GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Keywords
Language
  • 1
    Keywords: Earth sciences ; Earth Sciences ; Structural geology ; Mineralogy ; Natural disasters ; Earth sciences ; Structural geology ; Mineralogy ; Natural disasters ; Intrusion ; Gang ; Lakkolith ; Magmakammer ; Lagergang ; Magma ; Magmatismus ; Magmatisches Gestein ; Intrusion ; Gang ; Lakkolith ; Magmakammer ; Magmakammer ; Lagergang ; Magma ; Magmatismus ; Magmatisches Gestein
    Description / Table of Contents: Physical Geology of Shallow-Level Magmatic Systems—An Introduction -- Geometric Scaling of Tabular Igneous Intrusions: Implications for Emplacement and Growth -- Plumbing Systems of Shallow Level Intrusive Complexes -- Sub-Volcanic Intrusions and the Link to Global Climatic andEnvironmental Changes -- Sills in Sedimentary Basins and Petroleum Systems -- The Subvolcanic Units of the Late Paleozoic Halle Volcanic Complex, Germany: Geometry, Internal Textures and Emplacement Mode -- Laccolithic Emplacement of the Northern Arran Granite,Scotland, Based on Magnetic Fabric Data -- Erratum to: Sub-volcanic Intrusions in the Karoo Basin,South Africa. .
    Type of Medium: Online Resource
    Pages: Online-Ressource (400 p, online resource)
    Edition: Corrected publication
    ISBN: 9783319140841
    Series Statement: Advances in Volcanology
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Physical geology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (425 pages)
    Edition: 1st ed.
    ISBN: 9783319140841
    Series Statement: Advances in Volcanology Series
    Language: English
    Note: Intro -- Foreword -- Preface -- History, Design and Aims of This Book -- Acknowledgements -- References -- Contents -- About the Editors -- 32 Physical Geology of Shallow-Level Magmatic Systems-An Introduction -- 1 What Is a Subvolcanic Body? -- 2 Magma Ascent -- 3 Magma Flow/Emplacement -- 3.1 From Dyke to Sill-The Flip in Flow Direction -- 3.2 Filling up a Subvolcanic Body -- 4 Timing for the Emplacement -- 5 Environmental and Societal Impact -- References -- 1000 Geometric Scaling of Tabular Igneous Intrusions: Implications for Emplacement and Growth -- Abstract -- 1 Introduction -- 2 Geometric Scaling Analysis -- 3 General Characteristics and Scaling of Tabular Intrusion -- 3.1 Mafic Dykes -- 3.2 Sills and Sub-horizontal Sheets -- 3.3 Laccoliths -- 3.4 Plutons, Layered Intrusions and Batholiths -- 4 Relationships Between Emplacement Mechanisms, Depth and Scaling Relationships -- 4.1 Intrusions that Do not Interact with Earth's Surface -- 4.2 Intrusions that Do Interact with Earth's Surface -- 5 Modelling the Growth of Sills and Laccoliths -- 5.1 Influence of Emplacement Depth and Bulk Country Rock Mechanical Properties -- 5.2 Selected Case Studies of Sills and Laccoliths -- 5.2.1 Black Mesa Laccolith, Henry Mountains, Utah -- 5.2.2 San Martino Laccoliths, Elba Island -- 5.2.3 Torres Del Paine Pluton, Patagonia -- 5.2.4 Palisades Sill, Eastern USA and Franklin Sills, Nunavut, Canada -- 5.3 Timescales of Laccolith and Sill Growth -- 6 Discussion -- 6.1 Bifurcation Between Laccolith and Sill Growth Histories -- 6.2 Intrusions Too Deep to Interact with Earth's Surface -- 7 Towards a General Framework for Tabular Intrusion Emplacement and Growth -- Acknowledgements -- References -- 8 Plumbing Systems of Shallow Level Intrusive Complexes -- Abstract -- 1 Introduction -- 2 What is the Magma Plumbing System? -- 3 Large Igneous Provinces. , 4 Predominantly Rifted Settings -- 5 Plumbing at Polygenetic Volcanoes-Persistent Magma Pathways -- 6 Exposed Shallow Volcanic Centres and Complexes -- 7 Innovative Ways to Image and Understand Magma Plumbing -- 7.1 Geophysical Imaging of Ancient Magma Plumbing Systems in 3D -- 7.2 Using Volcanic Products to Investigate the Sub-volcanic System -- 8 Closing Remarks -- Acknowledgments -- References -- 11 The Volcanic-Plutonic Connection -- Abstract -- 1 Introduction -- 1.1 The Uncertain Relationships Between Volcanic and Plutonic Rocks -- 1.2 What Is a Pluton? -- 1.3 Historical Views of the Volcanic-Plutonic Connection -- 1.4 Relevant Data -- 2 Methods -- 3 The Sampling Problem -- 4 Compositional Comparison of Volcanic and Plutonic Rocks -- 4.1 Introduction -- 4.2 Global Comparison for Convergent Margins -- 4.3 Regional and Local Tests -- 4.4 The Titanite Problem -- 5 Geochronology -- 5.1 Magma Flux -- 5.2 Geochronologic Tests for the Link Between Plutons and Large-Volume Ignimbrites -- 6 Closing Remarks -- Acknowledgments -- References -- 31 Structures Related to the Emplacement of Shallow-Level Intrusions -- Abstract -- 1 Introduction -- 2 Structural Subdivisions Scheme -- 2.1 Intrusion-Related Structures -- 2.2 Magmatic Flow-Related Structures -- 2.2.1 Surface Structures -- 2.2.2 Internal Visibly-Oriented Features -- 2.2.3 Anisotropy of Magnetic Susceptibility -- 2.3 Solid-State Flow-Related Structures (Syn-magmatic, Non-tectonic) -- 2.4 Thermal and Fragmental Structures -- 2.5 Examining Multiple Approaches -- 3 Example of Elba Laccoliths: A Case for Coherence -- 3.1 Interior Fabrics and Flow -- 3.2 Ornamented Waveforms and Disrupted Contacts -- 3.3 Coherence -- 4 Concluding Summary -- Acknowledgements -- References -- 4 Geochemical Fingerprinting and Magmatic Plumbing Systems -- Abstract -- 1 Introduction -- 2 Chemical Fingerprinting. , 2.1 Element Ratios -- 2.2 Statistical Methods -- 3 Application to the Golden Valley Sill Complex (GVSC), Karoo Basin, South Africa -- 4 Implications -- 4.1 Genetic Relationship and Evolutionary History -- 4.2 Emplacement Mechanism of the GVSC Plumbing System -- 5 Summary and Perspectives -- References -- 6 Geophysics and Remote Sensing -- Abstract -- 1 Introduction (F1-3) -- 2 Seismic Reflection Method -- 2.1 Petrophysics -- 2.2 Seismic Imaging -- 2.3 Seismic Interpretation -- 3 Other Geophysical Methods -- 3.1 Integrated Seismic, Gravity, Magnetic Interpretation -- 3.2 Wide-Angle Seismic and Electromagnetic Data -- 3.3 Satellite Images and Topography -- 4 Summary -- Acknowledgments -- References -- 9 Laboratory Modelling of Volcano Plumbing Systems: A Review -- Abstract -- 1 Introduction -- 2 Model Materials -- 2.1 Model Magma -- 2.1.1 "High" Viscosity Magma -- 2.1.2 "Low" Viscosity Magma -- 2.1.3 Conceptual Magma Chambers -- 2.2 Model Rocks -- 2.2.1 Plasticity-Dominated Materials (Weak Materials) -- 2.2.2 Elasticity-Dominated Materials (Strong Materials) -- 2.2.3 Elasto-Plastic (Intermediate Strength) Materials -- 2.2.4 Other Materials -- 2.2.5 Summary -- 3 A Crucial Starting Point: The Model "Scaling" -- 3.1 Dimensional Analysis -- 3.2 Similarity to Geological Systems -- 4 Geological Applications -- 4.1 Dyke Formation -- 4.1.1 Dyke Nucleation from a Magma Reservoir -- 4.1.2 Dyke Propagation in a Homogeneous and Isotropic Medium-The Effects of Buoyancy -- 4.1.3 Effects of Contrasting Magma Viscosities on Composite Dyke Propagation -- 4.1.4 Effects of Mechanical Heterogeneity (Prexisting Dykes or Layering) on Dyke Propagation -- 4.1.5 Effects of Anisotropic Stress Fields (From Regional Tectonics or Local Topography) on Dyke Propagation -- 4.1.6 Interaction of Coevally Propagating Dykes -- 4.1.7 Inelastic Processes Associated with Dyke Propagation. , 4.1.8 Effects of Cooling on Dyke Propagation -- 4.2 Cone Sheet Emplacement -- 4.3 Sill Formation -- 4.3.1 Formation of Sills from Vertically-Propagating Dykes -- 4.3.2 Formation of Saucer-Shaped Sills -- 4.3.3 Effects of Cooling on Sill Emplacement -- 4.4 Laccoliths, Stocks and Cryptodomes -- 4.4.1 General Development of Laccolith Emplacement and Controls from Host Rock Layering -- 4.4.2 Controls of Regional Tectonics or Gravitational Spreading on Laccolith Emplacement -- 4.4.3 Formation of Stocks or Cryptodomes -- 4.4.4 The Roles of Magma Viscosity and Host Rock Strength in the Formation of Laccoliths, Stocks and Cryptodomes -- 4.5 Caldera-Related Structures and Intrusions -- 4.5.1 Generalised Geometry and Kinematics of Ring-Fault Related to Caldera Subsidence -- 4.5.2 Effects of Initial Geometric Parameters on Collapse -- 4.5.3 Effects of Host-Rock Cohesion on Collapse -- 4.5.4 Effects of Topography and Regional Tectonics on Collapse Structures -- 4.5.5 Effects of Caldera Collapse on Magma Chamber Dynamics and Ring-Dyke Intrusion -- 4.5.6 Kinematics of Pre-collapse 'Tumescence' and Post-collapse Caldera 'Resurgence' -- 4.5.7 Limitations of Caldera-Related Experiments -- 4.6 Ground Deformation Induced by Intrusions -- 4.6.1 Surface Deformation Related to Dykes -- 4.6.2 Surface Deformation Related to Saucer-Shaped Sills or Cone Sheets -- 4.6.3 Surface Deformation Related to Cryptodomes -- 4.7 Magma Intrusions in Deforming Crust (Magma-Fault Interactions) -- 4.8 Explosive Volcanic Vents -- 5 Conclusions and Perspectives -- References -- 1001 Catastrophic Collapse Features in Volcanic Terrains: Styles and Links to Subvolcanic Magma Systems -- Abstract -- 1 Introduction -- 2 Volcanic Landslides -- 2.1 Volcanic Slides -- 2.2 Volcanic Debris Avalanches -- 2.3 Volcanic Debris Flows. , 2.4 Mount St. Helens, USA: Classic Case Study of Cataclysmic Collapse and Eruption -- 3 Collapse Styles in Volcanic Terrains -- 3.1 Volcano Collapse Type -- 3.2 Laccolith Collapse Type -- 3.3 Volcanic Field Collapse Type -- 4 Volcanic Landslide Features and Deposits -- 4.1 Slide Zone -- 4.2 Debris Avalanche Zone -- 4.3 Debris Flow Zone -- 5 Causes of Volcanic Collapse in Volcanic Terrains -- 5.1 Role of Magma in Volcanic Destabilization -- 5.2 Triggers -- 6 Volcanic Landslide Transport and Mobility Mechanisms -- 7 Hazards -- 8 Summary -- Acknowledgements -- References -- 10 Sub-Volcanic Intrusions and the Link to Global Climatic and Environmental Changes -- Abstract -- 1 LIPs and the Environment -- 2 Sills and Pipes in the Karoo Basin -- 3 Methods -- 4 Results -- 4.1 Geology of the Ladybrand Area -- 4.2 The Olney Breccia -- 4.3 Basalt and Dolerite Geochemistry -- 4.4 Contact Metamorphism of Ecca Shale -- 5 Discussion -- 5.1 Aureole Thickness and Gas Volume -- 5.2 Relative Age of Sills, Phreatomagmatism, and Lavas -- 5.3 Short- and Long Term Fluid Flow -- 5.4 Perspectives on Sills, Aureoles, Venting and the Environment -- 6 Conclusions -- Acknowledgments -- References -- 17 Sills in Sedimentary Basins and Petroleum Systems -- Abstract -- 1 Introduction -- 2 Geological Summary of the Isle of Skye -- 3 Petroleum Geology of the Isle of Skye/Sea of Hebrides -- 3.1 The Upper Glen-1 Well -- 3.2 The Potential Petroleum System Across the Sea of Hebrides/Malin Basins -- 4 The Trotternish/Minch Sill Complex -- 5 Key Outcrops and Structures -- 6 Discussion -- 6.1 Emplacement of the Trotternish/Minch Sill Complex Compared with the North Atlantic Margin Sill Complexes -- 6.2 How Does the Structure of the Trotternish/Minch Sill Complex Compare to Offshore Examples in Other Sedimentary Basins? -- 6.3 Effect of Sill Intrusions on Jurassic Sequences and Source Rocks. , 6.4 Thermal Effects of the Skye Central Complex on Reservoir and Source Intervals.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract. The Abbott Unit (∼508 Ma) and the Vegetation Unit (∼475 Ma) of the Terra Nova Intrusive Complex (northern Victoria Land, Antarctica) represent the latest magmatic events related to the Early Paleozoic Ross Orogeny. They show different emplacement styles and depths, ranging from forcible at 0.4–0.5 GPa for the Abbott Unit to passive at ∼0.2 GPa for the Vegetation Unit. Both units consist of mafic, felsic and intermediate facies which collectively define continuous chemical trends. The most mafic rocks from both units show different enrichment in trace element and Sr-Nd isotopic signatures. Once the possible effects of upper crustal assimilation-fractional crystallisation (AFC) and lower crustal coupled AFC and magma refilling processes have been taken into account the following features are recognised: (1) the modelled primary Abbott Unit magma shows a slightly enriched incompatible element distribution, similar to common continental arc basalts and (2) the modelled primary Vegetation Unit magma displays highly enriched isotope ratios and incompatible element patterns. We interpreted these major changes in magmatic affinity and emplacement style as linked to a major change in the tectonic setting affecting melt generation, rise and emplacement of the magmas. The Abbott Unit mafic melts were derived from a mantle wedge above a subduction zone, with subcontinental lithospheric mantle marginally involved in the melting column. The Vegetation Unit mafic melts are regarded as products of a different source involving an old layer of subcontinental lithospheric mantle. The crustal evolution of both types of mafic melts is marked by significant compositional contrasts in Sr and Nd isotopes between mafic and associated felsic rocks. The crustal isotope signature showed an increase with felsic character. Geochemical variations for both units can be accounted for by a similar two-stage hybridisation process. In the first stage, the most mafic magma evolved mainly by fractional crystallisation coupled with assimilation of metasedimentary rocks having crustal time-integrated Sr and Nd compositions similar to those of locally exposed metamorphic basement. The second stage involves contaminated products mixing with independently generated crustal melts. Petrographic, geochemical and isotope data also provide evidence of significant compositional differences in the felsic end-members, pointing to the involvement of metaigneous and metasedimentary source rocks for the Abbott granite and Vegetation leucogranite, respectively.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2024-01-20
    Keywords: AND-2A; ANDRILL; Antarctic Geological Drilling; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Lithologic unit/sequence; Lithology/composition/facies; McMurdo Sound; McMurdo Station; Reworked; Rock type; Sample comment; Sample type; Sediment type; SMS; Southern McMurdo Sound
    Type: Dataset
    Format: text/tab-separated-values, 153 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Panter, Kurt S; Talarico, Franco M; Bassett, K; Del Carlo, Paola; Field, B; Frank, T; Hoffmann, Stefan; Kuhn, Gerhard; Reichelt, Lucia; Sandroni, Sonja; Taviani, Marco; Bracciali, Laura; Cornamusini, G; von Eynatten, Hilmar; Rocchi, Sergio; SMS Science Team (2009): Petrologic and geochemical composition of the AND-2A Core, ANDRILL Southern McMurdo Sound Project, Antarctica. Terra Antartica, 15(1), 147-192, hdl:10013/epic.36329.d001
    Publication Date: 2024-01-20
    Description: The compositional record of the AND-2A drillcore is examined using petrological, sedimentological, volcanological and geochemical analysis of clasts, sediments and pore waters. Preliminary investigations of basement clasts (granitoids and metasediments) indicate both local and distal sources corresponding to variable ice-volume and ice-flow directions. Low abundance of sedimentary clasts (e.g., arkose, litharenite) suggests reduced contributions from sedimentary covers while intraclasts (e.g., diamictite, conglomerate) attest to intrabasinal reworking. Volcanic material includes pyroclasts (e.g., pumice, scoria), sediments and lava. Primary and reworked tephra layers occur within the Early Miocene interval (1093 to 640 metres below sea floor mbsf). The compositions of volcanic clasts reveal a diversity of alkaline types derived from the McMurdo Volcanic Group. Finer-grained sediments (e.g., sandstone, siltstone) show increases in biogenic silica and volcanic glass from 230 to 780 mbsf and higher proportions of terrigenous material c. 350 to 750 mbsf and below 970 mbsf. Basement clast assemblages suggest a dominant provenance from the Skelton Glacier - Darwin Glacier area and from the Ferrar Glacier - Koettlitz Glacier area. Provenance of sand grains is consistent with clast sources. Thirteen Geochemical Units are established based on compositional trends derived from continuous XRF scanning. High values of Fe and Ti indicate terrigenous and volcanic sources, whereas high Ca values signify either biogenic or diagenic sources. Highly alkaline and saline pore waters were produced by chemical exchange with glass at moderately elevated temperatures.
    Keywords: Alkalinity, total; AND-2A; Bromide; Chloride; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Lithium; Magnesium; McMurdo Sound; McMurdo Station; pH; Potassium; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Salinity; SMS; Sodium; Southern McMurdo Sound; SPP1158; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 234 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2024-01-20
    Keywords: -; Age, dated; Age, dated standard deviation; Age model; Age model, optional; AND-2A; ANDRILL; Antarctic Geological Drilling; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; McMurdo Sound; McMurdo Station; Method comment; Sample amount; Sample type; SMS; Southern McMurdo Sound
    Type: Dataset
    Format: text/tab-separated-values, 261 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2024-01-20
    Keywords: Age, dated; Age, dated standard deviation; AND-2A; ANDRILL; Antarctic Geological Drilling; Argon-36; Argon-37; Argon-38; Argon-39; Argon-40; Calcium/Potassium ratio; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Grains, counted/analyzed; Grain size description; Laser power; McMurdo Sound; McMurdo Station; Method comment; Sample ID; Sample mass; Sample type; SMS; Southern McMurdo Sound; Standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 3384 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Di Vincenzo, Gianfranco; Bracciali, Laura; Del Carlo, Paola; Panter, Kurt S; Rocchi, Sergio (2010): 40Ar-39Ar dating of volcanogenic products from the AND-2A core (ANDRILL Southern McMurdo Sound Project, Antarctica): correlations with the Erebus Volcanic Province and implications for the age model of the core. Bulletin of Volcanology, 72(4), 487-505, https://doi.org/10.1007/s00445-009-0337-z
    Publication Date: 2024-01-20
    Description: The AND-2A drillcore (Antarctic Drilling Program-ANDRILL) was successfully completed in late 2007 on the Antarctic continental margin (Southern McMurdo Sound, Ross Sea) with the aim of tracking ice proximal to shallow marine environmental fluctuations and to document the 20-Ma evolution of the Erebus Volcanic Province. Lava clasts and tephra layers from the AND-2A drillcore were investigated from a petrographic and stratigraphic point of view and analyzed by the 40Ar-39Ar laser technique in order to constrain the age model of the core and to gain information on the style and nature of sediment deposition in the Victoria Land Basin since Early Miocene. Ten out of 17 samples yielded statistically robust 40Ar-39Ar ages, indicating that the AND-2A drillcore recovered 〈230 m of Middle Miocene (~128-358 m below sea floor, ~11.5-16.0 Ma) and 〉780 m of Early Miocene (~358-1093 m below sea floor, ~16.0-20.1 Ma). Results also highlight a nearly continuous stratigraphic record from at least 358 m below sea floor down hole, characterized by a mean sedimentation rate of ~19 cm/ka, possible oscillations of no more than a few hundreds of ka and a break within ~17.5-18.1 Ma. Comparison with available data from volcanic deposits on land, suggests that volcanic rocks within the AND-2A core were supplied from the south, possibly with source areas closer to the drill site for the upper core levels, and from 358 m below sea floor down hole, with the 'proto-Mount Morning' as the main source.
    Keywords: AND-2A; ANDRILL; Antarctic Geological Drilling; DRILL; Drilling/drill rig; International Polar Year (2007-2008); IPY; McMurdo Sound; McMurdo Station; SMS; Southern McMurdo Sound
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2019-03-28
    Description: Explosive volcanoes from the southern Andes are able to disperse ash over wide areas of the Southern Hemisphere, potentially as far as Antarctica. With the aim of improving correlations between sources and tephra in southernmost South America and, possibly, Antarctica, this work presents new field, textural and geochemical data on tephra layers from southern Patagonia and Tierra del Fuego (Argentina and Chile). Major- and trace-element data, obtained on single glass shards allowed to identify tephra sources in Late Glacial-Holocene eruptions from Hudson, Reclus and Mt Burney volcanoes, located in the Southern and Austral Volcanic Zone of the Andean Cordillera. Twelve new radiocarbon age determinations of charcoals, peats and soils have further constrained the correlations between the studied tephra layers and known eruptions from Hudson, Mt Burney and Reclus volcanoes. Therefore, this study contributes to expand the geochemical dataset on volcanic glasses valuable for tephra correlations in South America, and improves the current tephrostratigraphic framework of this region. Furthermore, we revised literature data by compiling a database including Neogene-Quaternary volcanic tephra found in Antarctic ice cores, marine sediments, blue ice and continental outcrops as well as tephra produced by volcanic sources located in Antarctica and circum-Antarctic areas. This revision shows that Antarctic tephra can be correlated with confidence to Antarctic and circum-Antarctic (South Shetlands and South Sandwich Islands) volcanic sources, whereas correlations with South American sources are arguable, and a complete geochemical fingerprinting is needed for validation
    Description: Published
    Description: 153-170
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...