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  • Rock mechanics  (8)
  • 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions  (3)
  • Geological Society of London  (5)
  • Institute of Physics
  • Molecular Diversity Preservation International
  • Project Management of the Continental Deep Drilling Programme of the Fed. Rep. of Germany in the Geol. Survey of Lower Saxony
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  • 1
    Publikationsdatum: 2020-11-26
    Beschreibung: We describe the evolution of the volcanic activity and deformation patterns observed at Mount Etna during the July–August 2001 eruption. Seismicity started at 3000 m below sea level on 13 July, accompanied by moderate ground swelling. Ground deformation culminated on 16 July with the development of a NE–SW graben c. 500 m wide and c. 1 m deep in the Cisternazza area at 2600–2500 m above sea level on the southern slope of the volcano. On 17 July, the eruption started at the summit of Mount Etna from the SE Crater (central–lateral eruptive system), from which two radial, c. 30 m wide, c. 3000 m long fracture zones, associated with eruptive fissures, propagated both southward (17 July) and northeastward (20 July). On 18 July, a new vent formed at 2100 m elevation, at the southern base of the Montagnola, followed on the next day by the opening of a vent further upslope, at 2550 m (eccentric eruptive system). The eruption lasted for 3 weeks. Approximately 80% of the total lava volume was erupted from the 2100 m and the 2550 m vents. The collected structural data suggest that the Cisternazza graben developed as a passive local response of the volcanic edifice to the ascent of a north–south eccentric dyke, which eventually reached the ground surface in the Montagnola area (18–19 July). In contrast, the two narrow fracture zones radiating from the summit are interpreted as the lateral propagation, from the conduit of the SE Crater, of north–south- and NE–SW-oriented shallow dykes, 2–3 m wide. The evolution of the fracture pattern together with other volcanological data (magma ascent and effusion rate, eruptive style, petrochemical characteristics of the erupted products, and petrology of xenoliths within magma) suggest that the eccentric and central–lateral eruptions were fed by two distinct magmatic systems. Examples of eccentric activity accompanied by central–lateral events have never been described before at Etna.
    Beschreibung: Published
    Beschreibung: 531-544
    Beschreibung: 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
    Beschreibung: 3.2. Tettonica attiva
    Beschreibung: 3.5. Geologia e storia dei sistemi vulcanici
    Beschreibung: 3.6. Fisica del vulcanismo
    Beschreibung: JCR Journal
    Beschreibung: reserved
    Schlagwort(e): Mount Etna ; July–August 2001 Eruption ; magmas ; dykes ; 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous ; 04. Solid Earth::04.04. Geology::04.04.09. Structural geology ; 04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous ; 04. Solid Earth::04.07. Tectonophysics::04.07.05. Stress ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous ; 04. Solid Earth::04.08. Volcanology::04.08.03. Magmas ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring ; 04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk ; 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    Geological Society of London
    Publikationsdatum: 2017-04-04
    Beschreibung: Although controversy exists about the age of its most recent eruption (either 36 ka or ,23 ka), Colli Albani volcano is unanimously considered to be quiescent and not exinct. During the Holocene, several lahars were generated by overflows from Albano crater lake up to the fourth century BCE, when the Romans excavated a drainage tunnel to keep the lake level below the crater rim. Such recent activity, together with the frequent occurrence of seismic swarms underneath the crater zone, the ongoing uplift of the volcanic edifice and the magmatic affinity of the emitted gas, indicate the presence of an active magma chamber. The most likely site for a new eruption is the deep crater hosted in the southern part of the Lake Albano, where the last eruptive events occurred. Any eruption would have a strong explosive character enhanced by the interaction of magma with the water of the lake and would endanger a densely inhabited area up to the outskirts of Rome. The hazard of a new overflow from Lake Albano is very low because of the present low level of the lae. There is instead a potential for CO2 release from the deep lake water following the occurrence of rollovers, which would threaten the lake shore, a site where thousands of people spend their vacations in the summer. However, the content of dissolved CO2 is presently far from saturation and no Nyos-type events will occur today. Presently, the main hazard is related to strong gas emissions (CO2, H2S and Rn) from fractured zones and gas blowouts from wells reaching shallow gas-pressurized aquifers.
    Beschreibung: Published
    Beschreibung: 279 – 297
    Beschreibung: 4.3. TTC - Scenari di pericolosità vulcanica
    Beschreibung: reserved
    Schlagwort(e): Colli Albani, volcanic hazard ; 04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk ; 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: book chapter
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2017-04-04
    Beschreibung: During volcanic eruptions, measurements of the rate at which magma is erupted underpin hazard assessments. For eruptions dominated by the effusion of lava, estimates are often made using satellite data; here, in a case study at Mount Etna (Sicily), we make the first measurements based on terrestrial laser scanning (TLS), and we also include explosive products. During the study period (17–21 July 2012), regular Strombolian explosions were occurring within the Bocca Nuova crater, producing a ~50 m-high scoria cone and a small lava flow field. TLS surveys over multi-day intervals determined a mean cone growth rate (effusive and explosive products) of ~0.24 m3·s−1. Differences between 0.3-m resolution DEMs acquired at 10-minute intervals captured the evolution of a breakout lava flow lobe advancing at 0.01–0.03 m3·s−1. Partial occlusion within the crater prevented similar measurement of the main flow, but integrating TLS data with time-lapse imagery enabled lava viscosity (7.4 × 105 Pa·s) to be derived from surface velocities and, hence, a flux of 0.11 m3·s−1 to be calculated. Total dense rock equivalent magma discharge estimates are ~0.1–0.2 m3·s−1 over the measurement period and suggest that simultaneous estimates from satellite data are somewhat overestimated. Our results support the use of integrated TLS and time-lapse photography for ground-truthing space-based measurements and highlight the value of interactive image analysis when automated approaches, such as particle image velocimetry (PIV), fail.
    Beschreibung: Published
    Beschreibung: 14967 - 14987
    Beschreibung: 3V. Dinamiche e scenari eruttivi
    Beschreibung: JCR Journal
    Beschreibung: open
    Schlagwort(e): lava flow; scoria cone; effusion rate; terrestrial laser scanning; time-lapse photography; Mt. Etna ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring ; 04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques ; 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    facet.materialart.
    Unbekannt
    Institute of Physics
    In:  Professional Paper, Boundary Element Methods. Theory and Application, Bristol, Institute of Physics, vol. 9, no. 16, pp. 1-23, (ISBN 1-4020-1729-4)
    Publikationsdatum: 1986
    Schlagwort(e): Stress ; Rock mechanics ; Stress intensity factor ; Boundary Element Method ; Fracture ; ENDNOTE?
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
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    Unbekannt
    Geological Society of London
    In:  New York, Geological Society of London, vol. 231, no. 3, pp. 2-203, (ISBN 1-86239-165-3, vi + 330 pp.)
    Schlagwort(e): Rock mechanics ; Structural geology ; cracks and fractures (.NE. fracturing) ; Fracture ; Friction
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
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    Unbekannt
    Project Management of the Continental Deep Drilling Programme of the Fed. Rep. of Germany in the Geol. Survey of Lower Saxony
    In:  Professional Paper, Contributions to the 6th Annual KTB-Colloquium: Geoscientific Results, Hannover, Project Management of the Continental Deep Drilling Programme of the Fed. Rep. of Germany in the Geol. Survey of Lower Saxony, vol. 172, no. 16, pp. 171-174, (ISBN 0080419208)
    Publikationsdatum: 1993
    Schlagwort(e): Stress ; Borehole breakouts ; Rock mechanics
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
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    Unbekannt
    Project Management of the Continental Deep Drilling Programme of the Fed. Rep. of Germany in the Geol. Survey of Lower Saxony
    In:  Bull., Polar Proj. OP-O3A4, Beiträge zum 2. KTB-Kolloquium, Hannover, Project Management of the Continental Deep Drilling Programme of the Fed. Rep. of Germany in the Geol. Survey of Lower Saxony, vol. 1, no. 4, pp. 120-129, (ISBN 0080419208)
    Publikationsdatum: 1989
    Schlagwort(e): Borehole geophys. ; Laboratory measurements ; Physical properties of rocks ; Dearth Core ; Rock mechanics ; Physical properties of rocks ; Review article
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    facet.materialart.
    Unbekannt
    Geological Society of London
    In:  Professional Paper, The Initiation, Propagation, and Arrest of Joints and Other Fractures, London, Geological Society of London, vol. 231, no. 16, pp. 117-128, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 2004
    Schlagwort(e): Rock mechanics ; Structural geology ; cracks and fractures (.NE. fracturing) ; Fracture ; Hydraulic fracturing ; Gudmundsson
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    facet.materialart.
    Unbekannt
    Institute of Physics
    In:  Bristol, Institute of Physics, vol. 8, no. Publ. No. 12, pp. 95-104, (ISBN 0-865-42078-5)
    Publikationsdatum: 1986
    Schlagwort(e): Rock mechanics ; Fracture ; Boundary Element Method ; Elasticity ; Dynamic
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    facet.materialart.
    Unbekannt
    Geological Society of London
    In:  Bull., Open-File Rept., The Initiation, Propagation, and Arrest of Joints and Other Fractures, London, Geological Society of London, vol. 231, no. 16, pp. 299-314, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publikationsdatum: 2004
    Schlagwort(e): Rock mechanics ; Structural geology ; cracks and fractures (.NE. fracturing) ; Fracture ; Friction ; Source
    Standort Signatur Erwartet Verfügbarkeit
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