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Friday, May 15, 2020 | History

2 edition of Paleoecology and depositional environment of Fort Hays limestone member, Niobrara Chalk (Upper Cretaceous) west-central Kansas found in the catalog.

Paleoecology and depositional environment of Fort Hays limestone member, Niobrara Chalk (Upper Cretaceous) west-central Kansas

Robert W. Frey

Paleoecology and depositional environment of Fort Hays limestone member, Niobrara Chalk (Upper Cretaceous) west-central Kansas

by Robert W. Frey

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  • 37 Currently reading

Published by University of Kansas Paleontological Institute in [Lawrence] .
Written in English

    Places:
  • Kansas.
    • Subjects:
    • Geology, Stratigraphic -- Cretaceous.,
    • Paleontology -- Cretaceous.,
    • Paleoecology -- Kansas.,
    • Geology -- Kansas.

    • Edition Notes

      Bibliography: p. 61-64.

      Statement[by] Robert W. Frey.
      SeriesUniversity of Kansas paleontological contributions; article 58 (Cretaceous 3), University of Kansas publications, University of Kansas paleontological contributions., 58.
      Classifications
      LC ClassificationsQE701 .K3 no. 58, QE685 .K3 no. 58
      The Physical Object
      Pagination72 p.
      Number of Pages72
      ID Numbers
      Open LibraryOL5394123M
      LC Control Number72611596

      The Austin Chalk Formation in south Texas and northern Mexico represents an "impure" onshore depositional chalk deposited within an environmental framework characterized by distinct paleobathymetric variations. Relatively shallower water, highly fossiliferous chalks containing appreciable amounts of primary metastable carbonate material were. phosphatic member by Sandberg and Gutschick () and presumably is the same as rocks included by these authors in the Delle Phosphatic Member when they extended usage of this name to the Samak area in We prefer not to use the member name here, however, because placement of its upper limit is essentially arbitrary, as explained below, and.

      Book Chapter (4) Article Type. Facet list. Research Article Fort Hays Limestone Member (1) Gulfian Niobrara Formation (2) Smoky Hill Chalk Member (2) Turonian . Fort Hays Limestone Member (4) Fox Hills Smoky Hill Chalk Member (5) Turonian Book Series. Facet list. GSA Field Guide (2) AAPG Hedberg Series (1) AAPG Memoir (1) GSA Special Papers.

      ABSTRACTS (By Author). AAPG Annual Convention April , , New Orleans, Louisiana. Search and Discovery Article # () Posted Novem Select letter corresponding to . Reservoir characteristics and depositional environments of upper Strawn Series (Pennsylvanian) Capps limestone and Fry sandstone core, Lake Abilene field, Taylor County, Texas.


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Paleoecology and depositional environment of Fort Hays limestone member, Niobrara Chalk (Upper Cretaceous) west-central Kansas by Robert W. Frey Download PDF EPUB FB2

Get this from a library. Paleoecology and depositional environment of Fort Hays Limestone Member, Niobrara Chalk (Upper Cretaceous), west-central Kansas. [Robert W Frey]. Niobrara Chalk Fort Hays Limestone Member. The Fort Hays Limestone Member is 55 to 75 feet ( to m) thick in the field-trip area, the latter figure being near the maximum for.

Frey, R. W.,Paleoecology and depositional environment of Fort Hays Limestone Member, Niobrara Chalk (Upper Cretaceous), west-central Kansas: University of Kansas Paleontological Contributions, Art.

58 (Cretaceous 3), 72 p. PDF | On Jan 1,K. Shimada and others published Ptychodus mammillaris (Elasmobranchii) and Enchodus cf.

shumardi (Teleostei) from the Fort Hays Limestone Member of the Niobrara Chalk. Shimada, K. Selachians from the Fort Hays Limestone Member of the Niobrara Chalk (Upper Cretaceous), Ellis County, Kansas. Transactions of the Kansas Academy of Science, 99() Shimada, K.

Fossil vertebrates are extremely rare in the Fort Hays Limestone member of the Niobrara Chalk in comparison to the rich variety of well-preserved fish, turtles, mosasaurs, pteranodons, and toothed. Paleoecology and depositional environment of Fort Hays Limestone Member, Niobrara Chalk (Upper Cretaceous), west-central Kansas.

Univ. Kansas Paleont. Contr., The Paleoecological and Environmental Significance Of Trace Fossils. In: Frey R.W. (eds) The Study of Trace Fossils. Springer, Berlin, Heidelberg.

Shimada, K. Selachians from the Fort Hays Limestone Member of the Niobrara Chalk (Upper Cretaceous), Ellis County, Kansas. Kansas Academy of Science, Transactions 99() Shimada, K. Dentition of Late Cretaceous shark, Ptychodus mortoni (Elasmobranchii, Ptychodontidae).

Journal of Vertebrate Paleontology Frey, R. W.,Trace fossils from the Fort Hays Limestone Member of the Niobrara Chalk (Upper Cretaceous) in west-central Kansas: Special Paper - Geological Society of America, p. Frey, R. W., and J. Cowles,New observations on Tisoa, a trace fossil from the Lincoln Creek Formation (mid-Tertiary) of Washington: Compass.

Frey RW () Paleoecology and depositional environment of Fort Hays Limestone Member, Niobrara Chalk (Upper Cretaceous), west-central Kansas. Univ of Kansas Paleontol Cont –72 Google Scholar Frey RW () Trace fossils and hummocky cross-stratification, Upper Cretaceous of Utah.

FREUD, S. ( JOAN RIVIERE) - Civilization and its discontents FREY, R. - Paleoecology and depositional environment of Fort Hays limestone member, Niobrara Chalk (Upper Cretaceous), West-central Kansas FREY, W., FRAHM, J.P., FISCHER, E.

& LOBIN, W. - Die Moos- und Farnpflanzen Europas FREY, D.G. - Remains of animals in Quaternary lake and. @article{osti_, title = {Depositional environments and paleoecology of the Oil Creek Formation (Middle Ordovician), Arbuckle Mountains and Criner Hills, Oklahoma}, author = {Lewis, R D}, abstractNote = {The Oil Creek Formation (Whiterockian) is the second oldest of the five formations which make up the Simpson Group.

Although widespread in the subsurface, it is exposed only in the study. Paleoecology and depositional environment of Fort Hays Limestone Member, Niobrara Chalk (Upper Cretaceous), west-central Kansas.

Pre-breakup of continental extension in East Gondawanaland and the Eariy Cretaceous opening of the eastern Indian Ocean. Stratigraphy and depositional environment of the Greenhorn Limestone (Upper Cretaceous) of Kansas.

BulletinKansas Geological Survey, pp. Hattin, D.E., Stratigraphy and depositional environment of the Smoky Hill Chalk Member, Niobrara Chalk (Upper Cretaceous) of the type area, western Kansas. Contact D.

Hill Jr. Library. 2 Broughton Drive Campus Box Raleigh, NC () James B. Hunt Jr. Library. Partners Way. Buy The Petrology and Depositional Environment of the Bainbridge Limestone (Middle and Upper Silurian) of Southeast Missouri and Southwest Illinois,85 pages with 3 plates.

on FREE SHIPPING on qualified orders. Figure 5 is a typical log for the study area. The Tussy interval is defined as the set of strata between the Tussy Limestone at the top and the Atokan Upper Dornick Hills Group at the base.

“This limestone is the key bed used in subsurface work of the Lower Deese Formation in southern Oklahoma” (Hoard, ). The stratigraphy and paleoecology of a hardground in the Grant Lake Limestone (Cincinnatian, Upper Ordovician) near Maysville, Kentucky Dana Dettmers Department of Geology, Beloit College, College St., Beloit, WI middle-shelf marine environment.

Table 1 shows the results of the amount of fossil fragments present from thin. The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast is also known as the Kaibab Formation in Arizona, Nevada, and Utah.

The Kaibab Limestone forms the rim of the Grand the Big Maria Mountains, California, the Kaibab Limestone is highly. The Niobrara Formation, also called the Niobrara Chalk, is a geologic formation in North America that was deposited between 87 and 82 million years ago during the Coniacian, Santonian, and Campanian stages of the Late Cretaceous.

It is composed of two structural units, the Smoky Hill Chalk Member overlying the Fort Hays Limestone Member. CONODONT BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE PERTH LIMESTONE MEMBER, STAUNTON FORMATION (PENNSYLVANIAN) OF THE ILLINOIS BASIN, U.S.A.

CARl B. REXROAD. lEWIS M. BROWN. JOE DEVERA. and REBECCA J. SUMAN Rexroad, c. Brown. L. Devera, and Suman, R. Conodont biostrati graphy and paleoec ology of the Perth Limestone Member.A New Fossil Vertebrate Locality of the Jetmore Chalk Member of the Upper Cretaceous Greenhorn Limestone in North-Central Kansas, U.S.A.

The Jetmore Chalk Member of the Greenhorn Limestone is a Late Cretaceous rock unit deposited under the Western Interior Seaway in North America. indicating that the marine paleoecology during the.Koša E. Lithostratigraphy and depositional environment of Lower-Middle Jurassic crinoidal limestone formations of the Vysoká Nappe Unit (Malé Karpaty Mts, Western Carpathians).

Geol. Carpath Kotake N. Paleoecology of .