Sector collapse, sedimentation and clast population evolution at an active island-arc volcano: Stromboli, Italy View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1995-08

AUTHORS

P. Kokelaar, C. Romagnoli

ABSTRACT

Sciara del Fuoco is the subaerial part of a partially filled sector-collapse scar that extends to 700 m below sea level on Stromboli volcano. The collapse occurred <5000 years ago, involved ≤1.81 km3 of rock and is the latest of a series of major collapses on the north-west flank of Stromboli. A north-east trending arc-axial fault system channels magmas into the volcano and has caused tilting and/or downthrow to the north-west. The slope of the partial cone constructed between the lateral walls of the collapse scar acts as a channelway to the sea for most eruptive products. From 700 m below sea level and extending to >2200 m and >10 km from the shore to the NNW, a fan-shaped mounded feature comprises debris avalanche deposits (>4 km3) from two or more sector collapses. Volcaniclastic density currents originating from Sciara del Fuoco follow the topographic margin of the debris avalanche deposits, although overbank currents and other unconfined currents widely cover the mounded feature with turbidites. Historical (recorded) eruptive activity in Sciara del Fuoco is considerably less than that which occurred earlier, and much of the partial fill may have formed from eruptions soon after the sector collapse. It is possible that a mass of eruptive products similar to that in the collapse scar is dispersed as volcanogenic sediment in deep water of the Tyrhennian basin. Evidence that the early post-collapse eruptive discharge was greater than the apparent recent flux (≈2kg/s) counters suggestions that a substantial part of Stromboli's growth has been endogenous. The partial fill of Sciaria del Fuoco is dominated by lava and spatter layers, rather than by the scoria and ash layers classically regarded as main constituents of Strombolian (‘cinder’) cones. Much of the volcanic slope beneath the vents is steeper than the angle of repose of loose tephra, which is therefore rapidly transported to the sea. Delicate pyroclasts that record the magmatic explosivity are selectively destroyed and diluted during sedimentary transport, mainly in avalanches and by shoreline wave reworking, and thus the submarine deposits do not record well the extent and diversity of explosive activity and associated clast-forming processes. Considerable amounts of dense (non-vesicular) fine sand and silt grains are produced by breakage and rounding of fragments of lava and agglutinate. The submarine extension of the collapse scar, and the continuing topographic depression to >2200 m below sea level, are zones of considerable by-passing of fine sand and silt, which are transported in turbidity currents. Evidently, volcanogenic sediments dispersed around island volcanoes by density currents are unlikely to record well the true spectrum and relative importance of clast-forming processes that occurred during an eruption. Marine sedimentary evidence of magmatic explosivity is particularly susceptible to partial or complete obliteration, unless there is a high rate of discharge of pyroclastic material into the sea. More... »

PAGES

240-262

References to SciGraph publications

  • 1996. Quantitative Reconstruction of Recent Volcanic Activity: A Contribution to Forecasting of Future Eruptions in MONITORING AND MITIGATION OF VOLCANO HAZARDS
  • 1986-10. Magma-water interactions in subaqueous and emergent basaltic in BULLETIN OF VOLCANOLOGY
  • 1989-07. Volcanological and magmatological evolution of Stromboli volcano (Aeolian Islands): The roles of fractional crystallization, magma mixing, crustal contamination and source heterogeneity in BULLETIN OF VOLCANOLOGY
  • 1994-03. Sulphur output and magma degassing budget of Stromboli volcano in NATURE
  • 1993-12. Endogenous growth of persistently active volcanoes in NATURE
  • 1987-10. Large-scale volcanic cone collapse: The 1888 slope failure of Ritter volcano, and other examples from Papua New Guinea in BULLETIN OF VOLCANOLOGY
  • 1992-09. Steady-state operation of Stromboli volcano, Italy: constraints on the feeding system in BULLETIN OF VOLCANOLOGY
  • 1987-02. Volcanic hazards from Bezymianny- and Bandai-type eruptions in BULLETIN OF VOLCANOLOGY
  • 1987-04. High velocity debris avalanche at Lastarria volcano in the north Chilean Andes in BULLETIN OF VOLCANOLOGY
  • 1989-09. A vesicularity index for pyroclastic deposits in BULLETIN OF VOLCANOLOGY
  • 1989-03. A geomorphological reconnaissance of the submarine part of the East Rift Zone of Kilauea Volcano, Hawaii in BULLETIN OF VOLCANOLOGY
  • 1988-07. Landsat Thematic Mapper observations of debris avalanche deposits in the Central Andes in BULLETIN OF VOLCANOLOGY
  • 1978-09. Stromboli and its 1975 eruption in BULLETIN VOLCANOLOGIQUE
  • 1988-12. The transition from calc-alkaline to potassic orogenic magmatism in the Aeolian Islands, Southern Italy in BULLETIN OF VOLCANOLOGY
  • Journal

    TITLE

    Bulletin of Volcanology

    ISSUE

    4

    VOLUME

    57

    Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1007/bf00265424

    DOI

    http://dx.doi.org/10.1007/bf00265424

    DIMENSIONS

    https://app.dimensions.ai/details/publication/pub.1024824153


    Indexing Status Check whether this publication has been indexed by Scopus and Web Of Science using the SN Indexing Status Tool
    Incoming Citations Browse incoming citations for this publication using opencitations.net

    JSON-LD is the canonical representation for SciGraph data.

    TIP: You can open this SciGraph record using an external JSON-LD service: JSON-LD Playground Google SDTT

    [
      {
        "@context": "https://springernature.github.io/scigraph/jsonld/sgcontext.json", 
        "about": [
          {
            "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/0403", 
            "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
            "name": "Geology", 
            "type": "DefinedTerm"
          }, 
          {
            "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/04", 
            "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
            "name": "Earth Sciences", 
            "type": "DefinedTerm"
          }
        ], 
        "author": [
          {
            "affiliation": {
              "alternateName": "University of Liverpool", 
              "id": "https://www.grid.ac/institutes/grid.10025.36", 
              "name": [
                "Earth Sciences Department, University of Liverpool, L69 3BX, Liverpool, UK"
              ], 
              "type": "Organization"
            }, 
            "familyName": "Kokelaar", 
            "givenName": "P.", 
            "id": "sg:person.01160134750.42", 
            "sameAs": [
              "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.01160134750.42"
            ], 
            "type": "Person"
          }, 
          {
            "affiliation": {
              "alternateName": "University of Bologna", 
              "id": "https://www.grid.ac/institutes/grid.6292.f", 
              "name": [
                "Departimento di Scienze Mineralogiche, Universit\u00e0 di Bologna, 40126, Bologna, Italy"
              ], 
              "type": "Organization"
            }, 
            "familyName": "Romagnoli", 
            "givenName": "C.", 
            "id": "sg:person.07663171313.28", 
            "sameAs": [
              "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.07663171313.28"
            ], 
            "type": "Person"
          }
        ], 
        "citation": [
          {
            "id": "sg:pub.10.1038/368326a0", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1002591528", 
              "https://doi.org/10.1038/368326a0"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf02597227", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1004212689", 
              "https://doi.org/10.1007/bf02597227"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf02597227", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1004212689", 
              "https://doi.org/10.1007/bf02597227"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0040-1951(82)90163-9", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1008972534"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0040-1951(82)90163-9", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1008972534"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1144/gsjgs.132.4.0429", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1015791273"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(84)90002-7", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1016476042"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(84)90002-7", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1016476042"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00569938", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1016642754", 
              "https://doi.org/10.1007/bf00569938"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0168-9622(86)90072-2", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1017157488"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/978-3-642-80087-0_19", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1017357856", 
              "https://doi.org/10.1007/978-3-642-80087-0_19"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01078811", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1017939651", 
              "https://doi.org/10.1007/bf01078811"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01078811", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1017939651", 
              "https://doi.org/10.1007/bf01078811"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0012-821x(85)90021-4", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1022675570"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0012-821x(85)90021-4", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1022675570"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1002/9781444303858.ch3", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1023805130"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1029/jb087ib05p04035", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1024482943"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01080358", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1025123668", 
              "https://doi.org/10.1007/bf01080358"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01080358", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1025123668", 
              "https://doi.org/10.1007/bf01080358"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01050638", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1026850566", 
              "https://doi.org/10.1007/bf01050638"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.3406/bagf.1982.5347", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1027008206"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0025-3227(90)90011-8", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1028140023"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0025-3227(90)90011-8", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1028140023"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01056897", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1028157096", 
              "https://doi.org/10.1007/bf01056897"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01081981", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1030465754", 
              "https://doi.org/10.1007/bf01081981"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01081981", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1030465754", 
              "https://doi.org/10.1007/bf01081981"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01245476", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1033033221", 
              "https://doi.org/10.1007/bf01245476"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1111/j.1365-246x.1987.tb01661.x", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1033642517"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(82)90009-9", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1033760811"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(82)90009-9", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1033760811"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(94)90053-1", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1034720039"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(94)90053-1", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1034720039"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01046635", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1036491679", 
              "https://doi.org/10.1007/bf01046635"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1130/0016-7606(1992)104<1433:omvasr>2.3.co;2", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1036916614"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(83)90061-6", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1037182164"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(83)90061-6", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1037182164"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1038/366554a0", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1037301642", 
              "https://doi.org/10.1038/366554a0"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(90)90054-j", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1037690583"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(90)90054-j", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1037690583"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1029/jb078i023p05221", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1039273424"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01081756", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1041163103", 
              "https://doi.org/10.1007/bf01081756"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01081756", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1041163103", 
              "https://doi.org/10.1007/bf01081756"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(89)90003-6", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1041446227"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(94)90052-3", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1042117455"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(94)90052-3", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1042117455"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1029/jb094ib12p17465", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1046802632"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(83)90006-9", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1048165048"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(83)90006-9", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1048165048"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1098/rspa.1972.0115", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1048356459"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0040-1951(72)90086-8", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1050823166"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0040-1951(72)90086-8", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1050823166"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0012-821x(74)90161-7", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1052553778"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0012-821x(74)90161-7", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1052553778"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(81)90054-8", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1053128692"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0377-0273(81)90054-8", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1053128692"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01047488", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1053738817", 
              "https://doi.org/10.1007/bf01047488"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1126/science.236.4807.1442", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1062534268"
            ], 
            "type": "CreativeWork"
          }
        ], 
        "datePublished": "1995-08", 
        "datePublishedReg": "1995-08-01", 
        "description": "Sciara del Fuoco is the subaerial part of a partially filled sector-collapse scar that extends to 700 m below sea level on Stromboli volcano. The collapse occurred <5000 years ago, involved \u22641.81 km3 of rock and is the latest of a series of major collapses on the north-west flank of Stromboli. A north-east trending arc-axial fault system channels magmas into the volcano and has caused tilting and/or downthrow to the north-west. The slope of the partial cone constructed between the lateral walls of the collapse scar acts as a channelway to the sea for most eruptive products. From 700 m below sea level and extending to >2200 m and >10 km from the shore to the NNW, a fan-shaped mounded feature comprises debris avalanche deposits (>4 km3) from two or more sector collapses. Volcaniclastic density currents originating from Sciara del Fuoco follow the topographic margin of the debris avalanche deposits, although overbank currents and other unconfined currents widely cover the mounded feature with turbidites. Historical (recorded) eruptive activity in Sciara del Fuoco is considerably less than that which occurred earlier, and much of the partial fill may have formed from eruptions soon after the sector collapse. It is possible that a mass of eruptive products similar to that in the collapse scar is dispersed as volcanogenic sediment in deep water of the Tyrhennian basin. Evidence that the early post-collapse eruptive discharge was greater than the apparent recent flux (\u22482kg/s) counters suggestions that a substantial part of Stromboli's growth has been endogenous. The partial fill of Sciaria del Fuoco is dominated by lava and spatter layers, rather than by the scoria and ash layers classically regarded as main constituents of Strombolian (\u2018cinder\u2019) cones. Much of the volcanic slope beneath the vents is steeper than the angle of repose of loose tephra, which is therefore rapidly transported to the sea. Delicate pyroclasts that record the magmatic explosivity are selectively destroyed and diluted during sedimentary transport, mainly in avalanches and by shoreline wave reworking, and thus the submarine deposits do not record well the extent and diversity of explosive activity and associated clast-forming processes. Considerable amounts of dense (non-vesicular) fine sand and silt grains are produced by breakage and rounding of fragments of lava and agglutinate. The submarine extension of the collapse scar, and the continuing topographic depression to >2200 m below sea level, are zones of considerable by-passing of fine sand and silt, which are transported in turbidity currents. Evidently, volcanogenic sediments dispersed around island volcanoes by density currents are unlikely to record well the true spectrum and relative importance of clast-forming processes that occurred during an eruption. Marine sedimentary evidence of magmatic explosivity is particularly susceptible to partial or complete obliteration, unless there is a high rate of discharge of pyroclastic material into the sea.", 
        "genre": "research_article", 
        "id": "sg:pub.10.1007/bf00265424", 
        "inLanguage": [
          "en"
        ], 
        "isAccessibleForFree": false, 
        "isPartOf": [
          {
            "id": "sg:journal.1051922", 
            "issn": [
              "0258-8900", 
              "1432-0819"
            ], 
            "name": "Bulletin of Volcanology", 
            "type": "Periodical"
          }, 
          {
            "issueNumber": "4", 
            "type": "PublicationIssue"
          }, 
          {
            "type": "PublicationVolume", 
            "volumeNumber": "57"
          }
        ], 
        "name": "Sector collapse, sedimentation and clast population evolution at an active island-arc volcano: Stromboli, Italy", 
        "pagination": "240-262", 
        "productId": [
          {
            "name": "readcube_id", 
            "type": "PropertyValue", 
            "value": [
              "764368368dae39055eb099cf33226122325e19056dfb03242434fce99654409f"
            ]
          }, 
          {
            "name": "doi", 
            "type": "PropertyValue", 
            "value": [
              "10.1007/bf00265424"
            ]
          }, 
          {
            "name": "dimensions_id", 
            "type": "PropertyValue", 
            "value": [
              "pub.1024824153"
            ]
          }
        ], 
        "sameAs": [
          "https://doi.org/10.1007/bf00265424", 
          "https://app.dimensions.ai/details/publication/pub.1024824153"
        ], 
        "sdDataset": "articles", 
        "sdDatePublished": "2019-04-11T13:47", 
        "sdLicense": "https://scigraph.springernature.com/explorer/license/", 
        "sdPublisher": {
          "name": "Springer Nature - SN SciGraph project", 
          "type": "Organization"
        }, 
        "sdSource": "s3://com-uberresearch-data-dimensions-target-20181106-alternative/cleanup/v134/2549eaecd7973599484d7c17b260dba0a4ecb94b/merge/v9/a6c9fde33151104705d4d7ff012ea9563521a3ce/jats-lookup/v90/0000000371_0000000371/records_130792_00000002.jsonl", 
        "type": "ScholarlyArticle", 
        "url": "http://link.springer.com/10.1007/BF00265424"
      }
    ]
     

    Download the RDF metadata as:  json-ld nt turtle xml License info

    HOW TO GET THIS DATA PROGRAMMATICALLY:

    JSON-LD is a popular format for linked data which is fully compatible with JSON.

    curl -H 'Accept: application/ld+json' 'https://scigraph.springernature.com/pub.10.1007/bf00265424'

    N-Triples is a line-based linked data format ideal for batch operations.

    curl -H 'Accept: application/n-triples' 'https://scigraph.springernature.com/pub.10.1007/bf00265424'

    Turtle is a human-readable linked data format.

    curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/bf00265424'

    RDF/XML is a standard XML format for linked data.

    curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/bf00265424'


     

    This table displays all metadata directly associated to this object as RDF triples.

    202 TRIPLES      21 PREDICATES      66 URIs      19 LITERALS      7 BLANK NODES

    Subject Predicate Object
    1 sg:pub.10.1007/bf00265424 schema:about anzsrc-for:04
    2 anzsrc-for:0403
    3 schema:author Naed048950bd14ecca2a485c2810e6249
    4 schema:citation sg:pub.10.1007/978-3-642-80087-0_19
    5 sg:pub.10.1007/bf00569938
    6 sg:pub.10.1007/bf01046635
    7 sg:pub.10.1007/bf01047488
    8 sg:pub.10.1007/bf01050638
    9 sg:pub.10.1007/bf01056897
    10 sg:pub.10.1007/bf01078811
    11 sg:pub.10.1007/bf01080358
    12 sg:pub.10.1007/bf01081756
    13 sg:pub.10.1007/bf01081981
    14 sg:pub.10.1007/bf01245476
    15 sg:pub.10.1007/bf02597227
    16 sg:pub.10.1038/366554a0
    17 sg:pub.10.1038/368326a0
    18 https://doi.org/10.1002/9781444303858.ch3
    19 https://doi.org/10.1016/0012-821x(74)90161-7
    20 https://doi.org/10.1016/0012-821x(85)90021-4
    21 https://doi.org/10.1016/0025-3227(90)90011-8
    22 https://doi.org/10.1016/0040-1951(72)90086-8
    23 https://doi.org/10.1016/0040-1951(82)90163-9
    24 https://doi.org/10.1016/0168-9622(86)90072-2
    25 https://doi.org/10.1016/0377-0273(81)90054-8
    26 https://doi.org/10.1016/0377-0273(82)90009-9
    27 https://doi.org/10.1016/0377-0273(83)90006-9
    28 https://doi.org/10.1016/0377-0273(83)90061-6
    29 https://doi.org/10.1016/0377-0273(84)90002-7
    30 https://doi.org/10.1016/0377-0273(89)90003-6
    31 https://doi.org/10.1016/0377-0273(90)90054-j
    32 https://doi.org/10.1016/0377-0273(94)90052-3
    33 https://doi.org/10.1016/0377-0273(94)90053-1
    34 https://doi.org/10.1029/jb078i023p05221
    35 https://doi.org/10.1029/jb087ib05p04035
    36 https://doi.org/10.1029/jb094ib12p17465
    37 https://doi.org/10.1098/rspa.1972.0115
    38 https://doi.org/10.1111/j.1365-246x.1987.tb01661.x
    39 https://doi.org/10.1126/science.236.4807.1442
    40 https://doi.org/10.1130/0016-7606(1992)104<1433:omvasr>2.3.co;2
    41 https://doi.org/10.1144/gsjgs.132.4.0429
    42 https://doi.org/10.3406/bagf.1982.5347
    43 schema:datePublished 1995-08
    44 schema:datePublishedReg 1995-08-01
    45 schema:description Sciara del Fuoco is the subaerial part of a partially filled sector-collapse scar that extends to 700 m below sea level on Stromboli volcano. The collapse occurred <5000 years ago, involved ≤1.81 km3 of rock and is the latest of a series of major collapses on the north-west flank of Stromboli. A north-east trending arc-axial fault system channels magmas into the volcano and has caused tilting and/or downthrow to the north-west. The slope of the partial cone constructed between the lateral walls of the collapse scar acts as a channelway to the sea for most eruptive products. From 700 m below sea level and extending to >2200 m and >10 km from the shore to the NNW, a fan-shaped mounded feature comprises debris avalanche deposits (>4 km3) from two or more sector collapses. Volcaniclastic density currents originating from Sciara del Fuoco follow the topographic margin of the debris avalanche deposits, although overbank currents and other unconfined currents widely cover the mounded feature with turbidites. Historical (recorded) eruptive activity in Sciara del Fuoco is considerably less than that which occurred earlier, and much of the partial fill may have formed from eruptions soon after the sector collapse. It is possible that a mass of eruptive products similar to that in the collapse scar is dispersed as volcanogenic sediment in deep water of the Tyrhennian basin. Evidence that the early post-collapse eruptive discharge was greater than the apparent recent flux (≈2kg/s) counters suggestions that a substantial part of Stromboli's growth has been endogenous. The partial fill of Sciaria del Fuoco is dominated by lava and spatter layers, rather than by the scoria and ash layers classically regarded as main constituents of Strombolian (‘cinder’) cones. Much of the volcanic slope beneath the vents is steeper than the angle of repose of loose tephra, which is therefore rapidly transported to the sea. Delicate pyroclasts that record the magmatic explosivity are selectively destroyed and diluted during sedimentary transport, mainly in avalanches and by shoreline wave reworking, and thus the submarine deposits do not record well the extent and diversity of explosive activity and associated clast-forming processes. Considerable amounts of dense (non-vesicular) fine sand and silt grains are produced by breakage and rounding of fragments of lava and agglutinate. The submarine extension of the collapse scar, and the continuing topographic depression to >2200 m below sea level, are zones of considerable by-passing of fine sand and silt, which are transported in turbidity currents. Evidently, volcanogenic sediments dispersed around island volcanoes by density currents are unlikely to record well the true spectrum and relative importance of clast-forming processes that occurred during an eruption. Marine sedimentary evidence of magmatic explosivity is particularly susceptible to partial or complete obliteration, unless there is a high rate of discharge of pyroclastic material into the sea.
    46 schema:genre research_article
    47 schema:inLanguage en
    48 schema:isAccessibleForFree false
    49 schema:isPartOf Nbadf93791eff4e899e507588ab5f1378
    50 Nd4c345488b4b461db1dfb1ea62b359ac
    51 sg:journal.1051922
    52 schema:name Sector collapse, sedimentation and clast population evolution at an active island-arc volcano: Stromboli, Italy
    53 schema:pagination 240-262
    54 schema:productId N622001c969574fd2ab203cad92f39e28
    55 N84188330658149f38cb58720dfb400e2
    56 N94c86d09a2c6409d833a987a1020e8aa
    57 schema:sameAs https://app.dimensions.ai/details/publication/pub.1024824153
    58 https://doi.org/10.1007/bf00265424
    59 schema:sdDatePublished 2019-04-11T13:47
    60 schema:sdLicense https://scigraph.springernature.com/explorer/license/
    61 schema:sdPublisher N6dfb3ec2003a4073bc5accae4f06061c
    62 schema:url http://link.springer.com/10.1007/BF00265424
    63 sgo:license sg:explorer/license/
    64 sgo:sdDataset articles
    65 rdf:type schema:ScholarlyArticle
    66 N5d544ee5b93449729dbd7bdfef2ee630 rdf:first sg:person.07663171313.28
    67 rdf:rest rdf:nil
    68 N622001c969574fd2ab203cad92f39e28 schema:name dimensions_id
    69 schema:value pub.1024824153
    70 rdf:type schema:PropertyValue
    71 N6dfb3ec2003a4073bc5accae4f06061c schema:name Springer Nature - SN SciGraph project
    72 rdf:type schema:Organization
    73 N84188330658149f38cb58720dfb400e2 schema:name readcube_id
    74 schema:value 764368368dae39055eb099cf33226122325e19056dfb03242434fce99654409f
    75 rdf:type schema:PropertyValue
    76 N94c86d09a2c6409d833a987a1020e8aa schema:name doi
    77 schema:value 10.1007/bf00265424
    78 rdf:type schema:PropertyValue
    79 Naed048950bd14ecca2a485c2810e6249 rdf:first sg:person.01160134750.42
    80 rdf:rest N5d544ee5b93449729dbd7bdfef2ee630
    81 Nbadf93791eff4e899e507588ab5f1378 schema:issueNumber 4
    82 rdf:type schema:PublicationIssue
    83 Nd4c345488b4b461db1dfb1ea62b359ac schema:volumeNumber 57
    84 rdf:type schema:PublicationVolume
    85 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
    86 schema:name Earth Sciences
    87 rdf:type schema:DefinedTerm
    88 anzsrc-for:0403 schema:inDefinedTermSet anzsrc-for:
    89 schema:name Geology
    90 rdf:type schema:DefinedTerm
    91 sg:journal.1051922 schema:issn 0258-8900
    92 1432-0819
    93 schema:name Bulletin of Volcanology
    94 rdf:type schema:Periodical
    95 sg:person.01160134750.42 schema:affiliation https://www.grid.ac/institutes/grid.10025.36
    96 schema:familyName Kokelaar
    97 schema:givenName P.
    98 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.01160134750.42
    99 rdf:type schema:Person
    100 sg:person.07663171313.28 schema:affiliation https://www.grid.ac/institutes/grid.6292.f
    101 schema:familyName Romagnoli
    102 schema:givenName C.
    103 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.07663171313.28
    104 rdf:type schema:Person
    105 sg:pub.10.1007/978-3-642-80087-0_19 schema:sameAs https://app.dimensions.ai/details/publication/pub.1017357856
    106 https://doi.org/10.1007/978-3-642-80087-0_19
    107 rdf:type schema:CreativeWork
    108 sg:pub.10.1007/bf00569938 schema:sameAs https://app.dimensions.ai/details/publication/pub.1016642754
    109 https://doi.org/10.1007/bf00569938
    110 rdf:type schema:CreativeWork
    111 sg:pub.10.1007/bf01046635 schema:sameAs https://app.dimensions.ai/details/publication/pub.1036491679
    112 https://doi.org/10.1007/bf01046635
    113 rdf:type schema:CreativeWork
    114 sg:pub.10.1007/bf01047488 schema:sameAs https://app.dimensions.ai/details/publication/pub.1053738817
    115 https://doi.org/10.1007/bf01047488
    116 rdf:type schema:CreativeWork
    117 sg:pub.10.1007/bf01050638 schema:sameAs https://app.dimensions.ai/details/publication/pub.1026850566
    118 https://doi.org/10.1007/bf01050638
    119 rdf:type schema:CreativeWork
    120 sg:pub.10.1007/bf01056897 schema:sameAs https://app.dimensions.ai/details/publication/pub.1028157096
    121 https://doi.org/10.1007/bf01056897
    122 rdf:type schema:CreativeWork
    123 sg:pub.10.1007/bf01078811 schema:sameAs https://app.dimensions.ai/details/publication/pub.1017939651
    124 https://doi.org/10.1007/bf01078811
    125 rdf:type schema:CreativeWork
    126 sg:pub.10.1007/bf01080358 schema:sameAs https://app.dimensions.ai/details/publication/pub.1025123668
    127 https://doi.org/10.1007/bf01080358
    128 rdf:type schema:CreativeWork
    129 sg:pub.10.1007/bf01081756 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041163103
    130 https://doi.org/10.1007/bf01081756
    131 rdf:type schema:CreativeWork
    132 sg:pub.10.1007/bf01081981 schema:sameAs https://app.dimensions.ai/details/publication/pub.1030465754
    133 https://doi.org/10.1007/bf01081981
    134 rdf:type schema:CreativeWork
    135 sg:pub.10.1007/bf01245476 schema:sameAs https://app.dimensions.ai/details/publication/pub.1033033221
    136 https://doi.org/10.1007/bf01245476
    137 rdf:type schema:CreativeWork
    138 sg:pub.10.1007/bf02597227 schema:sameAs https://app.dimensions.ai/details/publication/pub.1004212689
    139 https://doi.org/10.1007/bf02597227
    140 rdf:type schema:CreativeWork
    141 sg:pub.10.1038/366554a0 schema:sameAs https://app.dimensions.ai/details/publication/pub.1037301642
    142 https://doi.org/10.1038/366554a0
    143 rdf:type schema:CreativeWork
    144 sg:pub.10.1038/368326a0 schema:sameAs https://app.dimensions.ai/details/publication/pub.1002591528
    145 https://doi.org/10.1038/368326a0
    146 rdf:type schema:CreativeWork
    147 https://doi.org/10.1002/9781444303858.ch3 schema:sameAs https://app.dimensions.ai/details/publication/pub.1023805130
    148 rdf:type schema:CreativeWork
    149 https://doi.org/10.1016/0012-821x(74)90161-7 schema:sameAs https://app.dimensions.ai/details/publication/pub.1052553778
    150 rdf:type schema:CreativeWork
    151 https://doi.org/10.1016/0012-821x(85)90021-4 schema:sameAs https://app.dimensions.ai/details/publication/pub.1022675570
    152 rdf:type schema:CreativeWork
    153 https://doi.org/10.1016/0025-3227(90)90011-8 schema:sameAs https://app.dimensions.ai/details/publication/pub.1028140023
    154 rdf:type schema:CreativeWork
    155 https://doi.org/10.1016/0040-1951(72)90086-8 schema:sameAs https://app.dimensions.ai/details/publication/pub.1050823166
    156 rdf:type schema:CreativeWork
    157 https://doi.org/10.1016/0040-1951(82)90163-9 schema:sameAs https://app.dimensions.ai/details/publication/pub.1008972534
    158 rdf:type schema:CreativeWork
    159 https://doi.org/10.1016/0168-9622(86)90072-2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1017157488
    160 rdf:type schema:CreativeWork
    161 https://doi.org/10.1016/0377-0273(81)90054-8 schema:sameAs https://app.dimensions.ai/details/publication/pub.1053128692
    162 rdf:type schema:CreativeWork
    163 https://doi.org/10.1016/0377-0273(82)90009-9 schema:sameAs https://app.dimensions.ai/details/publication/pub.1033760811
    164 rdf:type schema:CreativeWork
    165 https://doi.org/10.1016/0377-0273(83)90006-9 schema:sameAs https://app.dimensions.ai/details/publication/pub.1048165048
    166 rdf:type schema:CreativeWork
    167 https://doi.org/10.1016/0377-0273(83)90061-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1037182164
    168 rdf:type schema:CreativeWork
    169 https://doi.org/10.1016/0377-0273(84)90002-7 schema:sameAs https://app.dimensions.ai/details/publication/pub.1016476042
    170 rdf:type schema:CreativeWork
    171 https://doi.org/10.1016/0377-0273(89)90003-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041446227
    172 rdf:type schema:CreativeWork
    173 https://doi.org/10.1016/0377-0273(90)90054-j schema:sameAs https://app.dimensions.ai/details/publication/pub.1037690583
    174 rdf:type schema:CreativeWork
    175 https://doi.org/10.1016/0377-0273(94)90052-3 schema:sameAs https://app.dimensions.ai/details/publication/pub.1042117455
    176 rdf:type schema:CreativeWork
    177 https://doi.org/10.1016/0377-0273(94)90053-1 schema:sameAs https://app.dimensions.ai/details/publication/pub.1034720039
    178 rdf:type schema:CreativeWork
    179 https://doi.org/10.1029/jb078i023p05221 schema:sameAs https://app.dimensions.ai/details/publication/pub.1039273424
    180 rdf:type schema:CreativeWork
    181 https://doi.org/10.1029/jb087ib05p04035 schema:sameAs https://app.dimensions.ai/details/publication/pub.1024482943
    182 rdf:type schema:CreativeWork
    183 https://doi.org/10.1029/jb094ib12p17465 schema:sameAs https://app.dimensions.ai/details/publication/pub.1046802632
    184 rdf:type schema:CreativeWork
    185 https://doi.org/10.1098/rspa.1972.0115 schema:sameAs https://app.dimensions.ai/details/publication/pub.1048356459
    186 rdf:type schema:CreativeWork
    187 https://doi.org/10.1111/j.1365-246x.1987.tb01661.x schema:sameAs https://app.dimensions.ai/details/publication/pub.1033642517
    188 rdf:type schema:CreativeWork
    189 https://doi.org/10.1126/science.236.4807.1442 schema:sameAs https://app.dimensions.ai/details/publication/pub.1062534268
    190 rdf:type schema:CreativeWork
    191 https://doi.org/10.1130/0016-7606(1992)104<1433:omvasr>2.3.co;2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1036916614
    192 rdf:type schema:CreativeWork
    193 https://doi.org/10.1144/gsjgs.132.4.0429 schema:sameAs https://app.dimensions.ai/details/publication/pub.1015791273
    194 rdf:type schema:CreativeWork
    195 https://doi.org/10.3406/bagf.1982.5347 schema:sameAs https://app.dimensions.ai/details/publication/pub.1027008206
    196 rdf:type schema:CreativeWork
    197 https://www.grid.ac/institutes/grid.10025.36 schema:alternateName University of Liverpool
    198 schema:name Earth Sciences Department, University of Liverpool, L69 3BX, Liverpool, UK
    199 rdf:type schema:Organization
    200 https://www.grid.ac/institutes/grid.6292.f schema:alternateName University of Bologna
    201 schema:name Departimento di Scienze Mineralogiche, Università di Bologna, 40126, Bologna, Italy
    202 rdf:type schema:Organization
     




    Preview window. Press ESC to close (or click here)


    ...