title: Antarctica: Geology of the Ellsworth Mountains.
abstract: Geologic reconnaissance indicates that the Ellsworth Mountains consist mainly of thousands of feet of folded, slightly metamorphosed, clastic sedimentary rocks of unknown age. Three major stratigraphic units are recognized, but only fragmentary fossils have been found. The folding is asymmetric, overturned, or recumbent; fold axes strike north, 10 degrees to 20 degrees west. Basic igneous sills occur in the northern Heritage Range.
authors.forename: J J
authors.initials: JJ
authors.lastname: Anderson
authors.forename: T W
authors.initials: TW
authors.lastname: Bastien
authors.forename: P G
authors.initials: PG
authors.lastname: Schmidt
authors.forename: J F
authors.initials: JF
authors.lastname: Splettstoesser
authors.forename: C
authors.initials: C
authors.lastname: Craddock