectonophysics ; 04.02. Exploration geophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
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    Piccolipiu, a multicenter birth cohort in Italy: protocol of the study (2014)
    Sara Farchi; Francesco Forastiere; Liza Vecchi Brumatti; Sabrina Alviti; Antonio Arnofi; Tommaso Bernardini; Maura Bin; Sonia Brescianini; Valentina Colelli; Rodolfo Cotichini; Martina Culasso; Paolo De Bartolo; Laura Felice; Valentina Fiano; Alessandra Fioritto; Alfio Frizzi; Luigi Gagliardi; Giulia Giorgi; Chiara Grasso; Francesca La Rosa; Claudia Loganes; Paola Lorusso; Valentina Martini; Franco Merletti; Emanuela Medda; Veronica Montelatici; Isabella Mugelli; Silvia Narduzzi; Lorenza NisticòLuana Penna; Elisa Piscianz; Carlo Piscicelli; Giulia Poggesi; Daniela Porta; Antonella Ranieli; Gherardo Rapisardi; Assunta Rasulo; Lorenzo Richiardi; Franca Rusconi; Laura Serino; Maria Antonietta Stazi; Virgilia Toccaceli; Tullia Todros; Veronica Tognin; Morena Trevisan; Erica Valencic; Patrizia Volpi; Valentina Ziroli; Luca Ronfani; Domenico Di Lallo
    BioMed Central
    Details
    Publication Date: 2014-02-08
    Description: Background: The fetal and infant life are periods of rapid development, characterized by high susceptibility to exposures. Birth cohorts provide unique opportunities to study early-life exposures in association with child development and health, as well as, with longer follow-up, the early life origin of adult diseases. Piccolipiu is an Italian birth cohort recently set up to investigate the effects of environmental exposures, parental conditions and social factors acting during pre-natal and early post-natal life on infant and child health and development. We describe here its main characteristics. Methods: Piccolipiu is a prospective cohort of expected 3000 newborns, who will be recruiting in six maternity units of five Italian cities (Florence, Rome, Trieste, Turin and Viareggio) since October 2011. Mothers are contacted during pregnancy or at delivery and are offered to participate in the study. Upon acceptance, their newborns are recruited at birth and followed up until at least 18 years of age. At recruitment, the mothers donate a blood sample and complete a baseline questionnaire. Umbilical cord blood, pieces of umbilical cord and heel blood spots are also collected. Postnatal follow-up currently occurs at 6, 12, and 24 months of age using on-line or postal self administered questionnaire; further questionnaires and medical examinations are envisaged. Questionnaires collect information on several factors, including mother's and/or child's environmental exposures, anthropometric measures, reproductive factors, diet, supplements, medical history, cognitive development, mental health and socioeconomic factors. Health promotion materials are also offered to parents.DiscussionPiccolipiu will broaden our understanding of the contribution of early-life factors to infant and child health and development. Several hypotheses on the developmental origins of health can be tested or piloted using the data collected from the Piccolipiu cohort. By pooling these data with those collected by other existing birth cohorts it will be possible to validate previous findings and to study rare exposures and outcomes.
    Electronic ISSN: 1471-2431
    Topics: Medicine
    Published by BioMed Central
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