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  • 1
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 95.0255
    In: Geological Society special publication
    Description / Table of Contents: Geoscientists need to familiarize themselves with the characteristics of actual plate motions. A popular, current thesis relates the state of stress to the degree of coupling of the two convergent plates. Recent two-dimentional, finite element modelling has demonstrated how the stress in the overriding plate is critically dependent on wether the subduction zone is locked (i.e. high degree of coupling) or unlocked. Thus the compressional stress regime occurs in locked systems, and extensional strees in unlocked systems; a gradient from compression in the fore-arc to extension in the back-arc is said to characterize partially locked system. However, studies of the strain field in real cases (modern arc regions) clearly indicate the prevalence of subhorizontal extension orientated nearly perpendicular to the arc. Implicit in these real observations is the suggestion that stresses resulting from plate coupling are either not transmitted to the volcanic arc, or else locked subduction zones are uncommon and extension may be the normal mode of behaviour. The rationale and evidence for extension and coeval volcanism at consuming plate margins is presented. Using mainly Cenozoic case histories for oceanic and continental margin arcs, structural evidence is presented, which demonstrates that volcanism in most arc systems is contemporaneous with normal faulting and subsidence as a general case. Representive, modern geochemical data sets are provided and integrated in a petrological discussion for each case history. The western Pacific, now widely regard as a type region for the study of convergent plate margin processes, is particularly well represented. Also included is evidence from less commonly insvestigated regions, where subduction has ceased or is no longer obvious but an association with an arc is unequivocal. By these means, it is hoped that this volume contains a representative cross-section of current research on extension-related arc volcanism in broadest sense, and that it will stimulate further discussion and research into the complex tectonics and petrology of covergent plate margins.
    Type of Medium: Monograph available for loan
    Pages: 293 S. , Ill., graph. Darst., Kt.
    ISBN: 1897799179
    Series Statement: Geological Society special publication 81
    Classification:
    Petrology, Petrography
    Language: English
    Note: J. L. Smellie: Volcanism associated with extension at consuming plate margins / Geological Society, London, Special Publications, 81:1, doi:10.1144/GSL.SP.1994.081.01.01 --- Tectonics and Magmatism --- Warren B. Hamilton: Subduction systems and magmatism / Geological Society, London, Special Publications, 81:3-28, doi:10.1144/GSL.SP.1994.081.01.02 --- Oceanic Arc Systems --- Peter D. Clift and ODP Leg 135 Scientific Party: Volcanism and sedimentation in a rifting island-arc terrain: an example from Tonga, SW Pacific / Geological Society, London, Special Publications, 81:29-51, doi:10.1144/GSL.SP.1994.081.01.03 --- Julian A. Pearce, Michelle Ernewein, Sherman H. Bloomer, Lindsay M. Parson, Bramley J. Murton, and Lynn E. Johnson: Geochemistry of Lau Basin volcanic rocks: influence of ridge segmentation and arc proximity / Geological Society, London, Special Publications, 81:53-75, doi:10.1144/GSL.SP.1994.081.01.04 --- Ulrich Knittel and Oles Dietmar: Basaltic volcanism associated with extensional tectonics in the Taiwan-Luzon island arc: evidence for non-depleted sources and subduction zone enrichment / Geological Society, London, Special Publications, 81:77-93, doi:10.1144/GSL.SP.1994.081.01.05 --- M. R. Wharton, B. Hathway, and H. Colley: Volcanism associated with extension in an Oligocene—Miocene arc, southwestern Viti Levu, Fiji / Geological Society, London, Special Publications, 81:95-114, doi:10.1144/GSL.SP.1994.081.01.06 --- Rex N. Taylor and Robert W. Nesbitt: Arc volcanism in an extensional regime at the initiation of subduction: a geochemical study of Hahajima, Bonin Islands, Japan / Geological Society, London, Special Publications, 81:115-134, doi:10.1144/GSL.SP.1994.081.01.07 --- C. Picard, M. Monzier, J.-P. Eissen, and C. Robin: Concomitant evolution of tectonic environment and magma geochemistry, Ambrym volcano (Vanuatu, New Hebrides arc) / Geological Society, London, Special Publications, 81:135-154, doi:10.1144/GSL.SP.1994.081.01.08 --- J. C. Aitchison and P. G. Flood: Gamilaroi Terrane: A Devonian rifted intra-oceanic island-arc assemblage, NSW, Australia. / Geological Society, London, Special Publications, 81:155-168, doi:10.1144/GSL.SP.1994.081.01.09 --- Continental Margin Arcs --- André Pouclet, Jin-Soo Lee, Philippe Vidal, Brian Cousens, and Hervé Bellon: Cretaceous to Cenozoic volcanism in South Korea and in the Sea of Japan: magmatic constraints on the opening of the back-arc basin / Geological Society, London, Special Publications, 81:169-191, doi:10.1144/GSL.SP.1994.081.01.10 --- J. A. Gamble, I. C. Wright, J. D. Woodhead, and M. T. McCulloch: Arc and back-arc geochemistry in the southern Kermadec arc-Ngatoro Basin and offshore Taupo Volcanic Zone, SW Pacific / Geological Society, London, Special Publications, 81:193-212, doi:10.1144/GSL.SP.1994.081.01.11 --- G. Pe-Piper, D. J. W. Piper, C. N. Kotopouli, and A. G. Panagos: Neogene volcanoes of Chios, Greece: the relative importance of subduction and back-arc extension / Geological Society, London, Special Publications, 81:213-231, doi:10.1144/GSL.SP.1994.081.01.12 --- Nicholas Petford and Michael P. Atherton: Cretaceous-Tertiary volcanism and syn-subduction crustal extension in northern central Peru / Geological Society, London, Special Publications, 81:233-248, doi:10.1144/GSL.SP.1994.081.01.13 --- Pavel Kepezhinskas: Diverse shoshonite magma series in the Kamchatka Arc: relationships between intra-arc extension and composition of alkaline magmas / Geological Society, London, Special Publications, 81:249-264, doi:10.1144/GSL.SP.1994.081.01.14 --- M. J. Hole, A. D. Saunders, G. Rogers, and M. A. Sykes: The relationship between alkaline magmatism, lithospheric extension and slab window formation along continental destructive plate margins / Geological Society, London, Special Publications, 81:265-285, doi:10.1144/GSL.SP.1994.081.01.15
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  • 2
    Keywords: Antarctica; glacial geology; paleoclimatology; paleoenvironment; Southern Ocean
    Description / Table of Contents: Introduction --- Antarctic Palaeoenvironments and Earth-Surface Processes in context / Michael J. Hambrey and Bethan J. Davies / Geological Society, London, Special Publications, 381, 1-5, 24 September 2013, https://doi.org/10.1144/SP381.27 --- A. Palaeozoic and Mesozoic evolution of the Antarctic Continent --- The geological and tectonic evolution of the Transantarctic Mountains: a review / David H. Elliot / Geological Society, London, Special Publications, 381, 7-35, 1 July 2013, https://doi.org/10.1144/SP381.14 --- Differential Movement across Byrd Glacier, Antarctica, as indicated by Apatite (U–Th)/He thermochronology and geomorphological analysis / D. J. Foley, E. Stump, M. van Soest, K. X. Whipple and K. V. Hodges / Geological Society, London, Special Publications, 381, 37-43, 6 August 2013, https://doi.org/10.1144/SP381.25 --- Mesozoic to recent evolution of intraplate stress fields under multiple remote stresses: The case of Signy Island (South Orkney Microcontinent, Antarctica) / A. Maestro, J. López-Martínez and F. Bohoyo / Geological Society, London, Special Publications, 381, 45-65, 19 April 2013, https://doi.org/10.1144/SP381.4 --- The Taylor Group (Beacon Supergroup): the Devonian sediments of Antarctica / Margaret A. Bradshaw / Geological Society, London, Special Publications, 381, 67-97, 6 August 2013, https://doi.org/10.1144/SP381.23 --- Late Cretaceous dinosaurs from the James Ross Basin, West Antarctica / Marcelo A. Reguero, Claudia P. Tambussi, Rodolfo A. Coria and Sergio A. Marenssi / Geological Society, London, Special Publications, 381, 99-116, 24 July 2013, https://doi.org/10.1144/SP381.20 --- Palaeobiogeography of Austral echinoid faunas: a first quantitative approach / Thomas Saucede, Benjamin Pierrat, Arnaud Brayard and Bruno David / Geological Society, London, Special Publications, 381, 117-127, 19 April 2013, https://doi.org/10.1144/SP381.6 --- B. Cenozoic glaciation and impacts --- Taxonomic diversity of Eocene Antarctic penguins: a changing picture / Piotr Jadwiszczak / Geological Society, London, Special Publications, 381, 129-138, 24 June 2013, https://doi.org/10.1144/SP381.7 --- Heat-flow determinations of basement age in small oceanic basins of the southern central Scotia Sea / P. F. Barker, L. A. Lawver and R. D. Larter / Geological Society, London, Special Publications, 381, 139-150, 19 April 2013, https://doi.org/10.1144/SP381.3 --- Cenozoic landscape and ice drainage evolution in the Lambert Glacier–Amery Ice Shelf system / Duanne A. White / Geological Society, London, Special Publications, 381, 151-165, 1 July 2013, https://doi.org/10.1144/SP381.15 --- History of the grounded ice sheet in the Ross Sea sector of Antarctica during the Last Glacial Maximum and the last termination / Brenda L. Hall, George H. Denton, John O. Stone and Howard Conway / Geological Society, London, Special Publications, 381, 167-181, 19 April 2013, https://doi.org/10.1144/SP381.5 --- Late Eocene Glaciofluvial to Glaciomarine transition in the Lambert Graben: constraints from lithofacies and mineralogy of ODP Site 1166 sediments, Prydz Bay, Antarctica / K. Strand, J. Köykkä and J. Lamminen / Geological Society, London, Special Publications, 381, 183-197, 30 July 2013, https://doi.org/10.1144/SP381.24 --- The Offshore New Harbour Project: deciphering the Middle Miocene through Late Eocene seismic stratigraphy of Offshore New Harbour, western Ross Sea, Antarctica / Stephen F. Pekar, Marvin A. Speece, Gary S. Wilson, David S. Sunwall and Kirsty J. Tinto / Geological Society, London, Special Publications, 381, 199-213, 19 April 2013, https://doi.org/10.1144/SP381.2 --- Constraints on Antarctic Ice Sheet configuration during and following the Last Glacial Maximum and its episodic contribution to sea-level rise / John B. Anderson, Alexandra E. Kirshner and Alexander R. Simms / Geological Society, London, Special Publications, 381, 215-232, 1 July 2013, https://doi.org/10.1144/SP381.13 --- Glaciomarine sedimentation dynamics of the Abbot glacial trough of the Amundsen Sea Embayment shelf, West Antarctica / Katharina Hochmuth and Karsten Gohl / Geological Society, London, Special Publications, 381, 233-244, 24 July 2013, https://doi.org/10.1144/SP381.21 --- Southern Ocean bioproductivity during the last glacial cycle – new detection method and decadal-scale insight from the Scotia Sea / D. Sprenk, M. E. Weber, G. Kuhn, P. Rosén, M. Frank, M. Molina-Kescher, V. Liebetrau and H.-G. Röhling / Geological Society, London, Special Publications, 381, 245-261, 30 July 2013, https://doi.org/10.1144/SP381.17 --- Palaeoenvironmental records from the West Antarctic Peninsula drift sediments over the last 75 ka / Maryline J. Vautravers, David A. Hodell, James E. T. Channell, Claus-Dieter Hillenbrand, Mike Hall, James Smith and Robert D. Larter / Geological Society, London, Special Publications, 381, 263-276, 5 July 2013, https://doi.org/10.1144/SP381.12 --- Provenance of Pleistocene sediments from Site U1359 of the Wilkes Land IODP Leg 318 – evidence for multiple sourcing from the East Antarctic Craton and Ross Orogen / N. C. Pant, P. Biswas, Prakash K. Shrivastava, S. Bhattacharya, Kamlesh Verma, Mayuri Pandey and Iodp Expedition 318 Scientific Party / Geological Society, London, Special Publications, 381, 277-297, 1 July 2013, https://doi.org/10.1144/SP381.11 --- C. Glacial and periglacial processes --- Geomorphological evidence of cold-based glacier activity in South Victoria Land, Antarctica / C. B. Atkins / Geological Society, London, Special Publications, 381, 299-318, 24 July 2013, https://doi.org/10.1144/SP381.18 --- A review of geomorphic processes and landforms in the Dry Valleys of southern Victoria Land: implications for evaluating climate change and ice-sheet stability / D. R. Marchant, S. L. Mackay, J. L. Lamp, A. T. Hayden and J. W. Head / Geological Society, London, Special Publications, 381, 319-352, 1 July 2013, https://doi.org/10.1144/SP381.10 --- Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula / Bethan J. Davies, Neil F. Glasser, Jonathan L. Carrivick, Michael J. Hambrey, John L. Smellie and Daniel Nývlt / Geological Society, London, Special Publications, 381, 353-395, 19 April 2013, https://doi.org/10.1144/SP381.1 --- Windows on Antarctic soil–landscape relationships: comparison across selected regions of Antarctica / Megan R. Balks, Jerónimo López-Martínez, Sergey V. Goryachkin, Nikita S. Mergelov, Carlos E. G. R. Schaefer, Felipe N. B. Simas, Peter C. Almond, Graeme G. C. Claridge, Malcolm Mcleod and Joshua Scarrow / Geological Society, London, Special Publications, 381, 397-410, 16 May 2013, https://doi.org/10.1144/SP381.9 --- Sedimentary processes in two different polar periglacial environments: Examples from Schirmacher Oasis and Larsemann Hills, East Antarctica / Rajesh Asthana, Prakash K. Shrivastava, M. Javed Beg, Ashit K. Swain, Amit Dharwadkar, Sandip K. Roy and Hari B. Srivastava / Geological Society, London, Special Publications, 381, 411-427, 30 July 2013, https://doi.org/10.1144/SP381.22 --- Periglacial processes and landforms of the Antarctic: a review of recent studies and directions / Kevin Hall / Geological Society, London, Special Publications, 381, 429-453, 1 July 2013, https://doi.org/10.1144/SP381.16 --- Palaeoshoreline records of glacial isostatic adjustment in the Dry Valleys region, Antarctica / Stephanie A. Konfal, T. J. Wilson and B. L. Hall / Geological Society, London, Special Publications, 381, 455-467, 30 July 2013, https://doi.org/10.1144/SP381.26 --- Characteristic atmosphere–ocean–solid earth interactions in the Antarctic coastal and marine environment inferred from seismic and infrasound recording at Syowa Station, East Antarctica / Masaki Kanao, Alessia Maggi, Yoshiaki Ishihara, Eleonore Stutzmann, Masa-Yuki Yamamoto and Genti Toyokuni / Geological Society, London, Special Publications, 381, 469-480, 16 May 2013, https://doi.org/10.1144/SP381.8 --- Evaluation of Envisat ASAR IMP imagery for snow mapping at varying spatial resolution (Deception Island, South Shetlands – Antarctica) / Carla Mora, Gonçalo Vieira and Miguel Ramos / Geological Society, London, Special Publications, 381, 481-493, 24 July 2013, https://doi.org/10.1144/SP381.19
    Pages: Online-Ressource (VI, 506 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862396401
    Language: English
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  • 3
    Description / Table of Contents: This volume focuses on magmas and cryospheres on Earth and Mars and is the first publication of its kind to combine a thematic set of contributions addressing the diverse range of volcano-ice interactions known or thought to occur on both planets. Understanding those interactions is a comparatively young scientific endeavour, yet it is vitally important for a fuller comprehension of how planets work as integrated systems. It is also topical since future volcanic eruptions on Earth may contribute to melting ice sheets and thus to global sea level rise. Papers included here are likely to influence the choice of sites for future Mars missions in exobiologically important areas. On Earth, snow and ice are widespread, not only in extensive icecaps but also as alpine glaciers at high elevations in tropical regions. By contrast, Mars today is an arid volcanic planet with only small polar ice-caps although an abundance of water is believed to be trapped in the cryolithosphere. It is also thought that the planet may have sustained extensive frozen oceans early in its history. The presence of a former hydrosphere, a cryosphere and coincident volcanism thus make Mars the likeliest prospect for the first discoveries of life away from Earth. Much research has assumed that terrestrial volcano-ice systems are plausible analogues for putative Martian examples, but until mankind finally sets foot on Mars, there is no simple test for that assumption. Our hope is that the knowledge presented here will stimulate research among planetary geologists in this exciting, rapidly expanding field for many years to come.
    Pages: Online-Ressource (431 Seiten)
    ISBN: 1862391211
    Language: English
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 55 (1993), S. 273-288 
    ISSN: 1432-0819
    Keywords: Volcanism ; subglacial ; lithofacies ; hyaloclastite ; Antarctic Peninsula ; palaeoenvironments
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Isolated, Late Miocene volcanogenic sequences in northern Alexander Island, Antarctic Peninsula, form an unusual, cogenetic association of volcaniclastic, sandy-gravelly lithofacies (including tillites) and volcanic (lava/hyalocalstite) lithofacies. Using simple lithofacies analysis and theoretical considerations of hydrodynamic effects of subglacial eruptions, valley-confined volcanic activity beneth thin, wet-based ice is suggested. The Alexander Island successions are complete enough to be regarded as model sequences for this uncommonly recorded type of eruptive/depositional activity. The sedimentary lithofacies represent resedimented tuffs and meltout or flow tills, which were probably deposited in subglacial ice tunnels eroded or enlarged by volcanically heated meltwater. The volcanic lithofacies formed by the interaction of hot magma with the ice tunnel walls (generating abundant meltwater) and water-saturatedsediments, resulting in the formation of heterogeneous masses of lava and hyaloclastite. There is no obvious sequence organisation in the sedimentary sections. This is probably due to a complex interplay of eruption-related and environmental hydrodynamic factors affecting the relative proportions of water and entrained sediment.
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 258 (1975), S. 701-702 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The geological history of the South Shetland Islands (which includes the Elephant and Clarence Islands group) is dominated by continuing volcanism from the (?) Jurassic to the present2. A structurally deformed sedimentary sequence of presumed Upper Palaeozoic age crops out on Livingston Island3'4. ...
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 56 (1994), S. 361-376 
    ISSN: 1432-0819
    Keywords: Key words volcanism ; stratigraphy ; 40Ar/39Ar geochronology ; migration ; Marie Byrd Land
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Mount Sidley is a complex, polygenetic stratovolcano composed primarily of phonolitic and trachytic lavas and subordinate pyroclastic lithologies at the southern extremity of the Executive Committee Range, a linear chain of volcanoes in central Marie Byrd Land, Antarctica. Detailed field investigation coupled with 14 high precision 40Ar/39Ar age determinations reveal a 1.5 million year life span between 5.7 and 4.2 Ma in which three major phonolitic central vent edifices (Byrd, Weiss and Sidley volcanoes) and their calderas were developed (5.7–4.8 Ma). This was followed (4.6–4.5 Ma) by the eruption of trachytic magmas from multiple vent localities further south, and then by small volume benmoreite-mugearite lavas and tephras around 4.4–4.3 Ma at the southern end of Mount Sidley. The final phase of activity was the eruption of basanite cones at approximately 4.2 Ma. The southward migration of volcanic activity was accompanied by distinct changes in magma composition and is best explained by the sequential release of magmas stored within an intricate system of conduits and chambers in the crust by tectonically driven (magma assisted?) fracture propagation. The style of volcanic migration at Mount Sidley is emulated on a larger scale by other volcanoes in the Executive Committee Range, in which progressive southward displacement of volcanic activity corresponds with significant petrological variations between major centers.
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  • 7
    ISSN: 1432-0819
    Keywords: Key words Lava dome ; Endogenous ; Basaltic ; Submarine ; Rheology ; Antarctica
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  On King George Island during latest Oligocene/earliest Miocene time, submarine eruptions resulted in the emplacement of a small (ca. 500 m estimated original diameter) basalt lava dome at Low Head. The dome contains a central mass of columnar rock enveloped by fractured basalt and basalt breccia. The breccia is crystalline and is a joint-block deposit (lithic orthobreccia) interpreted as an unusually thick dome carapace breccia cogenetic with the columnar rock. It was formed in situ by a combination of intense dilation, fracturing and shattering caused by natural hydrofracturing during initial dome effusion and subsequent endogenous emplacement of further basalt melt, now preserved as the columnar rock. Muddy matrix with dispersed hyaloclastite and microfossils fills fractures and diffuse patches in part of the fractured basalt and breccia lithofacies. The sparse glass-rich clasts formed by cooling-contraction granulation during interaction between chilled basalt crust and surrounding water. Together with muddy sediment, they were injected into the dome by hydrofracturing, local steam fluidisation and likely explosive bulk interaction. The basalt lava was highly crystallised and degassed prior to extrusion. Together with a low effusion temperature and rapid convective heat loss in a submarine setting, these properties significantly affected the magma rheology (increased the viscosity and shear strength) and influenced the final dome-like form of the extrusion. Conversely, high heat retention was favoured by the degassed state of the magma (minimal undercooling), a thick breccia carapace and viscous shear heating, which helped to sustain magmatic (eruption) temperatures and enhanced the mobility of the flow.
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  • 8
    ISSN: 1432-0819
    Keywords: Key words Volcanism ; Lithofacies ; Surtseyan ; Hyaloclastite ; Antarctic ; Englacial
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Pliocene–Recent volcanic outcrops at Seal Nunataks and Beethoven Peninsula (Antarctic Peninsula) are remnants of several monogenetic volcanoes formed by eruption of vesiculating basaltic magma into shallow water, in an englacial environment. The diversity of sedimentary and volcanic lithofacies present in the Antarctic Peninsula outcrops provides a clear illustration of the wide range of eruptive, transportational and depositional processes which are associated with englacial Surtseyan volcanism. Early-formed pillow lava and glassy breccia, representing a pillow volcano stage of construction, are draped by tephra erupted explosively during a tuff cone stage. The tephra was resedimented around the volcano flanks, mainly by coarse-grained sediment gravity flows. Fine-grained lithofacies are rare, and fine material probably bypassed the main volcanic edifice, accumulating in the surrounding englacial basin. The pattern of sedimentation records variations in eruption dynamics. Products of continuous-uprush eruptions are thought to be represented by stacks of poorly bedded gravelly sandstone, whereas better bedded, lithologically more diverse sequences accumulated during periods of quiescence or effusive activity. Evidence for volcano flank failure is common. In Seal Nunataks, subaerial lithofacies (mainly lavas and cinder cone deposits) are volumetrically minor and occur at a similar stratigraphical position to pillow lava, suggesting that glacial lake drainage may have occurred prior to or during deposition of the subaerial lithofacies. By contrast, voluminous subaerial effusion in Beethoven Peninsula led to the development of laterally extensive stratified glassy breccias representing progradation of hyaloclastite deltas.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 56 (1994), S. 361-376 
    ISSN: 1432-0819
    Keywords: volcanism ; stratigraphy ; 40Ar/39Ar geochromology ; migration ; Marie Byrd Land
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Mount Sidley is a complex, polygenetic stratovolcano composed primarily of phonolitic and trachytic lavas and subordinate pyroclastic lithologies at the southern extremity of the Executive Committee Range, a linear chain of volcanoes in central Marie Byrd Land, Antarctica. Detailed field investigation coupled with 14 high precision 40Ar/39Ar age determinations reveal a 1.5 million year life span between 5.7 and 4.2 Ma in which three major phonolitic central vent edifices (Byrd, Weiss and Sidley volcanoes) and their calderas were developed (5.7–4.8 Ma). This was followed (4.6–4.5 Ma) by the eruption of trachytic magmas from multiple vent localities further south, and then by small volume benmoreite-mugearite lavas and tephras around 4.4–4.3 Ma at the southern end of Mount Sidley. The final phase of activity was the eruption of basanite cones at approximately 4.2 Ma. The southward migration of volcanic activity was accompanied by distinct changes in magma composition and is best explained by the sequential release of magmas stored within an intricate system of conduits and chambers in the crust by tectonically driven (magma assisted?) fracture propagation. The style of volcanic migration at Mount Sidley is emulated on a larger scale by other volcanoes in the Executive Committee Range, in which progressive southward displacement of volcanic activity corresponds with significant petrological variations between major centers.
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  • 10
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    In:  Geological Society Special Publication 219: 285-313.
    Publication Date: 2003-01-01
    Description: The South Sandwich Islands are one of the world's classic examples of an intraoceanic arc. Formed on recently generated back-arc crust, they represent the earliest stages of formation of arc crust, and are an excellent laboratory for investigating variations in magma chemistry resulting from mantle processes, and generation of silicic magmas in a dominantly basaltic environment. Two volcanoes are examined. Southern Thule in the south of the arc is a complex volcanic edifice with three calderas and compositions that range from mafic to silicic and tholeiitic to calc-alkaline. It is compared to the Candlemas-Vindication edifice in the north of the arc, which is low-K tholeiitic and strongly bimodal from mafic to silicic. Critically, Southern Thule lies along a cross-arc, wide-angle seismic section that reveals the velocity structure of the underlying arc crust. Trace element variations are used to argue that the variations in both mantle depletion and input of a subducted sediment component produced the diverse low-K tholeiite, tholeiite and calc-alkaline series. Primitive, mantle-derived melts fractionally crystallized by c. 36% to produce the most Mg-rich erupted basalts and a high-velocity cumulitic crustal keel. Plagioclase cumulation produced abundant high-Al basalts (especially in the tholeiitic series), and strongly influenced Sr abundances in the magmas. However, examination of volumetric and geochemical arguments indicates that the silicic rocks do not result from fractional crystallization, and are melts of amphibolitic arc crust instead.
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