Lexicon of Antarctic Stratigraphic Names Introduced by Members of United States Expeditions (1972) / Chapter Skim
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Pages 121-131
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Unnamed MOuntains tuff 1. Firat published use Doumani , G .
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b . Lithology Dark-colored , fine -grained a late with one major and two minor cleavages .
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Welcome MOuntain metasedimentary rocks 1 . Firat published use Weihaupt , J .
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4 . Remarks a.
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d . Relation to other units Overlies Crashs ite Quartz ite(Devonia� conformab ly OVerlain (poss ibly dis conformably)
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formation is well exposed along a ridge ves t of the sumadt . The type section is located on the southeas ternmos t part of E lliott Ridge , where the Wiens Formation conformably overlies the Gamba cor ta Formation and is d is conformably overlain by the E lliott Sands tone .
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3 . body , which intrudes the migmatite .
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2 . Definition The section begins with a very th in discontinuous conglomerate , whiCh grades into a sands tone ranging in thickness from 5 1 - 100 1 in outcrops West of Windy Gully .
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of the Scott Glacier , the format ion varies in metamorphic grade in a south to north direction from unaltered pyroclas tics to rocks of the biotite zone . " (Minshew , 110)
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