1973
DOI: 10.1130/0016-7606(1973)84<773:scismt>2.0.co;2
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Syntectonic Conglomerates in Southwestern Montana: Their Nature, Origin, and Tectonic Significance

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Cited by 49 publications
(109 citation statements)
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“…), and resultant implications for the tectonic history of this part of the Cordillera are the subjects of our ongoing research. Preliminary results suggest that the character of the subBeaverhead unconformity changes laterally from the back Ryder and Scholten (1973) with interbedded quarzite-clast conglomerates and lithologies typical ofthe Aspen Formation.…”
Section: Introductionmentioning
confidence: 99%
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“…), and resultant implications for the tectonic history of this part of the Cordillera are the subjects of our ongoing research. Preliminary results suggest that the character of the subBeaverhead unconformity changes laterally from the back Ryder and Scholten (1973) with interbedded quarzite-clast conglomerates and lithologies typical ofthe Aspen Formation.…”
Section: Introductionmentioning
confidence: 99%
“…They stated that their Aspen Formation is overlain with profound angular unconformity by the Beaverhead Formation in the Lima region (Scholten and others, 1955, p. 368). Ryder and Scholten (1973) discussed the basal Beaverhead contact in detail, but their basal Beaverhead is equivalent in part to rocks that we consider to be either Frontier Formation or the underlying Blackleaf Formation ( fig. 1 ).…”
Section: Stratigraphic Nomenclature and Contact Relationshipsmentioning
confidence: 99%
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