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  • GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel  (9)
  • Wiley  (2)
  • Deutsches GeoForschungsZentrum GFZ  (1)
  • 1
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
    Publication Date: 2023-08-08
    Description: RV METEOR Expedition M191 „SUAVE“, 16.07. – 05.08.2023, Algeciras – Piraeus.
    Type: Report , NonPeerReviewed
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  • 2
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    Deutsches GeoForschungsZentrum GFZ
    In:  In: Vulkanismus und Gesellschaft: Zwischen Risiko, Vorsorge und Faszination. , ed. by Jorzik, O., Kandarr, J., Klinghammer, P. and Spreen, D. ESKP-Themenspezial . Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany, pp. 117-120.
    Publication Date: 2021-01-26
    Description: Millionen von Quadratkilometern im Meer sind von gigantischen Lavaschichten bedeckt. Sie sind das Resultat des Flutbasalt-Vulkanismus. Dabei entstand vulkanisches Gestein, welches auch zur Entfernung von CO2 aus der Atmosphäre beitragen kann. Erdgeschichtlich führte die-ser Vulkanismus jedoch immer wieder zum Massenaussterben von Arten.
    Type: Book chapter , NonPeerReviewed
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  • 3
    Publication Date: 2023-02-09
    Description: Despite their large number and in contrast to seamount chains, small solitary seamounts/seamount groups have rarely been sampled and therefore their origins remain enigmatic. Here we present 40Ar/39Ar, trace element and Nd‐Pb‐Hf isotope data from the solitary Demenitskoy Seamount, the isolated Tolkien seamount group and the Krylov Seamount and Ridge in the Canary Basin. Their chemical compositions range from intraplate ocean‐island‐basalt (Demenitskoy) to normal‐ and enriched‐mid‐ocean‐ridge‐basalt types (Tolkien and Krylov system, respectively). Lavas from all three seamount groups, however, show geochemical evidence for involvement of enriched (Canary/Cape Verde) plume material. Seismic tomography shows that large areas around these mantle plumes are affected by dispersal of presumably low‐velocity material, which also could have fed nearby isolated seamounts with diffusely‐upwelling plume material. This process may be extremely widespread but has been poorly studied to date.
    Type: Article , PeerReviewed
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  • 4
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
    Publication Date: 2024-01-10
    Description: FS METEOR, 31.07. –29.08.2021, Emden – Emden. 1. Wochenbericht (31.07-01.08. 2021) Die FS METEOR-Expedition M176 wird vom GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel in Zusammenarbeit mit dem GeoZentrum Nordbayern der Universität Erlangen-Nürnberg durchgeführt. Arbeitsgebiete sind die westliche Biskaya und der Azoren-Biskaya-Rücken, eine 750 km lange untermeerische Gebirgskette unbekannten Ursprungs.
    Type: Report , NonPeerReviewed
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  • 5
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
    Publication Date: 2024-01-10
    Description: FS METEOR, 31.07. –29.08.2021, Emden – Emden. 3. Wochenbericht (09.08-15.08.2021) Die FS METEOR-Expedition M176 wird vom GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel in Zusammenarbeit mit dem GeoZentrum Nordbayern der Universität Erlangen-Nürnberg durchgeführt. Arbeitsgebiete sind die westliche Biskaya und der Azoren-Biskaya-Rücken, eine 750 km lange untermeerische Gebirgskette unbekannten Ursprungs.
    Type: Report , NonPeerReviewed
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  • 6
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
    Publication Date: 2024-01-10
    Description: FS METEOR, 31.07. –29.08.2021, Emden – Emden. 4. Wochenbericht (16.08-22.08.2021) Die FS METEOR-Expedition M176 wird vom GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel in Zusammenarbeit mit dem GeoZentrum Nordbayern der Universität Erlangen-Nürnberg durchgeführt. Arbeitsgebiete sind die westliche Biskaya und der Azoren-Biskaya-Rücken, eine 750 km lange untermeerische Gebirgskette unbekannten Ursprungs.
    Type: Report , NonPeerReviewed
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  • 7
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
    Publication Date: 2024-01-10
    Description: FS METEOR, 31.07. –29.08.2021, Emden – Emden. 2. Wochenbericht (02.08-08.08.2021) Die FS METEOR-Expedition M176 wird vom GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel in Zusammenarbeit mit dem GeoZentrum Nordbayern der Universität Erlangen-Nürnberg durchgeführt. Arbeitsgebiete sind die westliche Biskaya und der Azoren-Biskaya-Rücken, eine 750 km lange untermeerische Gebirgskette unbekannten Ursprungs.
    Type: Report , NonPeerReviewed
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  • 8
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
    Publication Date: 2024-01-10
    Description: FS METEOR, 31.07. – 29.08.2021, Emden – Emden. 5. Wochenbericht (23.08-29.08.2021) Die FS METEOR-Expedition M176 wird vom GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel in Zusammenarbeit mit dem GeoZentrum Nordbayern der Universität Erlangen-Nürnberg durchgeführt. Arbeitsgebiete sind die westliche Biskaya und der Azoren-Biskaya-Rücken, eine 750 km lange untermeerische Gebirgskette unbekannten Ursprungs.
    Type: Report , NonPeerReviewed
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  • 9
    Publication Date: 2024-02-07
    Description: Although previous findings support an origin of the Shatsky Rise igneous plateau (Northwest Pacific) through interaction of a mantle plume with a mid-ocean ridge triple junction, the evidence for the involvement of a mantle plume is equivocal. The identification of an intraplate hotspot track emanating from the plateau could solve this controversy. Here we present major and trace element geochemical data from two different bathymetric features that emanate from the youngest end of Shatsky Rise: Papanin Ridge and the Ojin Rise Seamount province. Combining our results with plate tectonic reconstructions, we conclude that Papanin Ridge represents a hotspot track formed by plume-ridge interaction. Whereas the southwestern part was formed along the path of the retreating Pacific-Farallon-Izanagi triple junction, the northeastern part was built by preferential drainage into its Pacific-Farallon branch. In contrast, the Ojin Rise Seamounts formed as a true intraplate hotspot track of the Shatsky plume tail. Our wide-ranging study reveals systematic spatial geochemical variations, consistent with a lithospheric thickness control on magma composition derived from melting a heterogeneous plume source. The recognition of two hotspot tracks and in particular of the Ojin Rise Seamounts as an intraplate hotspot track that is directly linked to Shatsky plateau volcanism both in terms of geochemistry and plate tectonic reconstructions confirms the long-disputed involvement of a mantle plume for the formation of Shatsky Rise.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 10
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
    Publication Date: 2023-07-24
    Description: RV METEOR Expedition M191 „SUAVE“, 16.07. – 05.08.2023, Algeciras – Piraeus. The RV METEOR expedition M191 (SUAVE = Submarine volcanism in the western Sicilian Channel) is a joint project of GEOMAR Helmholtz Centre for Ocean Research Kiel (Germany), the University of Malta (Malta), the University of Birmingham (United Kingdom) and the Instituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS) (Italy) with cruise participants from these institutes as well as from the Monterey Bay Aquarium Research Institute (MBARI) (USA), Victoria University Wellington (New Zealand), and the Universities of Oxford and Edinburgh (United Kingdom). The main working area is the Sicilian Channel, located south of Sicily (Fig. 1), where tectonic movements cause melting in the upper mantle, presumably by decompression along extensional fracture zones and rifts. Therefore, magmatism is widespread and includes the volcanic islands of Pantelleria and Linosa, and numerous submarine volcanic edifices. Although some magmatic products date to 9.5 Ma, submarine eruptions have been reported up to historical times, such as at Pinne Bank during the first Punic War (264-261 BC), Graham Bank in 1831, and 5 km NW of Pantelleria in 1891.
    Type: Report , NonPeerReviewed
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