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                                       Details for article 11 of 13 found articles
 
 
  Stratigraphy of the Lamington Volcanics in far Northeastern New South Wales
 
 
Title: Stratigraphy of the Lamington Volcanics in far Northeastern New South Wales
Author: Duggan, M. B.
Mason, D. R.
Appeared in: Australian journal of earth sciences
Paging: Volume 25 (1978) nr. 1-2 pages 65-73
Year: 1978-03
Contents: The stratigraphic nomenclature for the Lamington Volcanics in the southern part of the Tweed Shield Volcano is revised. An alkaline formation (the Kyogle Basalt) containing discontinuous rhyolitic-agglomerate (the Homeleigh Agglomerate Member) and rhyolite flow (the Georgica Rhyolite Member) horizons is the basal unit of the volcanic succession. The Kyogle Basalt thins eastward where it is overlain by a subalkaline sequence comprising the Lismore Basalt, Nimbin Rhyolite, and Blue Knob Basalt respectively. The Lismore Basalt is composed predominantly of tholeiitic andesite with minor icelandite and sporadic flows of mildly alkaline rocks; tholeiitic andesites predominate in the Blue Knob Basalt. The Nimbin Rhyolite consists of rhyolite flows, and a relatively minor pyroclastic component (principally lapilli tuff).
Publisher: Taylor & Francis
Source file: Elektronische Wetenschappelijke Tijdschriften
 
 

                             Details for article 11 of 13 found articles
 
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