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  • 1
    Publication Date: 2023-06-27
    Description: Multiple peaks in sulfate concentration in ice cores have been identified as potential candidates for the ~74 ka Toba supereruption. The sulfur isotopic composition of sulfate preserved in two EPICA Antarctic ice cores, EDML and EDC, for 11 of the candidates has been analysed at high temporal resolution for mass-independent fractionation (MIF) using multi-collector inductively coupled plasma mass spectrometry. S-MIF signals preserved in volcanic sulfate are indicative of stratospheric eruptions due to sulfur aerosols being exposed to ultraviolet radiation when erupted into and above the ozone layer and subsequently undergoing photochemical reactions. Sulfur aerosols in the stratosphere will have longer residence times than those in the troposphere and will scatter incoming solar radiation. This data set includes the eruption, sample type, depths, ages (using the AICC2012 age model), sulfate concentration (determined by ion chromatography) and isotopic composition data (δ34S, δ33S, Δ33S) and their associated errors.
    Keywords: AGE; Antarctica; Calculated, in volcanic fraction; DEPTH, ice/snow; Dome C; Dome C, Antarctica; EDC; EDML; EDRILL; EPICA; EPICA-Campaigns; EPICA Dome C; EPICA drill; EPICA Dronning Maud Land, DML28C01_00; Eruption; European Project for Ice Coring in Antarctica; Event label; Ice core; ICEDRILL; Ice drill; Ion chromatography; Kohnen Station; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS); sulfate; Sulfate; Sulfur isotopes; Type; volcanic; Volcanic fraction; Volcanic fraction, standard deviation; Δ33S; Δ33S, standard deviation; δ33S; δ33S, standard deviation; δ34S; δ34S, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 1440 data points
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  • 2
    Publication Date: 2024-01-09
    Keywords: Date/Time of event; Deep Sea Drilling Project; Depth, bottom/max; Depth, top/min; DSDP; Event label; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Japan Trench; KR02-15-PC02; KR02-15-PC03; KR02-15-PC07; KR07-06-PC11-03; KR08-10-PC01; KR08-10-PC02; KR08-10-PC06; KR09-16-PC01; KR10-12-PC01; KR10-12-PC02; KR10-12-PC03; Latitude of event; Layer description; Longitude of event; MR00-K03-PC01; MR00-K03-PC02; MR00-K03-PC04; MR00-K05-PC02; MR06-02-PC04; MR97-04-PC01; MR97-04-PC02; MR98-05-PC01; MR99-K04-PC01; MR99-K04-PC02; NT04-01-PCODSR04E-B; Ocean Drilling Program; ODP; PC; Piston corer; Sample code/label; Sea of Okhotsk; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1206 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 127-794A; 127-794B; 127-795A; 127-795B; 186-1150A; 186-1150B; 190-1173A; 31-296; 322-C0011B; 322-C0012A; 56-434; 56-434A; 56-434B; 56-435; 56-435A; 56-436; 57-438A; 87-584; Chikyu; Comment; Date/Time of event; Deep Sea Drilling Project; Depth, bottom/max; Depth, top/min; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Exp322; Glomar Challenger; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Japan Sea; Joides Resolution; Latitude of event; Layer description; Leg127; Leg186; Leg190; Leg31; Leg56; Leg57; Leg87; Longitude of event; NanTroSEIZE Stage 2: Subduction Input; North Pacific; North Pacific/BASIN; North Pacific/Philippine Sea/RIDGE; North Pacific/RIDGE; North Pacific/TRENCH; North Pacific Ocean; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; Sample comment; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 10170 data points
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  • 4
    Publication Date: 2024-04-20
    Description: The VOLCORE (Volcanic Core Records) database is a collection of 34,696 visible tephra (volcanic ash and associated products) occurrences reported in the initial reports volumes of all of the Deep Sea Drilling Project (DSDP; 1966-1983), the Ocean Drilling Program (ODP; 1983-2003), the Integrated Ocean Drilling Program (IODP; 2003-2013) and the International Ocean Discovery Program (IODP; 2013-present) up to and including IODP Expedition 381. The combined international drilling programmes (OD) have locations with global coverage. Cored tephra layers and tephra-bearing sediments span timescales from recent to ~150 million years in age. This database is a collection of information about reported visible tephra layers entirely or predominantly composed of volcanic ash. Data include the depth below sea floor, tephra thickness, location, and any reported comments. An approximate age was estimated for most (29,493) of the tephra layers using available age-depth models. The database can be applied to tephrochronology, volcanology, geochemistry, studies of sediment transport and palaeoclimatology.
    Keywords: ash; Deep Sea Drilling Project; DSDP; Geochemistry; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Ocean Drilling Program; ODP; paleoclimatology; sediment; Tephra; tephrochronology; volcanic; Volcanology; VOLCORE
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 11.8 MBytes
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  • 5
    Publication Date: 2024-04-20
    Description: VOLCORE_2021 is an update on the original VOLCORE data released in 2020. Change notes are listed within the VOLCORE_2021 data file. A major update is the new merged Layers-Holes-AgeDepth sheet, enabling easier manipulation of the data. The VOLCORE (Volcanic Core Records) database is a collection of 34,696 visible tephra (volcanic ash and associated products) occurrences reported in the initial reports volumes of all of the Deep Sea Drilling Project (DSDP; 1966-1983), the Ocean Drilling Program (ODP; 1983-2003), the Integrated Ocean Drilling Program (IODP; 2003-2013) and the International Ocean Discovery Program (IODP; 2013-present) up to and including IODP Expedition 381. The combined international drilling programmes (OD) have locations with global coverage. Cored tephra layers and tephra-bearing sediments span timescales from recent to ~150 million years in age. This database is a collection of information about reported visible tephra layers entirely or predominantly composed of volcanic ash. Data include the depth below sea floor, tephra thickness, location, and any reported comments. An approximate age was estimated for most (29,493) of the tephra layers using available age-depth models. The database can be applied to tephrochronology, volcanology, geochemistry, studies of sediment transport and palaeoclimatology.
    Keywords: ash; Deep Sea Drilling Project; DSDP; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Ocean Drilling Program; ODP; paleoclimatology; sediment; Tephra; tephrochronology; volcanic; Volcanology; VOLCORE
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 20.6 MBytes
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  • 6
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    PANGAEA
    In:  Supplement to: Mahony, Sue H; Sparks, R Stephen J; Barnard, Nick H (2014): Quantifying uncertainties in marine volcanic ash layer records from ocean drilling cores. Marine Geology, 357, 218-224, https://doi.org/10.1016/j.margeo.2014.08.010
    Publication Date: 2024-04-11
    Description: Ocean drilling provides a global record of deposits throughout the oceans. An international collaborative ocean research programme was established in 1966, and the International Ocean Discovery Program (IODP) is the most recent manifestation of this. During each expedition a large amount of data are generated and collected by the shipboard science team. It could be suggested that due to the different staff and objectives during each expedition there would be significant variations in the consistency of data recorded in the shipboard visual core descriptions (VCDs). Use of shipboard VCD data in a global study of volcanism through time required the ground truthing of VCD data, to assess the consistency of ash layer reporting and to identify the amount of under/over recording of volcanic ash layers in cores. Approximately 1400 ash layers in DSDP, ODP, IODP and JAMSTEC cores were examined and it was found that on average 70-75% of recorded volcanic ash layers were present as described, an average of 17-20% were over recorded and 10-15% were under recorded. A number of factors could contribute to this variability, such as VCD format, lack of time for shipboard sampling of every ash layer, significant ash layer colour changes since time of coring, or differences in VCD recording and volcanic ash layer identification and description schemes between expeditions. These findings are important and will allow greater confidence in further studies based on data compiled from shipboard VCDs.
    Keywords: Deep Sea Drilling Project; DSDP; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 7
    Publication Date: 2024-04-11
    Keywords: 121-758A; 128-799A; 130-803D; 130-807A; 134-828A; 136-842B; 138-845A; 138-845B; 145-887A; 165-998A; 165-998B; 167-1010B; 181-1122C; 181-1123A; 181-1123B; 181-1124A; 181-1124B; 18-178; 18-182; 184-1148A; 185-1149A; 186-1150A; 190-1173A; 202-1236A; 31-292; 31-296; 329-U1371D; 333-C0018A; 334-U1381A; 5-33; 5-34; 5-36; 86-578; Chikyu; Colombia Basin, Caribbean Sea; Coral Sea; Costa Rica Seismogenesis Project (CRISP); Date/Time of event; Deep Sea Drilling Project; Depth, bottom/max; Depth, top/min; Depth comment; DRILL; Drilling/drill rig; DSDP; Event label; Exp329; Exp333; Exp334; Glomar Challenger; Indian Ocean; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Japan Sea; Joides Resolution; Latitude of event; Layer description; Leg121; Leg128; Leg130; Leg134; Leg136; Leg138; Leg145; Leg165; Leg167; Leg18; Leg181; Leg184; Leg185; Leg186; Leg190; Leg202; Leg31; Leg5; Leg86; Longitude of event; NanTroSEIZE Stage 2: Subduction Inputs 2 and Heat Flow; North Pacific; North Pacific/HILL; North Pacific/Philippine Sea/CONT RISE; North Pacific/Philippine Sea/RIDGE; North Pacific/PLAIN; North Pacific/RIDGE; North Pacific/SLOPE; North Pacific Ocean; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; South China Sea; South Pacific Gyre Microbiology; South Pacific Ocean; Visual description; West equatorial Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 2217 data points
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  • 8
    Publication Date: 2023-12-27
    Description: The Aso-4 explosive eruption on Kyushu, Japan, 89,500 years ago was one of the biggest eruptions in the last one hundred millennia, with a magnitude of approximately M8. Modern society requires the likelihood of natural events with potentially disastrous consequences to be evaluated, even if probabilities of occurrence are diminishingly small. For some situations, it is not satisfactory to assert an event scenario probability is “negligible” or can be “ignored”. Judicial hearings or litigation may require risk levels to be quantified, in which case, statements of scientific confidence could be decisive. Internation- ally, e.g., for nuclear site safety evaluations, event likelihoods on order of 10–7/year are often considered for quantitative assessment. At such hazard levels, this might include evaluating the proposition that a particular volcano can deliver a future super-eruption, a supposition that could be attached to Aso volcano. But, simplistically taking the average recurrence interval between past caldera-forming eruptions at a given volcano is an unreliable guide to the likelihood of a future repeat: each past event represented a unique set of tectonic and magmatic conditions within a continually evolving volcanic system. Such processes are not temporally stationary nor statistically uniform. To evaluate the probability of a new M8 event at Aso, within the next 100 years, we performed a comprehensive stochastic probability uncertainty analysis using a model implemented with advanced computational Bayes Net (BN) software. Our eruption process model is informed by multiple strands of evidence from volcanology, petrology, geochemistry and geophysics, together with estimates of epistemic (knowledge) uncertainty, adduced from reviews of published data, modelling and from expert judgement elicitation. Several lines of evidence characterise the likely structure, magmatic composition and eruptive state of the present-day Aso volcano, which has had numerous smaller eruptions since Aso-4. To calculate the probability of another M8 eruption of Aso, we implemented probabilistic ‘Importance Sampling’ in our model. With this approach, we find the chance of an Aso-4 scale eruption (characterised by mean volume 500 km3 DRE and approximate 90% credible interval [210 .. 1200] km3 DRE) is less than 1–in–1 billion in the next 100 years (i.e., 〈 10–9 probability). Based on current vol- canological understanding and evidence, we believe this probability estimate is robust to within an order of magnitude.
    Description: Published
    Description: 5
    Description: OSV1: Verso la previsione dei fenomeni vulcanici pericolosi
    Description: N/A or not JCR
    Keywords: 05.05. Mathematical geophysics ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford UK : Blackwell Science Ltd
    Sedimentology 46 (1999), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The behaviour of subaerial particle-laden gravity currents (e.g. pyroclastic flows, lahars, debris flows, sediment-bearing floods and jökulhlaups) flowing into the sea has been simulated with analogue experiments. Flows of either saline solution, simple suspensions of silicon carbide (SiC) in water or complex suspensions of SiC and plastic particles in methanol were released down a slope into a tank of water. The excess momentum between subaerial and subaqueous flow is dissipated by a surface wave. At relatively low density contrasts between the tank water and the saline or simple suspensions, the flow mixture enters the water and forms a turbulent cloud involving extensive entrainment of water. The cloud then collapses gravitationally to form an underwater gravity current, which progresses along the tank floor. At higher density contrasts, the subaerial flow develops directly into a subaqueous flow. The flow slows and thickens in response to the reduced density contrast, which is driving motion, and then continues in the typical gravity current manner. Complex suspensions become dense flows along the tank floor or buoyant flows along the water surface, if the mixtures are sufficiently denser or lighter than water respectively. Flows of initially intermediate density are strongly influenced by the internal stratification of the subaerial flow. Material from the particulate-depleted upper sections of the subaerial flow becomes a buoyant gravity current along the water surface, whereas material from the particulate-enriched lower sections forms a dense flow along the tank floor. Sedimentation from the dense flow results in a reduction in bulk density until the mixture attains buoyancy, lifts off and becomes a secondary buoyant flow along the water surface. Jökulhlaups, lahars and debris flows are typically much denser than seawater and, thus, will usually form dense flows along the seabed. After sufficient sedimentation, the freshwater particulate mixture can lift off to form a buoyant flow at the sea surface, leading to a decoupling of the fine and coarse particles. Flood waters with low particulate concentrations (〈2%) may form buoyant flows immediately upon entering the ocean. Subaerial pyroclastic flows develop a pronounced internal stratification during subaerial run-out and, thus, a flow-splitting behaviour is probable, which agrees with evidence for sea surface and underwater flows from historic eruptions of Krakatau and Mont Pelée. A pyroclastic flow with a bulk density closer to that of sea water may form a turbulent cloud, resulting in the deposition of much of the pyroclasts close to the shore. Dense subaqueous pyroclastic flows will eventually lift off and form secondary buoyant flows, either before or after the transformation to a water-supported nature.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 297 (1982), S. 554-557 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The intimate mixing between different magmas of disparate densities, characteristic of some calc-alkaline magma systems, is explained by a new mechanism involving the emplacement of a layer of wet undersaturated mafic magma at the base of a magma chamber containing more differentiated magma. ...
    Type of Medium: Electronic Resource
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