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  • 1
    Book
    Book
    Explosive volcanism in the central mediterranean area during the late quaternary : linking sources and distal archives (2008)
    Amsterdam [u.a.] : Elsevier
    Details
    UID:
    (DE-604)BV035164560
    Format: VII, 299 S. , Ill., graph. Darst., Kt.
    Series Statement: Journal of volcanology and geothermal research 177,1 : special issue
    Note: Einzelaufnahme eines Zeitschr.-H.
    Language: English
    Library Location Call Number Volume/Issue/Year Availability
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    Book
    BVB
  • 2
    Book
    Book
    Explosive volcanism in the central Mediterranean area during the late Quaternary : linking sources and distal archives (2008)
    Amsterdam [u.a.] : Elsevier
    Details
    UID:
    (DE-627)1358056234
    Format: VII, 299 S. , Ill., graph. Darst., Kt.
    Series Statement: Journal of volcanology and geothermal research 177,1
    Language: English
    Library Location Call Number Volume/Issue/Year Availability
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    Book
    BSZ
  • 3
    Online Resource
    Online Resource
    Stress Field Control of Eruption Dynamics (2017)
    [Erscheinungsort nicht ermittelbar] : Frontiers Media SA
    Details
    UID:
    (DE-627)1778561217
    Format: 1 Online-Ressource (131 p.)
    ISBN: 9782889452774
    Series Statement: Frontiers Research Topics
    Content: Increasing evidence supports the claim that stress changes play a fundamental role in triggering volcanic eruptions. Stress changes may vary in origin to include earthquakes, erosion and landslide processes, deglaciation, or tidal effects. The local stress can also change as response of magma influx from deeper reservoirs and an increase of the magma/gas pressure. The stress transfer may be of great importance in reawakening a dormant system. As an example, significant statistical correlation of large earthquakes and eruptions in time and space was suggested in many works. The interaction may be two-fold; where magma intrusions may change the stress at active faults and trigger earthquakes, while tectonic earthquakes may affect the magmatic system and change the eruption activity. The change in local tectonic stress has been claimed as trigger of large ignimbrite eruptions or for controlling the eruptive style of explosive eruptions. Sometimes volcano systems that are nested or closely located may become active in chorus; neighbouring volcanoes may interact in the sense that one volcano triggers its neighbouring volcano. However, although there is ample evidence of concurrence, the processes of interacting volcanoes and near- to far-field tectonic stress are not well understood. Some studies suggest that volcanic eruptions are triggered if compressive stress acts at the magma system and “squeezes” out magma. Other studies suggest that extensional stress fields facilitate magma rise and thus encourage eruptions, or that fluctuating compression and extension during the passing of seismic waves trigger eruptions. This research topic tries to address some of the important open questions in interaction between stress field and volcanic eruption, though both review papers and new contributions
    Note: English
    Language: English
    URL: kostenfrei
    Library Location Call Number Volume/Issue/Year Availability
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    Online Resource
    Stabi Berlin
    UB Potsdam
    BSZ
    GBV
  • 4
    Online Resource
    Online Resource
    Stress Field Control of Eruption Dynamics (2017)
    [Erscheinungsort nicht ermittelbar] : Frontiers Media SA
    Details
    UID:
    (DE-602)gbv_1778561217
    Format: 1 Online-Ressource (131 p.)
    ISBN: 9782889452774
    Series Statement: Frontiers Research Topics
    Content: Increasing evidence supports the claim that stress changes play a fundamental role in triggering volcanic eruptions. Stress changes may vary in origin to include earthquakes, erosion and landslide processes, deglaciation, or tidal effects. The local stress can also change as response of magma influx from deeper reservoirs and an increase of the magma/gas pressure. The stress transfer may be of great importance in reawakening a dormant system. As an example, significant statistical correlation of large earthquakes and eruptions in time and space was suggested in many works. The interaction may be two-fold; where magma intrusions may change the stress at active faults and trigger earthquakes, while tectonic earthquakes may affect the magmatic system and change the eruption activity. The change in local tectonic stress has been claimed as trigger of large ignimbrite eruptions or for controlling the eruptive style of explosive eruptions. Sometimes volcano systems that are nested or closely located may become active in chorus; neighbouring volcanoes may interact in the sense that one volcano triggers its neighbouring volcano. However, although there is ample evidence of concurrence, the processes of interacting volcanoes and near- to far-field tectonic stress are not well understood. Some studies suggest that volcanic eruptions are triggered if compressive stress acts at the magma system and “squeezes” out magma. Other studies suggest that extensional stress fields facilitate magma rise and thus encourage eruptions, or that fluctuating compression and extension during the passing of seismic waves trigger eruptions. This research topic tries to address some of the important open questions in interaction between stress field and volcanic eruption, though both review papers and new contributions
    Note: English
    Language: English
    URL: kostenfrei
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
    Online Resource
    Stabi Berlin
    UB Potsdam
    KOBV
  • 5
    Online Resource
    Online Resource
    Stress Field Control of Eruption Dynamics (2017)
    Frontiers Media SA
    Details
    UID:
    (DE-605)HT020097417
    Format: 1 electronic resource (131 p.)
    ISBN: 9782889452774
    Content: Increasing evidence supports the claim that stress changes play a fundamental role in triggering volcanic eruptions. Stress changes may vary in origin to include earthquakes, erosion and landslide processes, deglaciation, or tidal effects. The local stress can also change as response of magma influx from deeper reservoirs and an increase of the magma/gas pressure. The stress transfer may be of great importance in reawakening a dormant system. As an example, significant statistical correlation of large earthquakes and eruptions in time and space was suggested in many works. The interaction may be two-fold; where magma intrusions may change the stress at active faults and trigger earthquakes, while tectonic earthquakes may affect the magmatic system and change the eruption activity. The change in local tectonic stress has been claimed as trigger of large ignimbrite eruptions or for controlling the eruptive style of explosive eruptions. Sometimes volcano systems that are nested or closely located may become active in chorus; neighbouring volcanoes may interact in the sense that one volcano triggers its neighbouring volcano. However, although there is ample evidence of concurrence, the processes of interacting volcanoes and near- to far-field tectonic stress are not well understood. Some studies suggest that volcanic eruptions are triggered if compressive stress acts at the magma system and "squeezes" out magma. Other studies suggest that extensional stress fields facilitate magma rise and thus encourage eruptions, or that fluctuating compression and extension during the passing of seismic waves trigger eruptions. This research topic tries to address some of the important open questions in interaction between stress field and volcanic eruption, though both review papers and new contributions
    Note: English
    Language: Undetermined
    URL: DOAB: download the publication
    URL: DOAB: description of the publication
    Library Location Call Number Volume/Issue/Year Availability
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    Online Resource
    HBZ
  • 6
    Online Resource
    Online Resource
    Stress Field Control of Eruption Dynamics (2017)
    [Erscheinungsort nicht ermittelbar] : Frontiers Media SA | The Hague : OAPEN FOUNDATION
    Details
    UID:
    (DE-603)490235530
    Format: 1 Online-Ressource (131 p.)
    ISBN: 9782889452774 , 9782889452774
    Content: Increasing evidence supports the claim that stress changes play a fundamental role in triggering volcanic eruptions. Stress changes may vary in origin to include earthquakes, erosion and landslide processes, deglaciation, or tidal effects. The local stress can also change as response of magma influx from deeper reservoirs and an increase of the magma/gas pressure. The stress transfer may be of great importance in reawakening a dormant system. As an example, significant statistical correlation of large earthquakes and eruptions in time and space was suggested in many works. The interaction may be two-fold; where magma intrusions may change the stress at active faults and trigger earthquakes, while tectonic earthquakes may affect the magmatic system and change the eruption activity. The change in local tectonic stress has been claimed as trigger of large ignimbrite eruptions or for controlling the eruptive style of explosive eruptions. Sometimes volcano systems that are nested or closely located may become active in chorus; neighbouring volcanoes may interact in the sense that one volcano triggers its neighbouring volcano. However, although there is ample evidence of concurrence, the processes of interacting volcanoes and near- to far-field tectonic stress are not well understood. Some studies suggest that volcanic eruptions are triggered if compressive stress acts at the magma system and “squeezes” out magma. Other studies suggest that extensional stress fields facilitate magma rise and thus encourage eruptions, or that fluctuating compression and extension during the passing of seismic waves trigger eruptions. This research topic tries to address some of the important open questions in interaction between stress field and volcanic eruption, though both review papers and new contributions.
    Language: English
    URL: kostenfrei
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
    Online Resource
    HeBIS
  • 7
    Online Resource
    Online Resource
    Stress field control of eruption dynamics (2017)
    [Erscheinungsort nicht ermittelbar] : Frontiers Media SA
    Details
    UID:
    (DE-602)b3kat_BV044827220
    Format: 1 Online-Ressource (131 Seiten) , Illustrationen, Diagramme
    ISBN: 9782889452774
    Note: Published in: Frontiers in earth science
    Language: English
    Keywords: Vulkanismus ; Eruption ; Aufsatzsammlung
    DOI: 10.3389/978-2-88945-277-4
    URL: Volltext  (kostenfrei)
    Library Location Call Number Volume/Issue/Year Availability
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    Online Resource
    Fulltext
    EUV Frankfurt
    KOBV
  • 8
    Online Resource
    Online Resource
    Stress field control of eruption dynamics (2017)
    [Erscheinungsort nicht ermittelbar] : Frontiers Media SA
    Details
    UID:
    (DE-604)BV044827220
    Format: 1 Online-Ressource (131 Seiten) , Illustrationen, Diagramme
    ISBN: 9782889452774
    Note: Published in: Frontiers in earth science
    Language: English
    Keywords: Vulkanismus ; Eruption ; Aufsatzsammlung
    DOI: 10.3389/978-2-88945-277-4
    URL: Volltext  (kostenfrei)
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
    Online Resource
    Fulltext
    EUV Frankfurt
    BVB
  • 9
    Online Resource
    Online Resource
    Sedimentology and geochemistry on core Co1204, supplementary data to: Wagner, Bernd; Vogel, Hendrik; Zanchetta, Giovanni; Sulpizio, Roberto (2010): Environmental change within the Balkan region during the past ca. 50 ka recorded in the sediments from lakes Prespa and Ohrid. Biogeochemistry, 7, 3187-3198 (2010)
    Details
    UID:
    (DE-627)660143526
    Format: 3 Datasets , Format: application/zip
    Content: Lakes Prespa and Ohrid, in the Balkan region, are considered to be amongst the oldest lakes in Europe. Both lakes are hydraulically connected via karst aquifers. From Lake Ohrid, several sediment cores up to 15 m long have been studied over the last few years. Here, we document the first long sediment record from nearby Lake Prespa to clarify the influence of Lake Prespa on Lake Ohrid and the environmental history of the region. Radiocarbon dating and dated tephra layers provide robust age control and indicate that the 10.5 m long sediment record from Lake Prespa reaches back to 48 ka. Glacial sedimentation is characterized by low organic matter content and absence of carbonates in the sediments, which indicate oligotrophic conditions in both lakes. Holocene sedimentation is characterized by particularly high carbonate content in Lake Ohrid and by particularly high organic matter content in Lake Prespa, which indicates a shift towards more mesotrophic conditions in the latter. Long-term environmental change and short-term events, such as related to the Heinrich events during the Pleistocene or the 8.2 ka cooling event during the Holocene, are well recorded in both lakes, but are only evident in certain proxies. The comparison of the sediment cores from both lakes indicates that environmental change affects particularly the trophic state of Lake Prespa due to its lower volume and water depth.
    Note: This dataset is supplement to doi:10.5194/bg-7-3187-2010
    Language: English
    Keywords: Datensammlung
    DOI: 10.1594/PANGAEA.758818
    URN: urn:nbn:de:tib-10.1594/PANGAEA.7588187
    URL: Volltext
    URL: Volltext
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    Online Resource
    Online Access
    Open Access Request
    GBV
  • 10
    Online Resource
    Online Resource
    Tephrostratigraphy and major element concentrations in glass shards of sediment core MD90-917, supplementary data to: Siani, Giuseppe; Sulpizio, Roberto; Paterne, Martine; Sbrana, Alessandro (2004): Tephrostratigraphy study for the last 18,000 14C years in a deep-sea sediment sequence for the South Adriatic. Quaternary Science Reviews, 23(23-24), 2485-2500 (2004)
    Details
    UID:
    (DE-627)632978813
    Format: 2 Datasets , Format: application/zip
    Content: A detailed tephrostratigraphy supported by accelerator mass spectrometry (AMS) 14C dating and isotopic and geochemical analyses has been carried out for a deep-sea core collected from the Southern Adriatic Sea, which spans the last 18 14C?kyr. Fourteen ash layers have been recognized in the marine core and the origin was determined by comparing their age and geochemistry with tephra detected in terrestrial deposits. The geochemical signatures of marine ash layers indicate a prevailing Campanian and subordinate Etnean and Eolian provenances. Collectively, they are attributed to sources in the Phlegraean Fields (LAM-Lagno Amendolare; LN1/LN2-GM1; C-2/NYT-Neapolitan Yellow Tuff; C-1-Agnano Pomici Principali; AMS/PF-Agnano Monte Spina; AST-Astroni), Somma-Vesuvius (L9-Pomici di Base; L8-Greenish), Mount Etna (Et1-Y1-Biancavilla Ignimbrite), Lipari (E-1-Gabellotto-Fiumebianco) and Palinuro seamount (Pal 1). Some of these eruptions have been detected for the first time in marine cores (Astroni, LAM, L9, L8), and three were detected and dated by marine tephra (LN1, LN2, and Pal 1) providing new more precise stratigraphic markers for the last 18? kyr in the South Adriatic marine record.
    Note: This dataset is supplement to doi:10.1016/j.quascirev.2004.06.004
    Language: English
    Keywords: Datensammlung
    DOI: 10.1594/PANGAEA.742367
    URN: urn:nbn:de:tib-10.1594/PANGAEA.7423671
    URL: Volltext
    URL: Volltext
    Library Location Call Number Volume/Issue/Year Availability
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    Online Resource
    Online Access
    Open Access Request
    GBV
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