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  • 1
    Publication Date: 2023-04-24
    Keywords: Aluminium oxide; Axial_Ridge; Axial Ridge; Barium; Caesium; Calcium oxide; Cerium; Chromium; Copper; Dysprosium; Eastern_Seamount; Eastern Seamount; Erbium; Europium; Event label; Gadolinium; Gallium; Geological sample; GEOS; Iron oxide, FeO; Lanthanum; Magnesium oxide; Manganese oxide; Neodymium; Nickel; Niobium; Phosphorus pentoxide; Potassium oxide; Rubidium; Samarium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; Strontium; Titanium dioxide; Vanadium; Western_Seamount; Western Seamount; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 507 data points
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  • 2
    Publication Date: 2023-01-14
    Keywords: Bridgeman_Is; Bridgeman Island; Deception_Is; Deception Island; Eastern_Seamount; Eastern Seamount; Elevation of event; Event label; GAP98; Geological sample; GEOS; Latitude of event; Lead-206/Lead-204 ratio; Lead-207/Lead-204 ratio; Lead-208/Lead-204 ratio; Longitude of event; Low_Head; Low Head; Melville_Peak; Melville Peak; Neodymium-143/Neodymium-144 ratio; Penguin_Is; Penguin Island; Sample code/label; Sampling on land; Strontium-87/Strontium-86 ratio; Western_Seamount; Western Seamount
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
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  • 3
    Publication Date: 2023-05-12
    Keywords: Area/locality; axial deep of Gibbs Rise; central seamount of G ridge; Date/Time of event; Dredge; DRG; Event label; Hook Ridge crater; HYDROARC; inner southern flank of NE-SW trending ridge at Hook Ridge; Latitude of event; Latitude of event 2; Lead-206/Lead-204 ratio; Lead-206/Lead-204 ratio, error; Lead-207/Lead-204 ratio; Lead-207/Lead-204 ratio, error; Lead-208/Lead-204 ratio; Lead-208/Lead-204 ratio, error; Longitude of event; Longitude of event 2; lower NE end of G ridge; lower NE flank of G ridge; lower western flank of Bridgeman Ridge; lower western flank of Gibbs Rise; middle western flank of Gibbs Rise; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; Sample ID; seamount at northern flank of axial deep at Spanish Rise; seamount at NW end of Spanish Rise; seamount at SW end of G ridge; seamount at SW flank of axial deep at Spanish Rise; seamount in axial deep at Spanish Rise; seamount on NE flank of Spanish Rise; second highest seamount at SW end of G ridge; small seamount NW of Bridgeman Ridge; SO155; SO155_02DR; SO155_03DR; SO155_04DR; SO155_07GTV; SO155_13DR; SO155_14DR; SO155_15DR; SO155_16DR; SO155_17DR; SO155_18DR; SO155_20DR; SO155_21DR; SO155_23DR; SO155_25DR; SO155_26DR; SO155_27DR; SO155_28DR; SO155_38DR; Sonne; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error; Television-Grab; TVG; upper western flank of Bridgeman Ridge
    Type: Dataset
    Format: text/tab-separated-values, 248 data points
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  • 4
    Publication Date: 2023-05-12
    Keywords: Area/locality; Heat flow; LATITUDE; LONGITUDE; Method comment; Sample, optional label/labor no
    Type: Dataset
    Format: text/tab-separated-values, 163 data points
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Fretzdorff, Susanne; Worthington, Tim J; Haase, Karsten M; Hekinian, Roger; Franz, Leander; Keller, Randall A; Stoffers, Peter (2004): Magmatism in the Bransfield Basin: Rifting of the South Shetland Arc? Journal of Geophysical Research, 109(B12), https://doi.org/10.1029/2004JB003046
    Publication Date: 2023-10-28
    Description: Bransfield Basin is an actively extending marginal basin separating the inactive South Shetland arc from the northern Antarctic Peninsula. Rift-related volcanism is widespread throughout the central Bransfield Basin, but the wider eastern Bransfield Basin was previously unsampled. Lavas recovered from the eastern subbasin form three distinct groups: (1) Bransfield Group has moderate large-ion lithophile element (LILE) enrichment relative to normal mid-ocean ridge basalt (NMORB), (2) Gibbs Group has strong LILE enrichment and is restricted to a relic seamount interpreted as part of the South Shetland arc, and (3) fresh alkali basalt was recovered from the NE part of the basin near Spanish Rise. The subduction-related component in Bransfield and Gibbs Group lavas is a LILE-rich fluid with radiogenic Sr, Nd, and Pb isotope compositions derived predominantly from subducting sediment. These lavas can be modeled as melts from Pacific MORB source mantle contaminated by up to 5% of the subduction-related component. They further reveal that Pacific mantle, rather than South Atlantic mantle, has underlain Bransfield Basin since 3 Ma. Magma productivity decreases abruptly east of Bridgeman Rise, and lavas with the least subduction component outcrop at that end. Both the eastward decrease in subduction component and occurrence of young alkali basalts require that subduction-modified mantle generated during the lifetime of the South Shetland arc has been progressively removed from NE to SW. This is inconsistent with previous models suggesting continued slow subduction at the South Shetland Trench but instead favors models in which the South Scotia Ridge fault has propagated westward since 3 Ma generating transtension across the basin.
    Keywords: Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
    Publication Date: 2023-07-10
    Keywords: Aluminium oxide; Area/locality; axial deep of Gibbs Rise; Barium; Caesium; Calcium oxide; central seamount of G ridge; Cerium; Chromium; Cobalt; Copper; Date/Time of event; Dredge; DRG; Dysprosium; Elements, total; Erbium; Europium; Event label; Gadolinium; Group; Hafnium; Holmium; Hook Ridge crater; HYDROARC; Inductively coupled plasma - mass spectrometry (ICP-MS); inner southern flank of NE-SW trending ridge at Hook Ridge; Iron oxide, Fe2O3; Lanthanum; Latitude of event; Latitude of event 2; Lead; Longitude of event; Longitude of event 2; Loss on ignition; lower NE end of G ridge; lower NE flank of G ridge; lower western flank of Bridgeman Ridge; lower western flank of Gibbs Rise; Lutetium; Magnesium oxide; Manganese oxide; middle western flank of Gibbs Rise; Neodymium; Nickel; Niobium; Phosphorus pentoxide; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample ID; Scandium; seamount at northern flank of axial deep at Spanish Rise; seamount at NW end of Spanish Rise; seamount at SW end of G ridge; seamount at SW flank of axial deep at Spanish Rise; seamount in axial deep at Spanish Rise; seamount on NE flank of Spanish Rise; second highest seamount at SW end of G ridge; Silicon dioxide; small seamount NW of Bridgeman Ridge; SO155; SO155_02DR; SO155_03DR; SO155_04DR; SO155_07GTV; SO155_13DR; SO155_14DR; SO155_15DR; SO155_16DR; SO155_17DR; SO155_18DR; SO155_20DR; SO155_21DR; SO155_23DR; SO155_25DR; SO155_26DR; SO155_27DR; SO155_28DR; SO155_38DR; Sodium oxide; Sonne; Strontium; Tantalum; Television-Grab; Terbium; Thallium; Thorium; Thulium; Titanium dioxide; TVG; upper western flank of Bridgeman Ridge; Uranium; X-ray fluorescence (XRF); Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 2107 data points
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Keller, Randall A; Fisk, Martin R; White, William M (2000): Isotopic evidence for Late Cretaceous plume-ridge interaction at the Hawaiian hotspot. Nature, 405(6787), 673-676, https://doi.org/10.1038/35015057
    Publication Date: 2024-01-09
    Description: When a mantle plume interacts with a mid-ocean ridge, both are noticeably affected. The mid-ocean ridge can display anomalously shallow bathymetry, excess volcanism, thickened crust, asymmetric sea-floor spreading and a plume component in the composition of the ridge basalts (Schilling, 1973, doi:10.1038/242565a0; Verma et al., 1983, doi:10.1038/306654a0; Ito and Lin, 1995, doi:10.1130/0091-7613(1995)023〈0657:OSCHIC〉2.3.CO;2; Müller et al., 1998, doi:10.1038/24850). The hotspot-related volcanism can be drawn closer to the ridge, and its geochemical composition can also be affected (Ito and Lin, 1995, doi:10.1130/0091-7613(1995)023〈0657:OSCHIC〉2.3.CO;2; White et al., 1993, doi:10.1029/93JB02018; Kincaid et al., 1995, doi:10.1038/376758a0; Kingsley and Schilling, 1998, doi:10.1029/98JB01496 ). Here we present Sr–Nd–Pb isotopic analyses of samples from the next-to-oldest seamount in the Hawaiian hotspot track, the Detroit seamount at 51° N, which show that, 81 Myr ago, the Hawaiian hotspot produced volcanism with an isotopic signature indistinguishable from mid-ocean ridge basalt. This composition is unprecedented in the known volcanism from the Hawaiian hotspot, but is consistent with the interpretation from plate reconstructions (Mammerickx and Sharman, 1988, doi:10.1029/JB093iB04p03009) that the hotspot was located close to a mid-ocean ridge about 80 Myr ago. As the rising mantle plume encountered the hot, low-viscosity asthenosphere and hot, thin lithosphere near the spreading centre, it appears to have entrained enough of the isotopically depleted upper mantle to overwhelm the chemical characteristics of the plume itself. The Hawaiian hotspot thus joins the growing list of hotspots that have interacted with a rift early in their history.
    Keywords: 145-883F; 145-884C; 19-192A; 55-433C; AGE; Age, comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Joides Resolution; Lanthanum/Samarium ratio; Latitude of event; Lead-206/Lead-204 ratio; Lead-207/Lead-204 ratio; Lead-208/Lead-204 ratio; Leg145; Leg19; Leg55; Longitude of event; Neodymium-143/Neodymium-144 ratio; North Pacific/GUYOT; North Pacific/SEAMOUNT; North Pacific Ocean; Ocean Drilling Program; ODP; Rubidium/Strontium ratio; Samarium/Neodymium ratio; Sample code/label; Strontium-87/Strontium-86 ratio; Thorium/Lead ratio; Uranium/Lead ratio
    Type: Dataset
    Format: text/tab-separated-values, 99 data points
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  • 8
    Publication Date: 2024-01-09
    Description: Age-progressive, linear seamount chains in the northeast Pacific appear to have formed as the Pacific plate passed over a set of stationary hotspots; however, some anomalously young ages and the lack of an "enriched" isotopic signature in basalts from the seamounts do not fit the standard hotspot model. For example, published ages (28-30 Ma) for basalts dredged from the Patton-Murray seamount platform in the Gulf of Alaska are 2-4 m.y. younger than the time when the platform was above the Cobb hotspot. However, the lowermost basalt recovered by ocean drilling on Patton-Murray yielded a 40Ar-39Ar age of 33 Ma. This age exactly coincides with the time when the seamount platform was above the Cobb hotspot, consistent with a stationary, long-lived mantle plume. A 27 Ma alkalic basalt flow recovered 8 m above the 33 Ma basalt is similar in age and composition to the previously dredged basalts, and may be the alkalic capping phase typical of many hotspot volcanoes. A 17 Ma tholeiitic basalt sill recovered 5 m above the 27 Ma basalt was emplaced long after the seamount platform moved away from the hotspot, and may be associated with a period of intraplate extension. Anomalously young phases of volcanism on this and other hotspot seamounts suggest that they can be volcanically rejuvenated by nonhotspot causes, but this rejuvenation does not rule out the hotspot model as an explanation for the initial creation of the seamount platform. The lack of an "enriched" isotopic signature in any of these basalts shows that enriched compositions are not necessary characteristics of plume-related basalts. The isotopic compositions of the lower basalts are slightly more depleted than the 0-9 Ma products of the Cobb hotspot, despite the fact that the hotspot was closer to a spreading ridge at 0-9 Ma. It appears that this hotspot, like several others, has become more enriched with time.
    Keywords: 145-887D; Barium; Caesium; Calculated; Cerium; Depth, bottom/max; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Hafnium; Holmium; Inductively coupled plasma - mass spectrometry (ICP-MS); Isotope ratio mass spectrometry; Joides Resolution; Lanthanum; Lead; Lead-206/Lead-204 ratio; Lead-207/Lead-204 ratio; Lead-208/Lead-204 ratio; Leg145; Lithologic unit/sequence; Lutetium; Neodymium; Neodymium-143/Neodymium-144 ratio; Niobium; North Pacific Ocean; Ocean Drilling Program; ODP; Praseodymium; Rubidium; Samarium; Sample code/label; Strontium; Strontium-87/Strontium-86 ratio; Tantalum; Terbium; Thorium; Thulium; Uranium; Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 405 (2000), S. 673-676 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] When a mantle plume interacts with a mid-ocean ridge, both are noticeably affected. The mid-ocean ridge can display anomalously shallow bathymetry, excess volcanism, thickened crust, asymmetric sea-floor spreading and a plume component in the composition of the ridge basalts. The ...
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 1998-08-01
    Print ISSN: 0020-6814
    Electronic ISSN: 1938-2839
    Topics: Geosciences
    Published by Taylor & Francis
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