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Austinville Member

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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...
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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...
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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...
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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...
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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...
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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...
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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...
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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...
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