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  • AND-2A; ANDRILL; Antarctic Geological Drilling; DRILL; Drilling/drill rig; International Polar Year (2007-2008); IPY; McMurdo Sound; McMurdo Station; SMS; Southern McMurdo Sound  (1)
  • OIB  (1)
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  • 1
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    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
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  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © The Author, 2006. This is the author's version of the work. It is posted here by permission of Oxford University Press for personal use, not for redistribution. The definitive version was published in Journal of Petrology 27 (2006): 1673-1704, doi:10.1093/petrology/egl024.
    Description: This paper presents field, geochemical and isotopic (Sr, Nd, Pb) results on basalts from the Antipodes, Campbell and Chatham Islands, New Zealand. New 40Ar/39Ar age determinations along with previous K-Ar dates reveal three major episodes of volcanic activity on Chatham Island (85-82, 41-35, ~5 Ma). Chatham and Antipodes samples comprise basanite, alkali and transitional basalts that have HIMU-like isotopic (206Pb/204Pb 〉20.3-20.8, 87Sr/86Sr 〈0.7033, 143Nd/144Nd 〉0.5128) and trace element affinities (Ce/Pb 28-36, Nb/U 34-66, Ba/Nb 4-7). The geochemistry of transitional to Q-normative samples from Campbell Island is explained by interaction with continental crust. The volcanism is part of a long-lived (~100 Myr), low-volume, diffuse alkaline magmatic province that includes deposits on the North and South Islands as well as portions of West Antarctica and SE Australia. All of the continental areas were juxtaposed on the eastern margin of Gondwanaland at 〉83 Ma. A ubiquitous feature of mafic alkaline rocks from this region is their depletion in K and Pb relative to other highly incompatible elements when normalized to primitive mantle values. The inversion of trace element data indicates enriched mantle sources that contain variable proportions of hydrous minerals. We propose that the mantle sources represent continental lithosphere that host amphibole/phlogopite-rich veins formed by plume and/or subduction related metasomatism between 500 and 100 Ma. The strong HIMU signature (206Pb/204Pb 〉20.5) is considered to be an in-grown feature generated by partial-dehydration and loss of hydrophile elements (Pb, Rb, K) relative to more magmaphile elements (Th, U, Sr) during short-term storage at the base of the lithosphere.
    Description: This study was supported by National Science Foundation Grants OPP-9419686 and OPP-0003702 awarded to KSP.
    Keywords: Continental alkaline basalts ; Mantle metasomatism ; OIB ; HIMU ; Sr, Nd and Pb isotopes ; West Antarctica ; New Zealand ; Lithospheric mantle
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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