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  • 1
    In: Earth and planetary science letters, Amsterdam [u.a.] : Elsevier, 1966, 275(2008), 1/2, Seite 61-69, 1385-013X
    In: volume:275
    In: year:2008
    In: number:1/2
    In: pages:61-69
    Description / Table of Contents: During segment-scale studies of the southern Mid-Atlantic Ridge (MAR), 712° S, we found evidence in the water column for high-temperature hydrothermal activity, off-axis, east of Ascension Island. Extensive water column and seafloor work using both standard CTD and deep submergence AUV and ROV deployments led to the discovery and sampling of the Drachenschlundʺ (Dragon Throatʺ) black smoker vent at 8ʿ17.87? S/13ʿ30.45? W in 2915 m water depth. The vent is flanked by several inactive chimney structures in a field we have named Nibelungenʺ. The site is located 6 km south of a non-transform offset between two adjacent 2nd-order ridge-segments and 9 km east of the presently-active, northward-propagating A2 ridge-segment, on a prominent outward-facing fault scarp. Both vent-fluid compositions and host-rock analyses show this site to be an ultramafic-hosted system, the first of its kind to be found on the southern MAR. The thermal output of this single vent, based on plume rise-height information, is estimated to be 60 ± 15 MW. This value is high for a single black smokerʺ vent but small for an entire field. The tectonic setting and low He content of the vent fluids imply that high-temperature off-axis venting at Drachenschlundʺ is driven not by magmatic processes, as at the majority of on-axis hydrothermal systems, but by residual heat minedʺ from the deeper lithosphere. Whether this heat is being extracted from high-temperature mantle peridotites or deep crustal cumulates formed at the duellingʺ non-transfrom offset is unclear, in either case the Drachenschlund vent provides the first direct observations of how cooling of deeper parts of the lithosphere, at least at slow-spreading ridges, may be occurring.
    Type of Medium: Online Resource
    Pages: Ill., grap. Darst
    ISSN: 1385-013X
    Language: English
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  • 2
    Publication Date: 2020-02-24
    Description: Explosions of hot water, steam, and gas are common periodic events of subaerial geothermal systems. These highly destructive events may cause loss of life and substantial damage to infrastructure, especially in densely populated areas and where geothermal systems are actively exploited for energy. We report on the occurrence of a large number of explosion craters associated with the offshore venting of gas and thermal waters at the volcanic island of Panarea, Italy, demonstrating that violent explosions similar to those observed on land also are common in the shallow submarine environment. With diameters ranging from 5 to over 100 m, the observed circular seafloor depressions record a history of major gas explosions caused by frequent perturbation of the submarine geothermal system over the past 10,000 years. Estimates of the total gas flux indicate that the Panarea geothermal system released over 70 Mt of CO2 over this period of time, suggesting that CO2 venting at submerged arc volcanoes contributes significantly to the global atmospheric budget of this greenhouse gas. The findings at Panarea highlight that shallow submarine gas explosions represent a previously unrecognized volcanic hazard around populated volcanic islands that needs to be taken into account in the development of risk management strategies.
    Description: Published
    Description: 1937-1944
    Description: 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
    Description: JCR Journal
    Description: restricted
    Keywords: Gas explosions . ; Geothermal systems ; Submarine gas venting ; Volcanic CO2 flux ; Volcanic hazards ; Panarea island ; 04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2017-02-09
    Description: During segment-scale studies of the southern Mid-Atlantic Ridge (MAR), 7–12° S, we found evidence in the water column for high-temperature hydrothermal activity, off-axis, east of Ascension Island. Extensive water column and seafloor work using both standard CTD and deep submergence AUV and ROV deployments led to the discovery and sampling of the “Drachenschlund” (“Dragon Throat”) black smoker vent at 8°17.87′ S/13°30.45′ W in 2915 m water depth. The vent is flanked by several inactive chimney structures in a field we have named “Nibelungen”. The site is located 6 km south of a non-transform offset between two adjacent 2nd-order ridge-segments and 9 km east of the presently-active, northward-propagating A2 ridge-segment, on a prominent outward-facing fault scarp. Both vent-fluid compositions and host-rock analyses show this site to be an ultramafic-hosted system, the first of its kind to be found on the southern MAR. The thermal output of this single vent, based on plume rise-height information, is estimated to be 60 ± 15 MW. This value is high for a single “black smoker” vent but small for an entire field. The tectonic setting and low He content of the vent fluids imply that high-temperature off-axis venting at “Drachenschlund” is driven not by magmatic processes, as at the majority of on-axis hydrothermal systems, but by residual heat “mined” from the deeper lithosphere. Whether this heat is being extracted from high-temperature mantle peridotites or deep crustal cumulates formed at the “duelling” non-transfrom offset is unclear, in either case the Drachenschlund vent provides the first direct observations of how cooling of deeper parts of the lithosphere, at least at slow-spreading ridges, may be occurring.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2020-02-12
    Description: Die Potenzialfeld-Messungen östlich der Ortschaft Kreckwitz (Kreis Bautzen, Ost-Sachsen) ergaben Anzeichen für die Existenz einer Maarstruktur, die der von Baruth ähnlich ist. Die an 104 Schwere- und 371 Magnetfeldstationen durchgeführten Messungen zeigen ein Minimum der Bougueranomalie von (relativ) -4.5 · 10-5 m/s 2 und neben zwei kleineren negativen Anomalien eine positive des magnetischen Totalfeldes von ca. +200 nT (diese Messungen) bis +250 nT (Landesaufnahme). Alle Stationen sind bezüglich ihrer Höhe in das Höhennetz des Freistaates Sachsen eingebunden worden; zum Einsatz kamen differential GPS Mes- sungen, aber auch konventionelle Höhenbestimmungen. Für den Nahbereich ist für die topographische Nahfeldreduktion das Gelände mit einem SM 41 aufgenommen worden. Die Schwerewerte wurden mit LaCoste & Romberg G-Gravimetern bestimmt und sind Instrumentengang- und Gezeiten korrigiert und topographisch mit einem Reduktionsradius von 10 km reduziert worden. Für die Beseitigung des magnetischen Tagesganges wurde er an einer permanenten Basisstation im Messgebiet aufgezeichnet. Die aus diesen Messungen resultierenden Anomalien, die zusammen mit den Daten der Landesaufnahme in Karten interpretiert werden, ergaben zusammen mit den 3D-Modellierungen der gemessenen gravimetrischen Anomalien das typische Strukturbild eines Maares.
    Type: info:eu-repo/semantics/article
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