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Squaw Bay Limestone

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Journal Article
Published: 01 July 1967
Journal of Paleontology (1967) 41 (4): 902–919.
Image
—Isopach map of Unit A (top of <span class="search-highlight">Squaw</span> <span class="search-highlight">Bay</span> <span class="search-highlight">limestone</span> to base of Coldwater sha...
Published: 01 November 1954
Fig. 8. —Isopach map of Unit A (top of Squaw Bay limestone to base of Coldwater shale).
Image
—Sand-shale ratio map of Unit A (top of <span class="search-highlight">Squaw</span> <span class="search-highlight">Bay</span> <span class="search-highlight">limestone</span> to base of Cold...
Published: 01 November 1954
Fig. 9. —Sand-shale ratio map of Unit A (top of Squaw Bay limestone to base of Coldwater shale).
Image
—Per cent carbonate in Unit A (top of <span class="search-highlight">Squaw</span> <span class="search-highlight">Bay</span> <span class="search-highlight">limestone</span> to base of Coldwa...
Published: 01 November 1954
Fig. 10. —Per cent carbonate in Unit A (top of Squaw Bay limestone to base of Coldwater shale).
Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE256-p155
... The Late Devonian Michigan Basin was floored by the Middle and Upper Devonian Squaw Bay Limestone, which was deposited during the downwarping that produced the basin within a former Middle Devonian carbonate platform. The Squaw Bay comprises three beds, each having a different conodont fauna...
Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE256-p181
... transitans Zone with a calcareous mudstone bed at the top of the Squaw Bay Limestone. Subsidence was followed by a 12-m.y.-long Late Devonian episode of slow, hemipelagic, basinal sedimentation of organic black muds that formed the Antrim Shale, interrupted basinwide only by deposition of its prodeltaic...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1943
AAPG Bulletin (1943) 27 (5): 571–595.
... limestone, and Four Mile Dam formation. Following the reef stage, shales and impure limestones were deposited to form the Norway Point, Potter Farm, Thunder Bay, and Squaw Bay formations. Older parts of the group are Middle Devonian, but the three last-named formations are Upper Devonian in age...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2003
AAPG Bulletin (2003) 87 (4): 581–608.
... ( Figure 4 ; Table 1 ). Table 1 Outcrop and Subsurface Thicknesses of Formations within the Traverse Group Formation Name Outcrop Average Thickness, m (feet) Subsurface Average Thickness, m (feet) Jordan River Formation 3 (10) 6.7 (22) Squaw Bay Limestone 3 (10) 6.7 (22...
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Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5403-8.297
EISBN: 9780813754093
... display of numerous, largecalcareous concretions, in situ and free of shale matrix, is present in the quarry. How werethey formed? Partridge Point has an exposed limestone sequence that underlies Antrim black shales beneath Squaw Bay. Applying Walther’s Law, one can go up section and down dip from...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1954
AAPG Bulletin (1954) 38 (11): 2324–2356.
...Fig. 8. —Isopach map of Unit A (top of Squaw Bay limestone to base of Coldwater shale). ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1952
AAPG Bulletin (1952) 36 (8): 1642–1644.
... of the Traverse group. 3 The upper part of the Traverse (Upper Devonian “Squaw Baylimestone) is not found in southwestern Michigan. The irregularity and spottiness of the producing areas in this part of the Michigan basin have caused many geologists to consider the possibility that the oil fields...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1957
AAPG Bulletin (1957) 41 (12): 2677–2694.
... shaly limestone containing gray-black chert. Underlying the Squaw Bay a gray-black shale is found which has a marked resemblance to the “Traverse formation” shales of the Antrim above. Under this shale an upper limestone stringer is found which contains characteristic white chert. West of Sec. 15, T. 6...
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Journal Article
Published: 18 May 2004
Canadian Journal of Earth Sciences (2004) 41 (5): 527–551.
... near Squaw Cap Mountain (Fig.  2 ). These faunas belong to the H. crickmayi Zone, indicating a late Richmondian (middle Ashgillian) age and confirming that the upper (Llandoverian) part of the White Head Formation has been eroded in that area. At the Popelogan Inlier, limestone lenses in a thin unit...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1969
AAPG Bulletin (1969) 53 (5): 1043–1057.
... the Traverse Group. The group has a mean thickness of approximately 600 ft in the area studied and has been subdivided, both in outcrop and in the subsurface, into twelve formations. The present study is concerned with the surface of the youngest formation, the Squaw Bay Limestone ( Cohee, 1947...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1961
AAPG Bulletin (1961) 45 (12): 1994–2011.
...Harlan R. Bergquist ABSTRACT Distinctive Late Cretaceous foraminiferal microfaunas are present in shale beds of the Matanuska Formation in the Squaw Creek-Nelchina River area, south-central Alaska. Numerous species of Foraminifera and a few ostracods have been found in many surface and subsurface...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1944
AAPG Bulletin (1944) 28 (10): 1519–1527.
... VERMILION COUNTY: MYER’S FOREMAN NO. I, SEC. 13, T. 18 N., R. 14 W Black shale, with 2 feet loose sand at base Alto (or Squaw Bay?) limestone, 18 feet  Brown, medium granular dolomitic limestone 1,376-1,394 Logansport limestone, 21 feet  White, crystalline to marly, fossiliferous -1,415 limestone...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1966
AAPG Bulletin (1966) 50 (5): 901–920.
... the Prospect Mountain Quartzite do not reappear in the Cricket Mountains. Gray limestone beds cropping out approximately ½ mile west of Squaw Spring in a dry wash north of Highway 21 are assigned tentatively to the Lower Mississippian. The areal extent of the unit is not large and its thickness...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1944
AAPG Bulletin (1944) 28 (2): 173–196.
... in the Antrim, especially in the calcareous zones near the base. The basal contact of the Antrim shale is exceptionally sharp. The contrast in both color and texture between the brown limestone of the Squaw Bay division of the Traverse and the dark gray to black shale of the Antrim makes the distinction...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1990
AAPG Bulletin (1990) 74 (7): 1087–1099.
.... At the top of the Desert Creek, beneath the Gothic shale, is another carbonate unit, which averages 14 ft (4.2 m) thick. 2 Consultant, George Dewey High School, Subic Bay Naval Station, Philippines, Box 70, FPO San Francisco, California 96651. Formerly with Marathon Oil Company, Casper, Wyoming. I...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1960
AAPG Bulletin (1960) 44 (11): 1793–1808.
... University. Impure limestone containing grass-green grains of glauconite commonly as casts of shelled animals. G-3219 Glauconitic sandstone. Franconia formation. Upper Cambrian. Readstown, Wisconsin. Collected by C. S. Bays. G-3220 Glauconite. Uppermost Cretaceous. Top 2′ of Navesink formation...
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