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Egeberg, Per Kristian; Brunfelt, Arild O; Stabel, Arne S (1992): (Table 1) Composition of selected ash layers in ODP Site 126-792 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.774205, Supplement to: Egeberg, PK et al. (1992): Characterization and correlation of megascopic tephras in Site 792 cores from the Izu-Ogasawara Forearc Basin (Japan) by trace elements and 87Sr/86Sr and 143Nd/144Nd isotopes. In: Taylor, B; Fujioka, K; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 126, 457-465, https://doi.org/10.2973/odp.proc.sr.126.149.1992

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Published: 1992 (exact date unknown)DOI registered: 2012-02-15

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Abstract:
Glass shards from 26 megascopic tephras (1-29 cm thick) were separated and analyzed for 26 elements and 87Sr/86Sr and 143Nd/144Nd isotope ratios. The isotope data allowed us to assess the degree of alteration of the samples. The separates contain less than 10% of palagonitized glass or secondary alteration minerals. Correlation diagrams and multivariate analyses have been used to characterize the glass shards in a tectonic setting and group the tephras according to their magmatic affinity. Four tholeiitic groups, two calc-alkaline groups, and one group with glass of shoshonitic affinity can be distinguished. The tholeiitic groups form a time series; however, judging from the rare-earth-element patterns and the temporal variations of the Ce/Yb ratios, the evolution is not unidirectional from strong to weak tholeiitic affinity.
The tephras have been correlated with volcanism along the Izu-Ogasawara and Ryukyu arcs by means of trace element distribution, 87Sr/86Sr ratios, and their magmatic affinity. The tholeiitic layers were derived from volcanoes on the Izu-Ogasawara Arc, most probably from the volcanic island Hachijojima. Only one group of the calc-alkaline layers can have derived from the Izu-Ogasawara Arc. The other calc-alkaline layers and the two layers with shoshonitic affinity probably derive from volcanism along the Ryukyu Arc.
Project(s):
Coverage:
Median Latitude: 32.399600 * Median Longitude: 140.380000 * South-bound Latitude: 32.399400 * West-bound Longitude: 140.379300 * North-bound Latitude: 32.399800 * East-bound Longitude: 140.380700
Date/Time Start: 1989-05-17T01:36:00 * Date/Time End: 1989-05-26T06:40:00
Minimum DEPTH, sediment/rock: 6.34 m * Maximum DEPTH, sediment/rock: 309.45 m
Event(s):
126-792A * Latitude: 32.399800 * Longitude: 140.380700 * Date/Time Start: 1989-05-17T01:36:00 * Date/Time End: 1989-05-17T17:25:00 * Elevation: -1798.0 m * Penetration: 95 m * Recovery: 72.09 m * Location: North Pacific Ocean * Campaign: Leg126 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 95 m cored; 0 m drilled; 75.9 % recovery
126-792E * Latitude: 32.399400 * Longitude: 140.379300 * Date/Time Start: 1989-05-19T04:55:00 * Date/Time End: 1989-05-26T06:40:00 * Elevation: -1798.0 m * Penetration: 885.9 m * Recovery: 362.07 m * Location: North Pacific Ocean * Campaign: Leg126 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 78 cores; 750.3 m cored; 0 m drilled; 48.3 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Sample code/labelSample labelEgeberg, Per KristianDSDP/ODP/IODP sample designation
3Layer descriptionLayerEgeberg, Per KristianShipboard Scientific Party, ash layer number
4Layer descriptionLayerEgeberg, Per KristianShipboard Scientific Party, ash layer number
5DEPTH, sediment/rockDepth sedmGeocode – mbsf
6AGEAgeka BPGeocode
7Layer thicknessThicknessmEgeberg, Per Kristian
8Sodium oxideNa2O%Egeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 5.4 %
9SeleniumSemg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 2.3 %
10Titanium dioxideTiO2%Egeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 9.9 %
11Iron oxide, Fe2O3Fe2O3%Egeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 2.1 %
12CobaltComg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 1.9 %
13RubidiumRbmg/kgEgeberg, Per KristianIsotope dilutionRel. Std. = 0.03 %
14StrontiumSrmg/kgEgeberg, Per KristianIsotope dilutionRel. Std. = 0.03 %
15ZirconiumZrmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 9.02 %
16AntimonySbmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 25.76 %
17CaesiumCsmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 7.01 %
18BariumBamg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 4.75 %
19LanthanumLamg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 6.64 %
20CeriumCemg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 12.4 %
21NeodymiumNdmg/kgEgeberg, Per KristianIsotope dilutionRel. Std. = 0.05 %
22SamariumSmmg/kgEgeberg, Per KristianIsotope dilutionRel. Std. = 0.05 %
23EuropiumEumg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 2.04 %
24TerbiumTbmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 0.8 %
25HolmiumHomg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 5 %
26ThuliumTmmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 1.78 %
27YtterbiumYbmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 1.86 %
28LutetiumLumg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 9.83 %
29HafniumHfmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 2.42 %
30TantalumTamg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 1.58 %
31TungstenWmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 10.6 %
32ThoriumThmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 3.38 %
33UraniumUmg/kgEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 12.9 %
34Strontium-87/Strontium-86 ratio87Sr/86SrEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 0.0019 %
35Neodymium-143/Neodymium-144 ratio143Nd/144NdEgeberg, Per KristianInstrumental neutron activation analysis (INAA) (Reimann et al., 1998)Rel. Std. = 0.00075 %
Size:
827 data points

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