1986
DOI: 10.1029/ar036p0339
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The Beacon Supergroup (Devonian-Triassic) and Ferrar Group (Jurrasic) in the Beardmore Glacier area, Antarctica

Abstract: Are there petroleum resources in Antarctica?, by John C. Behrendt. in pre-break-up Triassic strata, to intracontinental rocks of the Beacon Supergroup and Ferrar. Group. These flat-lying rocks are especially wide-in the Beardmore Glacier area locality 69, fig. in the Devonian through Jurassic Beacon Super-. PaleoTerra: Devonian Lithological Database: Sources A-G basin antarctica terra: Topics by E-print Network-OSTI The Beacon Supergroup Devonian-Triassic and. Ferrar Group Jurassic in the Beardmore Glacier are… Show more

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Cited by 119 publications
(132 citation statements)
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“…and are within the upper Buckley Formation (Barrett et al 1986; for additional locality information, see Ryberg 2010). Specimens were cut into slabs with a lapidary saw and then immersed in hydrofluoric acid (49%) to dissolve the silica.…”
Section: Methodsmentioning
confidence: 99%
“…and are within the upper Buckley Formation (Barrett et al 1986; for additional locality information, see Ryberg 2010). Specimens were cut into slabs with a lapidary saw and then immersed in hydrofluoric acid (49%) to dissolve the silica.…”
Section: Methodsmentioning
confidence: 99%
“…An additional specimen was collected from Triassic Fremouw Formation strata at the base of Mount Falla, also in the Beardmore Glacier area (Barrett et al 1986). Peat blocks were cut into sections, and the flat surfaces were polished and then etched in 48%-50% hydrofluoric acid.…”
Section: Methodsmentioning
confidence: 99%
“…Early Middle Triassic (Anisian) for Fremouw Peak (Farabee et al 1990), Triassic at Mt. Falla (Barrett et al 1986).…”
Section: Order-cycadalesmentioning
confidence: 99%
“…The LP1 and LP2 apparently were more productive than the other contemporaneous forests that developed under similar paleoclimate, paleoenvironmental and soil nutrient conditions, which were enhanced by the occurrence of volcanic rock fragments in the sand (Barrett et al, 1986;Isbell, 1990).…”
mentioning
confidence: 99%
“…The Permian sequence consists of: 1) glacigenic, primarily glacial marine and glacial lacustrine deposits recording Gondwanan glaciation (Pagoda Formation, Isbell et al, 1997;; 2) shale and interbedded sandstone deposited in a large post-glacial lake or series of lakes filled by deltaic sediments (Mackellar Formation and lowermost Fairchild Formation, Miller, M.F., et al, 2010); 3) crossbedded sandstone lacking plant fossils deposited in braided stream channels (bulk of Fairchild Formation, Barrett et al, 1986); and sandstone, siltstone, shale and coal deposited in braided stream systems (Buckley Formation, Isbell, 1990;Isbell et al, 1997;Gulbranson et al, 2012Gulbranson et al, , 2014. The amount of plant material and the thickness and extent of coal increases upward within the Buckley Formation.…”
mentioning
confidence: 99%