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  • 1
    Monograph available for loan
    Monograph available for loan
    Volcanological and environmental studies of Mount Erebus, Antarctica (1994)
    Washington : American Geophysical Union
    Associated volumes
    Details Availability
    Call number: 13/M 95.0646
    In: Antarctic research series
    Type of Medium: Monograph available for loan
    Pages: xiv, 162 S.
    ISBN: 0875908756
    ISSN: 0066-4634
    Series Statement: Antarctic research series 66
    Classification:
    B.2.2.
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Volcanological and Environmental Studies of Mount Erebus, Antarctica (1994)
    Washington : AGU
    Associated volumes
    Details Availability
    Call number: AWI G9-95-0112
    In: Antarctic research series
    Type of Medium: Monograph available for loan
    Pages: XIV, 162 S. : Abb. ; 27 cm
    ISBN: 0875908756
    ISSN: 0066-4634
    Series Statement: Antarctic research series 66
    Branch Library: AWI Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Electron microprobe analysis of minerals in core samples from Dry Valley Drilling Project (DVDP) holes 1 and 2, Ross Island, Antarctica (1974)
    Wellington
    Associated volumes
    Details Availability
    Call number: MR 90.1065
    In: Department of Geology publication / Victoria University of Wellington
    Type of Medium: Monograph available for loan
    Pages: 27 S.
    Series Statement: Department of Geology publication / Victoria University of Wellington 4
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
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    Monitoring rapid temporal change in a volcano with coda wave interferometry (2005)
    In:  Geophys. Res. Lett., Hannover, Dt. Geophys. Ges. e. V., vol. 32, no. 6, pp. 77-91, pp. L06304, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 2005
    Keywords: Volcanology ; Wave propagation ; Real time earthquake monitoring ; Seismology ; GRL ; Gret
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Eruptive history and magmatic stability of Erebus volcano, Antarctica: Insights from englacial tephra (2014)
    Wiley
    Details
    Publication Date: 2014-10-09
    Description: A tephrostratigraphy of the active Antarctic volcano, Mt. Erebus, was determined from englacial tephra on the ice-covered flanks of Erebus and an adjacent volcano. The tephra are used to reconstruct the eruptive history and magmatic evolution of Erebus. More fine grained and blocky particles define tephra formed in phreatomagmatic eruptions and larger fluidal shards are characteristic of magmatic eruptions and in some cases both eruptive types are identified in a single mixed tephra. The eruptions forming the mixed tephra likely started as phreatomagmatic eruptions which transitioned into Strombolian eruptions as the non-magmatic water source was exhausted. We reconstructed the eruptive history of Erebus using the tephra layers stratigraphic position, 40 Ar/ 39 Ar ages, shard morphology and grain size. Major and trace element analyses of individual glass shards were measured by electron probe microanalysis and LA-ICP-MS. Trachybasalt, trachyte and phonolite tephra were identified. All phonolitic tephra are Erebus-derived with compositions similar to volcanic bombs erupted from Erebus over the past 40 years. The tephra show that Erebus magma has not significantly changed for 40ka. The uniformity of the glass chemical composition implies that the phonolite magma has crystallized in the same manner without change throughout the late Quaternary, suggesting long-term stability of the Erebus magmatic system. Trachyte and trachybasalt tephra were likely erupted from Marie Byrd Land and the McMurdo Sound area, respectively. The trachytic tephra can be regionally correlated, and could provide an important time-stratigraphic marker in Antarctic ice cores.
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
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    Backward tracking of gas chemistry measurements at Erebus volcano (2012)
    Wiley
    Details
    Publication Date: 2012-11-22
    Description: Erebus volcano in Antarctica offers an exceptional opportunity to probe the dynamics of degassing – its behavior is characterized by an active lava lake through which sporadic Strombolian eruptions occur. Here, we develop a framework for interpreting contrasting degassing signatures measured at high temporal resolution, which integrates physical scenarios of gas/melt separation into a thermodynamic model that includes new volatile solubility data for Erebus phonolite. In this widely applicable framework, the measured gas compositions are backtracked from surface to depth according to physical templates involving various degrees of separation of gas and melt during ascent. Overall, explosive signatures can be explained by large bubbles (gas slugs) rising slowly in equilibrium from at least 20 bars but at most a few hundred bars in a magmatic column closer to the stagnant end-member than the convecting end-member. The span of explosive signatures can be due to various departure depths and/or slug acceleration below a few tens of bars. Results also reveal that explosive gases last equilibrated at temperatures up to 300°C colder than the lake due to rapid gas expansion just prior to bursting. This picture (individual rise of gas and melt batches from a single, potentially very shallow phonolitic source) offers an alternative to the conclusions of previous work based on a similar data set at Erebus, according to which differences between quiescent and explosive gas signatures are due to the decompression of two deep, volatile-saturated sources that mixed to various degrees (phonolite at 1–3 kbar and basanite at 5–8 kbar).
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 7
    Electronic Resource
    Electronic Resource
    XRF AND INAA DETERMINATIONS OF MAJOR AND TRACE ELEMENTS IN GEOLOGICAL SURVEY OF JAPAN IGNEOUS AND SEDIMENTARY ROCK STANDARDS (1993)
    Oxford, UK : Blackwell Publishing Ltd
    Geostandards and geoanalytical research 17 (1993), S. 0 
    Details
    ISSN: 1751-908X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Major and trace element analyses have been obtained by wavelength dispersive X-ray fluorescence for the Geological Survey of Japan Igneous rock series and selected samples from the Sedimentary rock series reference samples. Additional trace element data for the Igneous rock series were obtained by instrumental neutron activation analysis. Samples were analyzed multiple times for 10 major elements (with loss-on-ignition) and the following trace elements; As, Ba, Ce, Co, Cr, Cs, Cu, Eu, Ga, Hf, La, Lu, Nb, Nd, Ni, Pb, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Th, U, V, W, Y, Yb, Zn and Zr.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1751-908X.1993.tb00128.x
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  • 8
    Electronic Resource
    Electronic Resource
    Rates of sulfur dioxide and particle emissions from White Island volcano, New Zealand, and an estimate of the total flux of major gaseous species (1986)
    Springer
    Bulletin of volcanology 48 (1986), S. 181-188 
    Details
    ISSN: 1432-0819
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Airborne correlation spectrometry (COSPEC) was used to measure the rate of SO2 emission at White Island on three dates, i.e., November 1983, 1230 ± 300 t/d; November 1984, 320 ± 120 t/d; and January 1985, 350 ± 150 t/d (t = metric tons). The lower emission rates are likely to reflect the long-term emission rates, whereas the November 1983 rate probably reflects conditions prior to the eruption of December 1983. The particle flux in the White Island plume, as determined with a quartz crystal microbalance/cascade in November 1983, was 1.3 t/d, unusually low for volcanic plumes. The observed plume particles, as shown from scanning electron microscopy, include halite, native sulfur, and silicates and are broadly similar to other volcanic plumes. Gas analyses from high-temperature volcanic fumaroles collected from June 1982 through November 1984 werde used together with the COSPEC data to estimate the flux of other gas species from White Island. The rates estimated are indicative of the long-term volcanic emission, i.e., 8000–9000 t/d H2O, 900–1000 t/d CO2, 70–80 t/d HCl, 1.5–2 t/d HF, and about 0.2 t/d NH3. The long-term thermal power output at White Island is estimated at about 400 MW.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01087672
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  • 9
    Electronic Resource
    Electronic Resource
    Rate of sulphur dioxide emission from Erebus volcano, Antarctica, December 1983 (1985)
    [s.l.] : Nature Publishing Group
    Nature 316 (1985), S. 710-712 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Mt Erebus is the only active and the largest of three volcanoes which form the bulk of Ross Island, in the Ross Sea (77.55 S, 167.17 E). It is made up chiefly of anorthoclase phonolite lavas and has sustained an active lava lake, at least since 1972, and possibly for more than a century. Most of ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/316710a0
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  • 10
    Electronic Resource
    Electronic Resource
    Development of heterogeneities in the subcontinental Mantle: Evidence from the Ferrar Group, Antarctica (1980)
    Springer
    Contributions to mineralogy and petrology 73 (1980), S. 89-104 
    Details
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Tholeiitic lava flows (Kirkpatrick Basalts) and dolerite sills and dikes (Ferrar Dolerites) of the Jurassic Ferrar Group from Antarctica and dolerite sills from Tasmania, Australia are characterised by initial strontium isotope ratios ranging from 0.7089 to 0.7153. The mean and standard deviation of 85 analyses is 0.7115±0.0012. Some of the scatter in the initial 87Sr/86Sr ratios can be attributed to sample inhomogeneity, analytical uncertainties and sample alteration. The published major element data show well-defined trends that are consistent with an evolution by fractional crystallization. Recognition of a parental magma is difficult due to the fractionated nature of the rocks. Trace element analyses, particularly the rare earth elements (REE) support a differentiation model. Compared to mid-ocean ridge basalts, Ferrar Group rocks are enriched in light REE. Kirkpatrick Basalts from the central Transantarctic Mountains show significant correlations between initial 87Sr/86Sr ratios and major elements only for SiO2 and CaO. The general lack of strong correlation is the basis for rejecting the possibility of wholesale contamination by sialic material as a possible cause of the high 87Sr/86Sr ratios. Selective contamination of the basaltic magmas is a possibility and cannot be completely discounted. It would probably involve a fluid phase in order to transport and mix the light REE, Rb, 87Sr, and other elements. By analogy with selective contamination of ocean ridge basalts by sea water it is difficult to envisage a similar process acting on magma emplaced in a non-marine environment. Because of the elevated values of the initial 87Sr/86Sr ratios, their similar average value over 2,500 km and the large volume of magma involved (4× 105 km3) a mantle origin for the high Sr ratios is preferred. Models to account for the enrichment of Rb and light REE in the Antarctic mantle during or prior to the Jurassic include: 1. addition of continental material from a Palezoic Mesozoic subduction zone; 2. metasomatism of volatile elements from the lower mantle; and 3. evolution of a mantle with a high Rb/Sr ratio.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00376262
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