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  • 04. Solid Earth::04.08. Volcanology::04.08.03. Magmas
  • 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks
  • 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions
  • Tsunami
  • Nature Publishing Group  (4)
  • Springer Berlin / Heidelberg  (4)
  • Bogotá D.C., Colombia  (3)
  • American Institute of Physics (AIP)
  • Springer Science + Business Media
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  • 1
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    Unknown
    Ed. Dimar | Bogotá D.C., Colombia
    Publication Date: 2023-12-28
    Description: Publicación de tipo educativo, dirigida al público infantil, para colorear. Editada en idioma español. Es una publicación de acceso abierto (Open Access, OA) para su consulta, sus condiciones de uso y distribución están definidas por el licenciamiento Creative Commons (CC).
    Description: Published
    Description: Non Refereed
    Keywords: Tsunami ; Sismo ; Amenaza natural ; ASFA_2015::E::Education ; ASFA_2015::T::Tsunamis ; ASFA_2015::H::Hazards
    Repository Name: AquaDocs
    Type: Book/Monograph/Conference Proceedings
    Format: 16pp.
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  • 2
    Publication Date: 2023-03-09
    Description: Contenido - Editorial - Buque de investigación científica marina ARC “Simón Bolívar”: aporte al desarrollo de la nación - El catastro marino: una herramienta para mejorar la administración y la gobernanza de los litorales colombianos - Protección del medio marino, rol de la Autoridad Marítima - Gestión del riesgo por tsunami y pérdida de contención de hidrocarburos y sustancias peligrosas asociado a actividades marítimas - Salvaguardando la vida humana en el mar. Dimar: una autoridad que trabaja 24x7 (SAR y tsunami) - Transformación tecnológica de la señalización marítima - Buques autónomos de superficie (MASS) un avance global y sus riesgos - Dimar 70 Años: su evolución histórica - Directores Marítimos - Buques de superficie, una parte de la historia de los 70 años de la Dirección General Marítima - Fortalecimiento de la Infraestructura de Datos Espaciales Marítima y Costera: datos abiertos para la toma de decisiones informadas - Alistamiento para la auditoría de la Organización Marítima Internacional 2024 - Dirección General Marítima certificada como un “Gran Lugar para Trabajar” - Harry Fernando Quiñones Torres. Veintiocho años trabajando por la investigación científica marina desde la ‘Perla del Pacífico’ - Cocinando en altamar - #LéxicoDelMar
    Description: Published
    Description: Non Refereed
    Keywords: Puertos ; Señalización marítima ; Seguridad del transporte ; Hidrocarburos ; Tsunami ; Buque ; ASFA_2015::V::Vessels ; ASFA_2015::T::Tsunamis ; ASFA_2015::C::Coastal planning ; ASFA_2015::S::Safety ; ASFA_2015::R::Risk management ; ASFA_2015::M::Marine meteorology
    Repository Name: AquaDocs
    Type: Book/Monograph/Conference Proceedings
    Format: 101pp.
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  • 3
    Publication Date: 2021-08-03
    Description: En el año 2002, el entonces Centro de Control de Contaminación del Pacífico (CCCP) publicó el libro titulado COMPILACIÓN OCEANOGRÁFICA DE LA CUENCA PACÍFICA COLOMBIANA, lo que sería un referente bibliográfico de vital importancia para la caracterización de las zonas marino-costeras del Pacífico colombiano, abarcando un total de cinco capítulos en temas tan variados como las particularidades geográficas de la Cuenca Pacífica Colombiana (CPC) y su investigación oceanográfica, la búsqueda de la relación entre las condiciones oceanográficas de la Cuenca y el ciclo de El Niño Oscilación del Sur (ENOS), además del plan científico del grupo de investigación en oceanografía para el periodo 2001-2010. Han transcurrido 18 largos años desde entonces, y la comunidad científica marina del país, así como la Autoridad Marítima colombiana y el gremio marítimo requieren no solo una actualización de dichas líneas de investigación, sino también mayor cantidad y mejor nivel de detalle en la información disponible para la toma de decisiones con base en el rigor técnico; así como el claro y amplio soporte de conocimiento del medio en el que se desenvuelven para el diario devenir en sus actividades en el mar y en la costa, teniendo en cuenta que las aguas del gran Pacífico no representan la frontera que separa, sino el puente que une a Colombia y los países de Oceanía y del sudeste asiático, considerada como la zona con los mercados de mayor proyección del mundo. Esta es una más de las principales razones, sumada a las necesidades de desarrollo y las aspiraciones nacionales de consolidar factores de seguridad multidimensional y de presencia estatal en las áreas de frontera, para aprovechar las múltiples potencialidades que ofrece el vasto océano Pacífico para una nación en desarrollo, y con la aspiración nacional de llegar a ser una potencia media regional influyente como lo es Colombia. Por lo anterior, el mismo CCCP, ahora denominado Centro de Investigaciones Oceanográficas e Hidrográficas del Pacífico, presenta con orgullo el resultado de un esfuerzo por satisfacer estos requerimientos a través de la publicación del título COMPILACIÓN OCEANOGRÁFICA DEL PACÍFICO COLOMBIANO II, el cual consta de siete capítulos que garantizan la continuidad en los anteriores temas y proporciona algunos nuevos, complementando y ampliando la información ofrecida por la primera edición. Dentro de estas líneas de investigación fueron incluidas las particularidades geográficas y geomorfología de la CPC, su meteorología, la investigación oceanográfica en la Cuenca e influencia de los eventos ENOS, las condiciones de oleaje en el Pacífico colombiano, la variabilidad del nivel del mar, la amenaza por tsunami en la CPC y, finalmente, las tendencias en la biogeoquímica del océano Pacífico Oriental Tropical y Sureste bajo diferentes escenarios de cambio climático. Bienvenidos entonces a una ventana más del conocimiento sobre nuestra Cuenca Pacífica Colombiana, desde donde contribuimos a la “consolidación de Colombia como país marítimo” y aportamos nuestro pequeño pero representativo grano de arena a la defensa del enorme, hermoso e imponente azul de la bandera. El reconocimiento de los espacios marítimos para el desarrollo de un país es de vital importancia. Desde su exploración oceánica y costera, la hidrografía ha representado el conocimiento científico sobre el territorio marítimo colombiano y ha brindado información, instrumentos y herramientas para una mejor compresión y desarrollo de las actividades marítimas en el país. La producción de la cartografía náutica para asegurar las rutas marítimas y el comercio internacional de la nación es un aspecto fundamental, que a su vez ha cumplido un papel importante en el reconocimiento de las profundidades y el descubrimiento de riquezas económicas y culturales en los fondos oceánicos, además de aportar seguridad en la navegación por el espacio marítimo colombiano y un mejor conocimiento de nuestros litorales y sus potencialidades. La hidrografía entonces ha desempeñado eficientemente el rol de fortalecer y desarrollar las riquezas que se encuentran en nuestras aguas jurisdiccionales, y ha sido la disciplina científica que ha aportado al reconocimiento de los territorios costeros y oceánicos, y, consecutivamente, al avance en el desarrollo de la infraestructura marítima para el país. Objetivos que podemos hallar desde sus comienzos y que fueron evidenciados y visibilizados a lo largo de su labor y trabajo en los espacios y frentes marinos, que le han permitido a la Autoridad Marítima Colombiana, a través de un interés nacional y una visión internacional, mantener una navegación segura que haga parte del impulso y progreso económico y nacional, en contribución paralela a los objetivos de desarrollo sostenible de la Organización de las Naciones Unidas.
    Description: Published
    Description: Not Known
    Keywords: Meteorología ; Tsunami ; Oceanografía física ; Biogeoquímica ; Climatología ; Oceanografía Química ; Inundación ; Cambio climático ; Biología ; ASFA_2015::M::Marine biology ; ASFA_2015::P::Physical oceanography ; ASFA_2015::C::Chemical oceanography ; ASFA_2015::M::Marine meteorology ; ASFA_2015::T::Tsunamis ; ASFA_2015::C::Climatology
    Repository Name: AquaDocs
    Type: Book/Monograph/Conference Proceedings
    Format: 231pp
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  • 4
    Publication Date: 2017-04-04
    Description: In this paper, we describe the 1809 eruption of Mt. Etna, Italy, which represents one historical rare case in which it is possible to observe details of the internal structure of the feeder system. This is possible thanks to the presence of two large pit craters located in the middle of the eruptive fracture field that allow studying a section of the shallow feeder system. Along the walls of one of these craters, we analysed well-exposed cross sections of the uppermost 15–20 m of the feeder system and related volcanic products. Here, we describe the structure, morphology and lithology of this portion of the 1809 feeder system, including the host rock which conditioned the propagation of the dyke, and compare the results with other recent eruptions. Finally, we propose the dynamic model of the magma behaviour inside a laterally-propagating feeder dyke, demonstrating how this dynamic triggered important changes in the eruptive style (from effusive/Strombolian to phreatomagmatic) during the same eruption. Our results are also useful for hazard assessment related to the development of flank eruptions, potentially the most hazardous type of eruption from basaltic volcanoes in densely urbanized areas, such as Mt. Etna.
    Description: Published
    Description: 1-11
    Description: 2T. Tettonica attiva
    Description: 2V. Dinamiche di unrest e scenari pre-eruttivi
    Description: 3V. Dinamiche e scenari eruttivi
    Description: 4V. Vulcani e ambiente
    Description: 6A. Monitoraggio ambientale, sicurezza e territorio
    Description: N/A or not JCR
    Description: open
    Keywords: feeder dyke ; basaltic volcanoes ; flank eruptions ; Etna ; volcanic hazards ; sill ; volcanic rift ; 04. Solid Earth::04.04. Geology::04.04.09. Structural geology ; 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::04.08.04. Thermodynamics ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks ; 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)
    Type: article
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  • 5
    Publication Date: 2017-04-04
    Description: The 2011 Tohoku-oki (Mw 9.1) earthquake is so far the best-observed megathrust rupture, which allowed the collection of unprecedented offshore data. The joint inversion of tsunami waveforms (DART buoys, bottom pressure sensors, coastal wave gauges, and GPS-buoys) and static geodetic data (onshore GPS, seafloor displacements obtained by a GPS/acoustic combination technique), allows us to retrieve the slip distribution on a non-planar fault. We show that the inclusion of near-source data is necessary to image the details of slip pattern (maximum slip ,48 m, up to ,35 m close to the Japan trench), which generated the large and shallow seafloor coseismic deformations and the devastating inundation of the Japanese coast. We investigate the relation between the spatial distribution of previously inferred interseismic coupling and coseismic slip and we highlight the importance of seafloor geodetic measurements to constrain the interseismic coupling, which is one of the key-elements for long-term earthquake and tsunami hazard assessment.
    Description: Published
    Description: 385
    Description: 3.1. Fisica dei terremoti
    Description: N/A or not JCR
    Description: restricted
    Keywords: Tohoku ; Subduction ; Tsunami ; Inverse problem ; 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics ; 04. Solid Earth::04.07. Tectonophysics::04.07.06. Subduction related processes
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2017-04-04
    Description: In recent decades, geophysical investigations have detected wide magma reservoirs beneath quiescent calderas. However, the discovery of partially melted horizons inside the crust is not sufficient to put constraints on capability of reservoirs to supply cataclysmic eruptions, which strictly depends on the chemical-physical properties of magmas (composition, viscosity, gas content etc.), and thus on their differentiation histories. In this study, by using geochemical, isotopic and textural records of rocks erupted from the high-risk Campi Flegrei caldera, we show that the alkaline magmas have evolved toward a critical state of explosive behaviour over a time span shorter than the repose time of most volcanic systems and that these magmas have risen rapidly toward the surface. Moreover, similar results on the depth and timescale of magma storage were previously obtained for the neighbouring Somma-Vesuvius volcano. This consistency suggests that there might be a unique long-lived magma pool beneath the whole Neapolitan area.
    Description: Published
    Description: article 712
    Description: 2.3. TTC - Laboratori di chimica e fisica delle rocce
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: 3.6. Fisica del vulcanismo
    Description: 4.3. TTC - Scenari di pericolosità vulcanica
    Description: N/A or not JCR
    Description: open
    Keywords: magma ; campi flegrei caldera ; 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology ; 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::04.08.08. Volcanic risk
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
    Publication Date: 2017-04-04
    Description: The MW 8.8 mega-thrust earthquake and tsunami that occurred on February 27, 2010, offshore Maule region, Chile, was not unexpected. A clearly identified seismic gap existed in an area where tectonic loading has been accumulating since the great 1835 earthquake experienced and described by Darwin during the voyage of the Beagle. Here we jointly invert tsunami and geodetic data (InSAR, GPS, land-level changes), to derive a robust model for the co-seismic slip distribution and induced co-seismic stress changes, and compare them to past earthquakes and the pre-seismic locking distribution. We aim to assess if the Maule earthquake has filled the Darwin gap, decreasing the probability of a future shock . We find that the main slip patch is located to the north of the gap, overlapping the rupture zone of the MW 8.0 1928 earthquake, and that a secondary concentration of slip occurred to the south; the Darwin gap was only partially filled and a zone of high pre-seismic locking remains unbroken. This observation is not consistent with the assumption that distributions of seismic rupture might be correlated with pre-seismic locking, potentially allowing the anticipation of slip distributions in seismic gaps. Moreover, increased stress on this unbroken patch might have increased the probability of another major to great earthquake there in the near future.
    Description: Published
    Description: 173-177
    Description: 3.1. Fisica dei terremoti
    Description: 4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionale
    Description: JCR Journal
    Description: restricted
    Keywords: Source process ; Chile ; Tsunami ; Joint Inversion ; Seismic Gap ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous ; 04. Solid Earth::04.07. Tectonophysics::04.07.05. Stress ; 04. Solid Earth::04.07. Tectonophysics::04.07.06. Subduction related processes ; 05. General::05.01. Computational geophysics::05.01.03. Inverse methods
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2017-04-04
    Description: We use a kinematic GPS and laser range finder survey of a 200 m-long section of the Muliwai a Pele lava channel (Mauna Ulu, Kilauea) to examine the construction processes and flow dynamics responsible for the channel–levee structure. The levees comprise three packages. The basal package comprises an 80–150 m wide ′a′a flow in which a ∼2 m deep and ∼11 m wide channel became centred. This is capped by a second package of thin (〈45 cm thick) sheets of pahoehoe extending no more than 50 m from the channel. The upper-most package comprises localised ′a′a overflows. The channel itself contains two blockages located 130 m apart and composed of levee chunks veneered with overflow lava. The channel was emplaced over 50 h, spanning 30 May–2 June, 1974, with the flow front arriving at our section (4.4 km from the vent) 8 h after the eruption began. The basal ′a′a flow thickness yields effusion rates of 35 m3 s−1 for the opening phase, with the initial flow advancing across the mapped section at ∼10 m/min. Short-lived overflows of fluid pahoehoe then built the levee cap, increasing the apparent channel depth to 4.8 m. There were at least six pulses at 90–420 m3 s−1, causing overflow of limited extent lasting no more than 5 min. Brim-full flow conditions were thus extremely short-lived. During a dominant period of below-bank flow, flow depth was ∼2 m with an effusion rate of ∼35 m3 s−1, consistent with the mean output rate (obtained from the total flow bulk volume) of 23–54 m3 s−1. During pulses, levee chunks were plucked and floated down channel to form blockages. In a final low effusion rate phase, lava ponded behind the lower blockage to form a syn-channel pond that fed ′a′a overflow. After the end of the eruption the roofed-over pond continued to drain through the lower blockage, causing the roof to founder. Drainage emplaced inflated flows on the channel floor below the lower blockage for a further ∼10 h. The complex processes involved in levee–channel construction of this short-lived case show that care must be taken when using channel dimensions to infer flow dynamics. In our case, the full channel depth is not exposed. Instead the channel floor morphology reflects late stage pond filling and drainage rather than true channel-contained flow. Components of the compound levee relate to different flow regimes operating at different times during the eruption and associated with different effusion rates, flow dynamics and time scales. For example, although high effusion rate, brim-full flow was maintained for a small fraction of the channel lifetime, it emplaced a pile of pahoehoe overflow units that account for 60% of the total levee height. We show how time-varying volume flux is an important parameter in controlling channel construction dynamics. Because the complex history of lava delivery to a channel system is recorded by the final channel morphology, time-varying flow dynamics can be determined from the channel morphology. Developing methods for quantifying detailed flux histories for effusive events from the evidence in outcrop is therefore highly valuable. We here achieve this by using high-resolution spatial data for a channel system at Kilauea. This study not only indicates those physical and dynamic characteristics that are typical for basaltic lava flows on Hawaiian volcanoes, but also a methodology that can be widely applied to effusive basaltic eruptions.
    Description: Published
    Description: 459-474
    Description: 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
    Description: 1.10. TTC - Telerilevamento
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: JCR Journal
    Description: reserved
    Keywords: Lava channel ; Levees ; Effusion rates ; Flow dynamics ; 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks ; 04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2017-04-04
    Description: On 28 December 2002, new vents opened on the flanks of Stromboli, just below the summit craters, interrupting the persistent activity of the volcano with a 7-month-long effusive eruption. We here report on the plagioclase size distribution (PlgSD) in lava samples collected following the chronology of the 2002–2003 eruption. Data reveal a linear PlgSD similar to that found in samples of normal Stromboli activity, indicating that the switch from Strombolian explosive to effusive activity is not associated with changes in texture. Nevertheless, the crystal size distribution slopes and intercepts exhibit slight sinusoidal temporal variations that are here ascribed to a magma supply mechanism able to induce “resonance” in the crystal size distribution, with an amplitude that depends on the supply rate.
    Description: Published
    Description: 631-641
    Description: 2.3. TTC - Laboratori di chimica e fisica delle rocce
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: JCR Journal
    Description: reserved
    Keywords: Plagioclase ; Crystal size distribution ; Stromboli ; 2002–2003 eruption ; Magma supply rate ; Effusive activity ; Crystallization ; 04. Solid Earth::04.04. Geology::04.04.11. Instruments and techniques ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks ; 04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 10
    Publication Date: 2017-04-04
    Description: During its 1800-year-long persistent activity the Stromboli volcano has erupted a highly porphyritic (HP) volatile-poor scoriaceous magma and a low porphyritic (LP) volatile-rich pumiceous magma. The HP magma is erupted during normal Strombolian explosions and lava effusions, while the LP one is related to more energetic paroxysms. During the March–April 2003 explosive activity, Stromboli ejected two typologies of juvenile glassy ashes, namely highly vesicular LP shards and volatile-poor HP shards. Their textural and in situ chemical characteristics are used to unravel mutual relationships between HP and LP magmas, as well as magma dynamics within the shallow plumbing system. The mantle-normalized trace element patterns of both ash types show the typical arc-lava pattern; however, HP glasses possess incompatible element concentrations higher than LP glasses, along with Sr and Eu negative anomalies. HP shards are generally characterized by higher Li contents (to ~20 ppm) and lower δ7Li values (+1.2 to −3.8‰) with respect to LP shards (Li contents of 7–14 ppm and δ7Li ranging between +4.6 and +0.9‰). Fractional crystallization models based on major and trace element compositions, combined with a degassing model based on open-system Rayleigh distillation and on the assumption that melt/fluidDLi 〉 1, show that abundant (~30%) plagioclase precipitation and variable degrees of degassing can lead the more primitive LP magma to evolve toward a differentiated (isotopically lighter) HP magma ponding in the upper conduit and undergoing slow continuous degassing-induced crystallization. This study also evidences that in March 2003 Stromboli volcano poured out a small early volume of LP magma that traveled slower within the conduit with respect to later and larger volumes of fast ascending LP magma erupted during the April 5 paroxysm. The different ascent rates and cooling rates of the two LP magma batches (i.e., pre- and post-paroxysm) resulted in small, but detectable, differences in their chemical signatures. Finally, this study highlights the high potential of in situ investigations of juvenile glassy ashes in petrologic and geochemical monitoring the volcanic activity and of Li isotopes as tracers of degassing processes within the shallow plumbing system.
    Description: In press
    Description: 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
    Description: 2.3. TTC - Laboratori di chimica e fisica delle rocce
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: JCR Journal
    Description: reserved
    Keywords: Stromboli ; Volcanic ash ; Lithium isotopes ; Degassing ; induced crystallization ; Petrologic monitoring ; 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology ; 04. Solid Earth::04.04. Geology::04.04.07. Rock geochemistry ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 11
    Publication Date: 2017-04-04
    Description: Dikes within stratovolcanoes are commonly expected to have radial patterns. However, other patterns may also be also found, due to regional stresses, magmatic reservoirs, topographic variations. Here we investigate dike patterns within volcanic edifices, by studying dike and fissure complexes at Somma-Vesuvius and Etna (Italy) and using analogue models. At the surface, the dikes and fissures show a radial configuration. At depths of tens to several hundreds of m, in areas exposed by erosion, tangential and oblique dikes are also present. Analogue models indicate that dikes approaching the flanks of cones, regardless of their initial orientation, reorient to become radial (parallel to the maximum gravitational stress). This reorientation is a significant process in shallow magma migration and may also control the emplacement of dike-fed fissures reaching the lower slopes of the volcano.
    Description: In press
    Description: 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
    Description: 3.2. Tettonica attiva
    Description: 3.5. Geologia e storia dei sistemi vulcanici
    Description: 3.6. Fisica del vulcanismo
    Description: 4.3. TTC - Scenari di pericolosità vulcanica
    Description: JCR Journal
    Description: open
    Keywords: dike ; Etna ; Somma-Vesuvius ; analogue models ; 04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processes ; 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::04.07.07. 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::04.08.04. Thermodynamics ; 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)
    Type: article
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