Byron Formation

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Journal Article
Published: 01 August 2010
European Journal of Mineralogy (2010) 22 (4): 605–612.
... . Tarashchan , A.N. ( 1978 ): Luminescence of Minerals . Naukova Dumka , Kiev (in Russian) . Yakubovich , O.V. , Pekov , I.V. , Steele , I.M. , Massa , W. , Chukanov , N.V. ( 2009 ): Alkali metals in beryl and their role in the formation of derivative structural motifs...
FIGURES | View All (9)
Series: GSA Special Papers
Published: 10 May 2018
DOI: 10.1130/2017.2531(04)
EISBN: 9780813795317
..., of the open-marine deposits of the Lime Island Formation, the restricted lagoonal–tidal flat Byron Formation, and the open-marine deposits of the Hendricks Formation. The contacts with the underlying Cataract Group and overlying Manistique Group are gradational. Identification and description of facies...
FIGURES | View All (9)
Journal Article
Published: 01 July 1999
Journal of Paleontology (1999) 73 (4): 667–676.
.... Associated with the thelodont scales are rare phosphatic fragments of questionable dermal "bone" and scales, possibly of heterostracan origin. Thelodont scales are also found in the Hendricks Formation at Fayette State Park, Michigan and in the subsurface Byron Formation (Burnt Bluff Group) in Schoolcraft...
Series: Society of Exploration Geophysicists Geophysical Monograph Series
Published: 01 January 2014
DOI: 10.1190/1.9781560803140.ch5
EISBN: 9781560803140
... at the beautiful mansion, the Villa Diodati.” “Watson, you will recall that the villa carries the bold elegance of a building that will never look anything less than magnificent. It sits on a gentle hill, looking onto the vast crystal expanse of Lake Geneva.” “On 25 April 1816, Lord Byron left England...
Series: AAPG Methods in Exploration Series
Published: 01 January 2003
DOI: 10.1306/Mth14824C9
EISBN: 9781629810553
... ; Simmons and Scholle, 1990 ). As a result, the unit is variable in thickness. The Tensleep, which is approximately 34 m (110 ft) thick in Byron field, is unconformably overlain by red beds, shales, evaporites, and dolomites of the Goose Egg member of the Phosphoria Formation. The Tensleep conformably...
FIGURES | View All (17)
Maps showing locations of boreholes in the (A) Brentwood, (B) <b>Byron</b>, and (C...
Published: 01 December 2005
Figure 5. Maps showing locations of boreholes in the (A) Brentwood, (B) Byron, and (C) Tracy oil and gas fields. Geology is from Dibblee ( 1980b , d , 1981a , b ). Qa, Quaternary alluvium; Qoa, Older alluvium of Pleistocene age; Qot, older terrace of Pleistocene age; Tps, Pliocene
—<b>Byron</b> and Garland domes, Big Horn and Park counties, Wyoming, contoured on...
Published: 01 May 1954
Fig. 10. —Byron and Garland domes, Big Horn and Park counties, Wyoming, contoured on Tensleep formation. After C. E. Dobbin, “Exceptional Oil Fields in Rocky Mountain Region of United States,” Bull. Amer. Assoc. Petrol. Geol., Vol. 31, No. 5 (May, 1947 ), Fig. 12 , p. 812. Both structures
Series: GSA Memoirs
Published: 01 September 1945
DOI: 10.1130/MEM10-p1
.... The samples were obtained from 12 stratigraphic horizons. These assemblages contain 104 species, a considerable number of which were originally described from the Sidney and Kellogg shales from the Mount Diablo and Byron quadrangles. The conclusion is that the zone represented by the Sidney shale...
Journal Article
Published: 01 May 1981
Canadian Journal of Earth Sciences (1981) 18 (5): 869–883.
... represented in the Schoolcraft. Facies relationships between the Michigan Hendricks dolomite and its correlative Mindemoya and St. Edmund Formations argue for their valid maintenance. The relationship between the Byron and Wingfield Formations is less clear. Probably the Dyer Bay Formation should be extended...
Journal Article
Journal: GSA Bulletin
Published: 01 July 1970
GSA Bulletin (1970) 81 (7): 2123–2128.
...-shale units: the Albian-Turonian Adobe Flat Shale, the Coniacian-Campanian Panoche Formation, and the Campanian-Maestrichtian Moreno Formation. Both the upper and lower parts of this section are absent locally, having been removed by erosion or faulting, or both. The middle unit, the Panoche Formation...
Journal Article
Journal: Economic Geology
Published: 01 March 2010
Economic Geology (2010) 105 (2): 257–262.
...John Mavrogenes; Richard W. Henley; Agnes G. Reyes; Byron Berger Abstract In enargite-gold (high-sulfidation) vein deposits, magmatic fluid is considered responsible for the transport of metals and sulfur into the depositional regime. New data from Field-Emission SEM analyses of sulfosalt mineral...
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Series: Geological Society, London, Special Publications
Published: 01 January 1999
DOI: 10.1144/GSL.SP.2000.169.01.11
EISBN: 9781862394179
... Abstract The Fall River Formation around the Black Hills uplift is pervasively fractured by layer-perpendicular joints. Systematic joints in the formation maintain consistent orientations over large areas and are commonly abutted by later-formed fractures, resulting in an orthogonal pattern...
Journal Article
Published: 01 December 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (4): 654–673.
...Anthony P. Hamblin; Byron W. Abrahamson GeoRef, Copyright 2004, American Geological Institute. 1996 ...
Journal Article
Published: 01 September 1961
Journal of Paleontology (1961) 35 (5): 1089.
...John Harger Hoyt; Byron John Chronic Abstract The occurrence of Triticites ventricosus in the basal beds of the Ingleside Formation at the type locality, Owl Canyon, Colorado, indicates a Wolfcampian [Permian] age for this formation. GeoRef, Copyright 2004, American Geological Institute...
Series: GSA Memoirs
Published: 01 January 1953
DOI: 10.1130/MEM55-p1
Journal Article
Journal: GSA Bulletin
Published: 01 January 1946
GSA Bulletin (1946) 57 (1): 35–114.
...BYRON N COOPER; G ARTHUR COOPER Abstract In classifying the lower Middle Ordovician of the Shenandoah Valley, the formation names Stones River, Mosheim, Lenoir, Holston, Whitesburg, and Athens have been used without adequate evidence. Detailed study shows that the so-called Athens and Whitesburg...
Journal Article
Journal: GSA Bulletin
Published: 01 June 1943
GSA Bulletin (1943) 54 (6): 819–886.
...BYRON N. COOPER; CHILTON E. PROUTY Abstract The lower Middle Ordovician succession of Tazewell County, in southwestern Virginia, is herewith subdivided into 29 distinctive zones. Detailed tracing and mapping have led to the recognition of inconsistencies in the use of the stratigraphic names Stones...
Series: Society of Exploration Geophysicists Geophysical Monograph Series
Published: 01 January 1991
DOI: 10.5382/Mono.08.12
EISBN: 9781629490038
... assemblages. In 1922, he coined the term “epithermal” for the shallower, volcanic rock-related banded veins. Elie de Beaumont (1847), LeConte (1883), Posepny (1893), Lindgren (1901), and others recognized the possible link of active thermal systems to the formation of vein deposits. It was noticed that H 2 S...
Journal Article
Journal: Economic Geology
Published: 01 April 2003
Economic Geology (2003) 98 (2): 387–408.
...Byron R. Berger; Joseph V. Tingley; Lawrence J. Drew Abstract Bonanza-grade orebodies in epithermal-style mineral deposits characteristically occur as discrete zones within spatially more extensive fault and/or fracture systems. Empirically, the segregation of such systems into compartments...
FIGURES | View All (16)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1973
AAPG Bulletin (1973) 57 (4): 801–802.
...Byron L. Ristvet; Fred T. MacKenzie; Donald C. Thorstenson; Robert H. Leeper ABSTRACT Pore-water chemistry and mineralogy of carbonate and terrigenous sediments from Kaneohe Bay, Oahu, Hawaii, were analyzed to determine differences in pore-water compositions, in nature and extent of early...