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Austinville

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Journal Article
Journal: Economic Geology
Published: 01 November 1981
Economic Geology (1981) 76 (7): 2012–2017.
...Nora K. Foley; A. Krishna Sinha; James R. Craig Abstract Lead isotopic studies from the Austinville-Ivanhoe district of southwest Virginia demonstrate that galenas of different generation have distinct lead isotopic compositions. Within a single orebody paragenetically early galenas have lower lead...
Journal Article
Journal: GSA Bulletin
Published: 01 June 1956
GSA Bulletin (1956) 67 (6): 683–696.
...H. V McMURRY; A. D HOAGLAND Abstract Applied potential data from diamond-drill holes at Austinville, Virginia, have shown that the host rocks of the ore bodies are of extremely high resistivity and are strongly anisotropic. Triaxial anisotropy is prominent and is thought to be controlled...
Journal Article
Journal: Economic Geology
Published: 01 June 1935
Economic Geology (1935) 30 (4): 425–433.
Journal Article
Journal: Economic Geology
Published: 01 July 1979
Economic Geology (1979) 74 (4): 908–918.
Journal Article
Published: 01 March 1980
Journal of Sedimentary Research (1980) 50 (1): 91–116.
...R. W. Pfeil; J. F. Read Abstract Shelf edge, foreslope, and slope facies in the Lower to Middle Cambrian Shady Dolomite (600-1300 m thick) are exposed southeast of Austinville, southwestern Virginia, Valley and Ridge Province of the Appalachians. The Shady-Rome beds constitute an important type...
Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 1977
DOI: 10.2110/pec.77.25.0083
EISBN: 9781565761551
... canyons are local features at or near the carbonate shelf margin. The composition and organization of breccia deposits and surrounding rocks in the Shady Dolomite (Lower and Middle Cambrian) near Austinville, Virginia, in the Kinzers Formation (Lower and Middle Cambrian) near Thomasville, Pennsylvania...
Journal Article
Journal: Economic Geology
Published: 01 May 1994
Economic Geology (1994) 89 (3): 493–514.
... and, as such, define a positive thermal anomaly. Host rocks to the Austinville-Ivanhoe, northern Newfoundland, and Robb Lake deposits (group 3) revealed the highest color alteration index values of North American Mississippi Valley-type districts, with host-rock temperatures greatly exceeding ore mineral fluid...
Journal Article
Journal: Economic Geology
Published: 01 April 1994
Economic Geology (1994) 89 (2): 307–321.
... clusters, whereas barite, fluorite, and sparry dolomite compositions are more scattered. These lead isotope compositions reflect the distribution of the deposits, which are hosted by two main palcoaquifers. Lower Cambrian clastic and carbonate rocks host the Austinville (Zn-Pb), Cartersville (Ba...
Book Chapter

Author(s)
Ernest L. Ohle
Series: DNAG, Geology of North America
Published: 01 January 1991
DOI: 10.1130/DNAG-GNA-P2.43
EISBN: 9780813754697
... New Orleans, localities where lead mineralization cropped out soon attracted attention and became population centers. The Wisconsin-Illinois District (discovered in 1682), southeast Missouri (1720), Austinville, Virginia (1750), and Rosiclaire, Illinois (1830), are notable examples. There were also...
Journal Article
Journal: GSA Bulletin
Published: 01 March 1990
GSA Bulletin (1990) 102 (3): 391–404.
...ROGER J. BARNABY; J. FRED READ Abstract Drill cores through the Lower to Middle Cambrian Shady Dolomite carbonate platform (600 to 1,200 m thick) in the Austinville, Virginia, region have provided critical platform-margin facies relations not exposed in outcrop. The control provided by the closely...
Journal Article
Published: 01 August 1983
American Mineralogist (1983) 68 (7-8): 845–848.
...Michael E. Fleet; Mizuhiko Akizuki Abstract Several years ago, following studies of ZnS minerals from Pribram, Czechoslovakia, Thomaston Dam, Connecticut and Austinville, Virginia (Fleet, 1976; 1977a; 1977b), I concluded that in natural (low temperature) assemblages; (1) complete transformation...
Journal Article
Published: 01 June 1977
American Mineralogist (1977) 62 (5-6): 540–546.
... by inversion of a more wurtzitic precursor. In contrast, solid-state transformation in ideal 3 C sphalerite is limited to the formation of deformation twins ([111] twin axis). This is illustrated by X-ray diffraction study of a deformed sphalerite from Austinville, Virginia. Copyright © 1977...
Journal Article
Journal: Economic Geology
Published: 01 August 1971
Economic Geology (1971) 66 (5): 805–810.
... classified. With the exception of the Austinville-type deposits, which will not be considered herein, the subject deposits are related to a Lower Ordovician paleoaquifer. The classic examples are Friedensville, Pennsylvania; Timberville (Shenandoah Valley), Virginia; Mascot-Jefferson City district, Tennessee...
Journal Article
Journal: Economic Geology
Published: 01 November 1950
Economic Geology (1950) 45 (7): 654–670.
... of zinc content of the soil to the underlying ore bodies has been studied including consideration of the influence of depth of ore, nature of soil cover, mineralization in rock above ore, faults and fractures, and ground water circulation. The field work was conducted at Austinville, Virginia...
Image
Grade-tonnage for 113 MVT deposits and 10 districts. Diagonal lines represe...
Published: 01 May 2010
F ig . 17. Grade-tonnage for 113 MVT deposits and 10 districts. Diagonal lines represent tonnage of Pb and Zn metal. Select districts and deposits are labeled as: AB = Admiral Bay, AI = Austinville-Ivanhoe, CT = Central Tennessee, ET = East Tennessee, F = Fankou, M = Mehdiabad, ME = Metaline, N
Image
Sphalerite commonly contains textural evidence of its growth history. Bands...
Published: 01 August 2001
by variable concentrations of minor elements, as shown by the distribution of iron (left) and cadmium (right) in concentric growth-zones in sphalerite. Samples (a) and (c) are from the Idol mine, Tennessee; (b) is from Austinville, Virginia. Width of the field of view is 10 cm in (a), 0.6 mm in (b), and 2 mm
Image
Sphalerite commonly contains textural evidence of its growth history. Bands...
Published: 01 August 2001
by variable concentrations of minor elements, as shown by the distribution of iron (left) and cadmium (right) in concentric growth-zones in sphalerite. Samples (a) and (c) are from the Idol mine, Tennessee; (b) is from Austinville, Virginia. Width of the field of view is 10 cm in (a), 0.6 mm in (b), and 2 mm
Image
Sphalerite commonly contains textural evidence of its growth history. Bands...
Published: 01 August 2001
by variable concentrations of minor elements, as shown by the distribution of iron (left) and cadmium (right) in concentric growth-zones in sphalerite. Samples (a) and (c) are from the Idol mine, Tennessee; (b) is from Austinville, Virginia. Width of the field of view is 10 cm in (a), 0.6 mm in (b), and 2 mm
Image
Ptychobaba buttsi  ( Resser, 1938b ) from the lower to middle Cambrian Rome...
Published: 01 September 2014
Figure 10 Ptychobaba buttsi ( Resser, 1938b ) from the lower to middle Cambrian Rome Formation, southwestern Virginia, U.S.A. ( 1–5 , “Rome; 3.5 miles southwest of Buchanan”; 6–8 “Shady; 0.7 mile northwest of Bethany, near Austinville”): 1–3 , complete exoskeleton (dorsal, anterior
Journal Article
Journal: GSA Bulletin
Published: 01 December 1945
GSA Bulletin (1945) 56 (12): 1079–1098.
..., the position of the Taconic thrust is locally obscure, but its existence is demonstrated. NEW JERSEY ZINC COMPANY, AUSTINVILLE, VA. 15 12 1944 Copyright © 1945, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within...