Austinville Member

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 March 1980
Journal of Sedimentary Research (1980) 50 (1): 91–116.
... of Lower Paleozoic platform margin. The upward-shallowing platform sequence consists of shallow subtidal ribbon-laminated carbonates (Patterson Member) overlain by shoal water to tidal flat massive dolomites and fenestral cryptalgal carbonates (Austinville and Ivanhoe Members) that pass up into red...
Series: Memoir, Memoir
Published: 01 January 2012
DOI: 10.1306/13331500M983500
EISBN: 9781629810201
... ramp carbonates similar to those in the lower part of the Sauk I supersequence (sequence 2 of Read, 1989 ) in Virginia (Patterson Creek and Austinville Members of the Shady Dolomite) and Pennsylvania (Vintage Formation). The mottled fabric of the Bolivar Heights Member is unquestionably the product...
FIGURES | View All (22)
Journal Article
Published: 01 September 2014
Journal of Paleontology (2014) 88 (5): 906–924.
... bioclastic grainstone deposited in an inner shelf setting. The El Estero Member and the basal 0.2 m of the Soldano Member contain a trilobite fauna of olenelloids and ‘simple' ptychoparioids indicative of the early Cambrian (series 2, stage 4; Dyeran stage of Laurentia). The succeeding 50 m of the lower...
FIGURES | View All (12)
Series: Memoir, Memoir
Published: 01 January 2012
DOI: 10.1306/13331499M980271
EISBN: 9781629810201
...-stone overlain by mud-mound facies. The Patterson Member is overlain by the Austinville Member of the Shady Dolomite, a shallow-water, white, massive, locally oolitic dolomite and cyclic dolomite with at least three thin quartzose units that mark a significant low-stand at the base of the second...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1974
AAPG Bulletin (1974) 58 (4): 575–620.
... conglomerate ( Fig. 4 ) of the Diamond Hill member ( Lowry et al. , 1972 ) are interbedded with graptolite-bearing black shales approximately 1,000 ft above the base of the Liberty Hall Formation ( Fig. 3 ). The clasts ( Fig. 5 ) tend toward the discoidal and range in diameter to more than two ft. Conodonts...
FIGURES | View All (8)
Journal Article
Published: 01 July 2009
Journal of Paleontology (2009) 83 (4): 524–547.
... southwards into the northern Delamar Mountains ( Fig. 1 inset). The bed lies less than 2 meters below the Dyeran-Delamaran boundary (the traditional “Lower-Middle Cambrian” boundary of Laurentia) in the upper part of the Combined Metals Member of the Pioche Formation ( Sundberg and McCollum, 2000...
FIGURES | View All (19)
Journal Article
Published: 17 December 2007
Canadian Journal of Earth Sciences (2007) 44 (12): 1661–1673.
... than ore,” making it similar to the Austinville–Ivanhoe, Daniels Harbor, and Robb Lake Mississippi Valley-type (MVT) deposits. The paleomagnetic fold test indicates ∼70% postfolding ChRMs for host dolostone and dolomite and for YO and JO Zn–Pb mineralization sites that are statistically...
FIGURES | View All (11)
Journal Article
Published: 01 May 2018
Journal of Paleontology (2018) 92 (3): 442–458.
... Formation, as noted by Landing (2007, 2012 , and references therein). Landing (2007, 2012 ) also reported an unidentifiable trilobite fragment from the top of the Bomoseen Member of the Nassau Formation in the Taconics of New York State, which is believed to be age-equivalent to the upper Pinnacle...
FIGURES | View All (4)
Series: Economic Geology, Economic Geology
Published: 01 January 2005
DOI: 10.5382/AV100.18
EISBN: 9781934969519
Journal Article
Journal: Economic Geology
Published: 01 May 2010
Economic Geology (2010) 105 (3): 593–625.
... endowment and the salinity and temperature of the fluid inclusions in ore minerals ( Leach et al., 2005b ). Discussions on the geochemistry of sediment-hosted Pb-Zn ore fluids generally refer to end-member compositions based on the dominant redox state of sulfur. Oxidized sedimentary brines are those...
FIGURES | View All (19)