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Sevy Dolomite

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Journal Article
Published: 01 January 1964
Journal of Paleontology (1964) 38 (1): 74–84.
...J. G. Johnson; Anthony Reso Abstract A thick section of Sevy Dolomite in the Pahranagat Range of Nevada has yielded a small brachiopod fauna from a horizon about 90 feet above the base. Eleven species are described including 3 new species GeoRef, Copyright 2004, American Geological Institute...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1962
AAPG Bulletin (1962) 46 (11): 2033–2056.
...John C. Osmond ABSTRACT The Sevy is typically fine crystalline to microcrystalline tan and gray dolomite which weathers with a distinctive very light gray surface. It occurs in beds from a few inches to 2 feet thick and is usually finely laminated. Sedimentary breccias, and soft-sediment...
FIGURES | View All (21)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1954
AAPG Bulletin (1954) 38 (5): 954–955.
...-weathering dolomite. It unconformably overlies the Laketown dolomite (Silurian) and grades upward into the Simonson dolomite (Middle Devonian). Halysites, found in the lower part, indicates at least part of the Sevy is Silurian; the upper part is probably Devonian. The Sevy is tentatively correlated...
Image
—<b>Sevy</b> <b>Dolomite</b>, Egan Range, Nevada, showing splintery fracturing of beds. B...
Published: 01 November 1962
Fig. 2. —Sevy Dolomite, Egan Range, Nevada, showing splintery fracturing of beds. Bedding horizontal in this view.
Image
—Sigmoidal fold in finely laminated <b>Sevy</b> <b>Dolomite</b>, Egan Range, Nevada.
Published: 01 November 1962
Fig. 5. —Sigmoidal fold in finely laminated Sevy Dolomite, Egan Range, Nevada.
Image
—Cherty argillaceous member of <b>Sevy</b> <b>Dolomite</b>, Desert Range. Argillaceous do...
Published: 01 November 1962
Fig. 6. —Cherty argillaceous member of Sevy Dolomite, Desert Range. Argillaceous dolomite (light gray) with irregular nodules of chert parallel with bedding in upper right part of picture; bands of partly silicified dolomite (dark gray) containing irregular chert nodules (gray). Photo by W. B. R.
Image
—Irregular body of quartz sand in sandy member of <b>Sevy</b> <b>Dolomite</b>, Egan Range...
Published: 01 November 1962
Fig. 15. —Irregular body of quartz sand in sandy member of Sevy Dolomite, Egan Range, 6 miles south of Lund, Nevada. Matrix is homogeneous, non-laminated, microcrystalline dolomite which probably was mud when sand was deposited. Upper margin of sand is a small, poorly developed stylolitic contact.
Image
—Cross sections of <b>Sevy</b> <b>Dolomite</b> reconstructed to original extent with sand...
Published: 01 November 1962
Fig. 20. —Cross sections of Sevy Dolomite reconstructed to original extent with sandy member as horizontal datum plane.
Image
—Isopachous map of <b>Sevy</b> <b>dolomite</b>.
Published: 01 September 1954
Fig. 1. —Isopachous map of Sevy dolomite.
Image
—Exceptionally well developed lamination from <b>Sevy</b> <b>dolomite</b>. Note silt and ...
Published: 01 September 1954
Fig. 4. —Exceptionally well developed lamination from Sevy dolomite. Note silt and very fine-grain quartz and dolomite in lower laminae. Cross-lamination in upper left and lower middle of field. Granule of dolomite in lower right has caused depression of underlying dolomite. (×1.5)
Image
—Etched surface of sandy member of <b>Sevy</b> <b>dolomite</b> showing well rounded quart...
Published: 01 September 1954
Fig. 5. —Etched surface of sandy member of Sevy dolomite showing well rounded quartz sand grains (black), zones of slightly different color and crystal-size dolomite, and plastimorphic fragments of dolomite (some contain quartz sand grains). Roiled sedimentary breccia indicating plastic state
Image
—Cumulative curves of sandy member of <b>Sevy</b> <b>dolomite</b>, north and east of Egan...
Published: 01 September 1954
Fig. 6. —Cumulative curves of sandy member of Sevy dolomite, north and east of Egan Range.
Image
—Cumulative curves of sandy member of <b>Sevy</b> <b>dolomite</b>, in Egan Range.
Published: 01 September 1954
Fig. 7. —Cumulative curves of sandy member of Sevy dolomite, in Egan Range.
Image
—Cumulative curves of sandy member of <b>Sevy</b> <b>dolomite</b>, south and west of Egan...
Published: 01 September 1954
Fig. 8. —Cumulative curves of sandy member of Sevy dolomite, south and west of Egan Range.
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1954
AAPG Bulletin (1954) 38 (9): 1911–1956.
...Fig. 1. —Isopachous map of Sevy dolomite. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1957
AAPG Bulletin (1957) 41 (10): 2175–2191.
... and Stromatoporoid- Cladopora (Middle Devonian). The Devils Gate limestone faunas range in age from Middle Devonian to early Late Devonian. The Nevada formation is regarded as a lithic correlative of the Simonson and the major part, if not all, of the Sevy dolomites of western Utah and possibly of parts...
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Journal Article
Published: 01 September 2007
Journal of Paleontology (2007) 81 (5): 824–840.
...CAROLE J. BURROW Abstract Isolated spines and scales from acanthodian fishes are common elements in vertebrate assemblages from the Early Devonian (Emsian) of Arizona, Idaho, Nevada, Utah, and Wyoming. The material described here is from the Sevy Dolomite and lower Grassy Flat Member, Water Canyon...
FIGURES | View All (9)
Image
—Finely laminated <b>dolomite</b> typical of <b>Sevy</b>, showing various sedimentary str...
Published: 01 November 1962
Fig. 3. —Finely laminated dolomite typical of Sevy, showing various sedimentary structures.
Image
—Very finely laminated <b>dolomite</b> typical of <b>Sevy</b> illustrating detail of sedi...
Published: 01 November 1962
Fig. 4. —Very finely laminated dolomite typical of Sevy illustrating detail of sedimentary deformation.
Image
—Subdivisions of <b>Sevy</b> and Simonson <b>dolomites</b>. Thickness in feet.
Published: 01 September 1954
Fig. 2. —Subdivisions of Sevy and Simonson dolomites. Thickness in feet.