Last edited by Vugul
Monday, July 13, 2020 | History

1 edition of Depositional environment of Upper Cretaceous black sandstones of the Western Interior found in the catalog.

Depositional environment of Upper Cretaceous black sandstones of the Western Interior

Depositional environment of Upper Cretaceous black sandstones of the Western Interior

  • 232 Want to read
  • 3 Currently reading

Published by U.S. Dept. of the Interior in Washington .
Written in English


Edition Notes

11

The Physical Object
Pagination29 p.
Number of Pages29
ID Numbers
Open LibraryOL22014074M

The Upper Cretaceous Fox Hills Formation on the southeastern flank of the Powder River basin, Wyoming, was deposited along a regressive, northeast-trending, low-energy, tidally affected, wave-dominated coastline. The Fox Hills Formation consists of rocks deposited successively in . Two small mouth-bars are then deposited in the mouths of these channels and the channel continues to split until become too small to carry sediments ().After this, the system becomes chocked and avulsion or lobe switching occ the good example is Mississippi delta system.. The formation of shallow-marine deltaic basins is typically exhibit a lobe shape with multi-scale coeval terminal.

These sandstones are con- sidered as a part of the Nubian sandstones, whose age and environment is problematic. Blake and Ionides () gave a Early Cretaceous age for all the sandstones in southern Jordan, while Bender () was able to sub- divide these rocks Cited by: Sandy depositional systems also play a key role in helping us assign a basin to its proper type and in relating it to a plate tectonic or other genetic framework. With the exception of some carbonates, sandstones are commonly the most permeable of all sedimentary rocks—a key element in their economic significance for oil, gas, groundwater Cited by: 1.

The Kaiparowits Formation is an unusually thick package of Upper Cretaceous (late Campanian) strata exposed in Grand Staircase-Escalante National Monument of southern Utah, USA. The formation was deposited within the rapidly subsiding Cordilleran foreland basin as part of a thick clastic wedge derived from sources in the Sevier orogenic belt, thrust sheets in southeastern Nevada and southern Cited by: The precipitation of cements in quartzarenites and subarkoses deposited in a marine environment tends to follow a predictable pattern beginning with clay authigenesis associated with quartz and feldspar overgrowths, followed by carbonate precipitation. Clay minerals form first because they precipitate more easily than quartz and feldspar overgrowths, which require more ordered crystal : Web page.


Share this book
You might also like
Elderly people in the community

Elderly people in the community

Evolutionary ethics

Evolutionary ethics

introduction to Victorian genre painting

introduction to Victorian genre painting

Lung cancer mortality in Ontario with special reference to the influence of urbanization.

Lung cancer mortality in Ontario with special reference to the influence of urbanization.

Selcted poems

Selcted poems

Biography

Biography

Tourist attractions.

Tourist attractions.

Crime and custom in savage society

Crime and custom in savage society

The Virginia chronicle

The Virginia chronicle

Christopher Columbus

Christopher Columbus

Annus mirabilis of Sir Isaac Newton, 1666-1966.

Annus mirabilis of Sir Isaac Newton, 1666-1966.

The 2000-2005 Outlook for Wholesale Petroleum and Petroleum Products in the Middle East

The 2000-2005 Outlook for Wholesale Petroleum and Petroleum Products in the Middle East

poetical works of James Thomson ...

poetical works of James Thomson ...

Circumspection in our walk distinguishes the wise from the foolish

Circumspection in our walk distinguishes the wise from the foolish

continuation of Samuel Puffendorfs Introduction to the history of the principal kingdoms and states of Europe, brought downto this present year.

continuation of Samuel Puffendorfs Introduction to the history of the principal kingdoms and states of Europe, brought downto this present year.

Depositional environment of Upper Cretaceous black sandstones of the Western Interior Download PDF EPUB FB2

Depositional environment of Upper Cretaceous black sandstones of the Western Interior (Upper Cretaceous black sandstones of the Western Interior) (Geological Survey Professional Paper A) Bibliography: p.

* 1. Geology, Stratigraphic-Cretaceous. 2.,Sandstone--The West. Placer deposits-The West. Murphy, John Francis, II Cited by: 7.

Depositional environment of Upper Cretaceous black sandstones of the Western Interior Professional Paper A By: Robert Stroud Houston and John F. Murphy.

Get this from a library. Depositional environment of Upper Cretaceous black sandstones of the Western Interior: Cretaceous black sandstone deposits of the Western Interior have stratigraphic, structural, textural, and mineralogical characteristics helpful in reconstructing local and regional depositional environments.

[Robert S Houston; John F Murphy; Geological Survey (U.S.)] -- Cretaceous. OCLC Number: Notes: "Upper Cretaceous black sandstones of the Western Interior." "Cretaceous black sandstone deposits of Western Interior have stratigraphic, structural, textural, and mineralogical characteristics helpful in reconstructing local and regional depositional environments.".

Buy Cretaceous Shelf Sandstones and Shelf Depositional Sequences, Western Interior Basin, Utah, Colorado and New Mexico: Salt Lake City, Utah to 30 - July 7, (Field Trip Guidebooks) on FREE SHIPPING on qualified orders. Cretaceous Shelf Sandstones and Shelf Depositional Sequences, Western Interior Basin, Utah, Colorado and New Mexico: The second theme focuses on Upper Cretaceous coastal and shallow marine rocks as displayed by exposures in the spectacular Book Cliffs of Utah.

The shelf and shoreface sequences seen in these rocks represent some of the. Upper Cretaceous Stratigraphy and Depositional Environments of Western Kansas by Donald E. Hattin, Indiana University, and Charles T.

Siemers, Cities Service Company Assisted by Gary F. Stewart, Oklahoma State University. Originally published in as Kansas Geological Survey Guidebook 3.

The book was reprinted in with some modifications. The Hatch Mesa succession is located 1–2 km southwest of Hatch Mesa in a gently curving, northwest to southeast trending outcrop belt which is approximately 7 km long ().The Hatch Mesa succession is a 6–20 m thick package, that is subdivided into 3–4 coarsening-upward cycles, consisting of approximately 30–40% sandstone ().Most sandstone beds are very fine- to fine-grained, sharp-based Cited by: The Upper Cretaceous (Campanian) Horsethief.

Formation in the Northern Disturbed Belt and Sweetgrass Arch areas of Montana (Fig. I) consists of sandstones, siltstones, and mudstones which were deposited along the western margin of the Western Interior Cretaceous seaway (Fig.

David A. Carr, "Fades and depositional environments of the coal-bearing upper carbonaceous member of the Wepo Formation (Upper Cretaceous), northeastern Black Mesa, Arizona", Stratigraphy, depositional environments; and sedimentary tectonics of the western margin, Cretaceous Western Interior Seaway, J.

Dale Nations, Jeffrey G. Eaton. The Sego Sandstone Member was deposited on the western margin of the Cretaceous Western Interior Seaway and is a member of the Mesaverde Group (Warner ) (Figs.

1, 2). Whereas the coeval stratigraphy west of Green River, Utah is composed of the Upper Castlegate Sandstone, its basinward correlatives in the study area are the. Depositional Framework of the Upper Cretaceous Mancos Shale and the Lower Part of the Upper Cretaceous Mesaverde Group, Western Colorado and Eastern Utah By Ronald C.

Johnson Abstract A detailed history of subsidence and of infilling patterns for part of File Size: 1MB. Barbara A. am Ende, "Depositional environments, palynology, and age of the Dakota Formation, south-central Utah", Stratigraphy, depositional environments; and sedimentary tectonics of the western margin, Cretaceous Western Interior Seaway, J.

Dale Nations, Jeffrey G. Eaton. Ichnology and depositional environments of the Upper Cretaceous Dinosaur Park – Bearpaw formation transition in the Cypress Hills region of Southwestern Saskatchewan, Canada. Facies architecture and depositional environments of the Upper Cretaceous Kaiparowits Formation, southern Utah Article (PDF Available) in Sedimentary Geology June with Reads.

The Upper Cretaceous Sego Sandstone Member of the Mesaverde Group has been extensively studied in the Book Cliffs area of Utah and Colorado, and has been the focus of stratigraphic reconstruction.

The Milk River and Eagle formations in southern Alberta and north-central Montana form the core of the first Upper Cretaceous clastic wedge in this part of the Western Interior Foreland Basin. Cretaceous Shelf Sandstones and Shelf Depositional Sequences, Western Interior Basin, Utah, Colorado and New Mexico Salt Lake City, Utah to Albuquerque, New Mexico June July 7, Field Trip Guidebook Tl 19 Leaders: Dag Nummedal, Editor Robyn Wright Associate Leaders: Rex Cole Robert Retny, Editor American Geophysical Union, Washington, D.C.

The table below includes specific environments where various types of sediments are deposited and common rocks, structures, and fossils that aid in deducing the depositional environment from examining a sedimentary rock outcrop.

Although this is not a complete list, it is a good introduction to depositional environments. Continental; Transitional. The Mancos Shale represents the offshore and open sea environment of the Cretaceous Western Interior Seaway (Weimer, ).

During the Cretaceous, marine waters flooded across the North American continent simultaneously from the Arctic and the Tethys regions. These epicontinental seas joined in Colorado to form the Cretaceous western interior. Request PDF | Depositional remnants, part 2: Examples from the Western Interior Cretaceous basin of North America | The Western Interior Cretaceous basin contains numerous examples of depositional Author: Randi Martinsen.Depositional environment and tectono-provenance of Upper Kaimur Group sandstones, Son Valley, Central India Article (PDF Available) in Arabian Journal of Geosciences 10(1) January with the Cretaceous Western Interior Seaway of western North America.

Sediment sourced from the uplifted Sevier Orogen to the west fed a shoreline in the adjacent subsiding north–south trending foredeep. These sandstones are now superbly exposed along a km-long, strike-parallel, continuous outcrop in the cliffs of the Wasatch Plateau of.