Basaltic maar-diatreme volcanism in the Lower Carboniferous of the Limerick Basin (SW Ireland)
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  • 作者:H. A. L. Elliott ; T. M. Gernon ; S. Roberts ; C. Hewson
  • 关键词:Maar ; diatremes ; Phreatomagmatic ; Lower Carboniferous ; Shallow marine environment
  • 刊名:Bulletin of Volcanology
  • 出版年:2015
  • 出版时间:May 2015
  • 年:2015
  • 卷:77
  • 期:5
  • 全文大小:7,714 KB
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  • 作者单位:H. A. L. Elliott (1)
    T. M. Gernon (1)
    S. Roberts (1)
    C. Hewson (2)

    1. Ocean and Earth Science, National Oceanography Centre, Southampton, University of Southampton, Southampton, SO14 3ZH, UK
    2. Teck Ireland Ltd, The Murrough, Wicklow, Ireland
  • 刊物主题:Geology; Geophysics/Geodesy; Mineralogy; Sedimentology;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1432-0819
文摘
Lead-zinc exploration drilling within the Limerick Basin (SW Ireland) has revealed the deep internal architecture and extra-crater deposits of five alkali-basaltic maar-diatremes. These were emplaced as part of a regional north-east south-west tectonomagmatic trend during the Lower Carboniferous Period. Field relationships and textural observations suggest that the diatremes erupted into a shallow submarine environment. Limerick trace element data indicates a genetic relationship between the diatremes and extra-crater successions of the Knockroe Formation, which records multiple diatreme filling and emptying cycles. Deposition was controlled largely by bathymetry defined by the surrounding Waulsortian carbonate mounds. An initial non-diatreme forming eruption stage occurred at the water-sediment interface, with magma-water interaction prevented by high magma ascent rates. This was followed by seawater incursion and the onset of phreatomagmatic activity. Magma-water interaction generated poorly vesicular blocky clasts, although the co-occurrence of plastically deformed and highly vesicular clasts indicate that phreatomagmatic and magmatic processes were not mutually exclusive. At a later stage, the diatreme filled with a slurry of juvenile lapilli and country rock lithic clasts, homogenised by the action of debris jets. The resulting extra-crater deposits eventually emerged above sea level, so that water ingress significantly declined, and late-stage magmatic processes became dominant. These deposits, largely confined to the deep vents, incorporate high concentrations of partially sintered globular and large ‘raggy’ lapilli showing evidence for heat retention. Our study provides new insights into the dynamics and evolution of basaltic diatremes erupting into a shallow water (20–120 m) submarine environment.

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