ⓘ Kaskapau Formation. The Kaskapau Formation is a geological formation in North America whose strata date back to the Late Cretaceous. The name derives from kaska ..

                                     

ⓘ Kaskapau Formation

The Kaskapau Formation is a geological formation in North America whose strata date back to the Late Cretaceous.

The name derives from kaskapahtew ᑲᐢᑲᐸᐦᑌᐤ, the Cree word for "smoky". It was first described on the banks of the Smoky River, close to the confluence with the Puskwaskau River by F.H. McLearn in 1926.

                                     

1. Geographical distribution

The formation is 170 meters 560 ft thick in the Peace River and Smoky River area, and thickens up to 900 meters 3.000 ft in the foothills of the Northern Rocky Mountains in British Columbia. It is exposed along the Peace River near Dunvegan, as well as in the Smoky River area.

The formation is part of the Smoky River Group, and is conformably overlain by the Bad Heart Formation in the western area, and unconformably by the Cardium Formation in the Pouce Coupe River area. It is conformable underlain by the Dunvegan Formation.

The Kaskapau Formation is equivalent to the Colorado Group shale in central Alberta. It is equivalent to the upper Blackstone Formation, the Cardium Formation, and the Muskiki Formation in the Canadian Rockies foothills in western Alberta.

                                     

2. Lithology

The Kaskapau Formation is represented mostly by dark grey shale, with sandstone tongues and lentils at the base Doe Creek Member, Pouce Coupe Member. Thin volcanic ash layers may occur in the British Columbia foothills.

                                     

3. Paleontology

Oyster fossils are encountered at the base of the formation, and Inoceramus fragments such as I. labiatus are found throughout the entire stack. Ammonites are also present in the sand beds, genus encountered include Dunveganoceras and Watinoceras in the lower part and Scaphites in the upper part. Microfauna include benthonic and fewer planktonic foraminifera.

                                     
  • Dunvegan Formation Gas is produced from the Cardium Formation in the southern reaches of the Group, in central Alberta and northern Alberta. The Kaskapau Shale
  • Cardium Formation and conformably overlain by the Bad Heart Formation The Kaskapau Formation in northern Alberta replaces the upper Blackstone Formation the
  • overlain by the Wapiabi Formation and underlain by the Blackstone Formation The formation is partly equivalent to the Kaskapau Formation Natural gas is produced
  • the Caribou Mountains. The Dunvegan Formation is conformably overlain by marine shales of the Kaskapau Formation in the Peace River Country and overlies
  • The Redknife Formation is a stratigraphical unit of Devonian age in the Western Canadian Sedimentary Basin. It takes the name from Redknife River, a tributary
  • the following formations Buckinghorse Formation is equivalent to the sum of Lepine Formation Scatter Formation and Garbutt Formation It occurs north - east
  • Mount Head Formation and Livingstone Formation in the Rocky Mountains by the Turner Valley Formation Shunda Formation and Pekisko Formation in the foothills
  • extends throughout the plains of the Peace River Country. The Pardonet Formation has its type locality at Pardonet Hill, on the south shore of the Williston
  • has been subdivided into numerous formations many which host major petroleum and natural gas reservoirs. The formations of the Elk Point Group are composed
  • Oil geological staff in 1950. The Formation is composed of crystalline and dolomitized limestone Cooking Lake Formation in off - reef areas, bituminous shale


                                     
  • Slave Point Formation and Waterways Formation in northeastern Alberta, with the Slave Point Formation and the lower Hay River Formation in the District
  • and siltstone. Pinnacle reefs develop in the Nisku Formation Oil is produced from the Nisku Formation in the Pembina oil field. The Winterburn Group reaches
  • The Duvernay Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin. It was first described in well Anglo Canadian
  • The Banff Formation is a stratigraphical unit of Devonian age in the Western Canadian Sedimentary Basin. It takes the name from the town of Banff, Alberta
  • The Montney Formation is a stratigraphical unit of Lower Triassic age in the Western Canadian Sedimentary Basin in British Columbia and Alberta. It takes
  • Debolt Formation It can be correlated with the Tunnel Mountain Formation the Kananaskis Formation the Mattson Formation and the Mount Head Formation of
  • The Leduc Formation is a stratigraphic unit of Late Devonian Frasnian age in the Western Canada Sedimentary Basin. It takes its name from the city of
  • The Baldonnel Formation is a stratigraphical unit of Carnian age in the Western Canadian Sedimentary Basin. It takes the name from the hamlet of Baldonnel
  • Retrieved 10 July 2014. Alberta Geological Survey, 2015. Alberta Table of Formations Alberta Energy Regulator Retrieved 26 June 2014. Glass, D.J. editor
  • The Cadomin Formation is a stratigraphic unit of Early Cretaceous Barremian to Aptian age in the western part of the Western Canada Sedimentary Basin
  • The Belloy Formation is a stratigraphical unit of Permian age in the Western Canadian Sedimentary Basin. It takes the name from the hamlet of Belloy
  • The Bluesky Formation is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin. It takes the name from the hamlet of Bluesky
                                     
  • The Exshaw Formation is a stratigraphic unit in the Western Canada Sedimentary Basin. It takes the name from the hamlet of Exshaw, Alberta in the Canadian
  • Gething Formation is a stratigraphic unit of Lower Cretaceous Aptian age in the Western Canada Sedimentary Basin. It is present in northeastern British
  • The Muskeg Formation is a geologic formation of Middle Devonian Givetian age in the Western Canada Sedimentary Basin. It extends from the plains of
  • The Wabamun Formation is a stratigraphic unit of Late Devonian Famennian age in the Western Canada Sedimentary Basin. It takes the name from Wabamun
  • The Debolt Formation is a stratigraphical unit of Meramecian age in the Western Canadian Sedimentary Basin. It takes the name from the hamlet of Debolt
  • The Kiskatinaw Formation is a stratigraphical unit of Mississippian age in the Western Canadian Sedimentary Basin. It takes the name from the Kiskatinaw
  • The Kakisa Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin. It takes the name from the Kakisa River, a tributary
  • The Doig Formation is a geologic formation of middle Triassic age in the Western Canadian Sedimentary Basin. It takes the name from Doig River, a tributary


Users also searched:

Formation, Kaskapau, Kaskapau Formation, kaskapau formation, stratigraphy of alberta. kaskapau formation,

Encyclopedic dictionary

Translation

Kaskapau Formation Visually.

Perdrix and Mount Hawk Formations. Shaftesbury and Dunvegan Formations, Kaskapau Formation consists of dark grey silty shale, These shales. Canadian Science Publishing. Cardium Shale Cardium Formation Cardium Oil Play Alberta Canada, Montana, Wapiabi Formation, Blackstone Formation, and the Kaskapau Formation. Allostratigraphy of the Kaskapau Formation Semantic Scholar. Shaftesbury, and Kaskapau formations in the northwestern Alberta subsurface Kaskapau Formation and are interpreted as being genetically related to the. Rotary Steerable Technology Creates Value in Western Canadian. The bones from this Kaskapau Formation Turonian about 90 million years old proved much older than any others found in western Canada to date. With such Следующая Войти Настройки.


Preliminary observations on the sedimentology of the doe creek.

At Liard river, the stratigraphic hiatus eliminates the underlying Lower ​Cardium sandstone, the Kaskapau formation, and the upper Dunvegan sandstones. Allostratigraphy of the Kaskapau Formation GeoScienceWorld. Abstract The Kaskapau Formation is a major, mudstone dominated syntectonic wedge deposited in Late Cretaceous time in the foredeep of the Western Canada​.


APS Folders 2007 Alberta Palaeontological Society.

Bhattacharya, J. and Walker, R.G. 1991, allostratigraphic subdivision of the Upper Cretaceous Dunvegan, Shaftesbury, and Kaskapau Formations in the. Get PDF Sequence stratigraphy and paleogeography of a. Biostratigraphy of the Cenomanian type Hazera formation M. Hamaoui, with a Sedimentology and source rock potential of the lower Kaskapau Formation. Near Watino, Alberta Canadian Science Publishing. The Cenomanian to earliest Turonian Cretaceous Kaskapau Formation in northwestern Alberta and adjacent British Columbia contains three.





The Lower Kaimur Porcellanite Vindhyan Supergroup is of.

Fossil marine actinopterygian fishes from the Kaskapau Formation Upper Cretaceous: Turonian near Watino, Alberta. Wilson, Mark V. H. Chalifa, Yael. Regional Hydrological Assessment MPWA State of the Watershed. The Kaskapau Formation is a geological formation in North America whose strata date back to the Late Cretaceous. The name derives from kaskapahtew. The Lower Kaskapau Formation Cenomanian A Multiple. E mail: gplint@. ABSTRACT. The Middle Turonian Kaskapau Formation in the Rocky Mountain. Foothills of northeastern British Columbia comprises up.


Cardium Formation of the Foothills of Northeastern British OneMine.

Turonian fossil marine fishes occur at several localities near Watino, Alberta, in sandstones and in shale concretions of the Vimy Member, Kaskapau Formation. Middle Turonian dinosaur paleoenvironments in. Numerous isolated euselachian teeth were recovered from the early Turonian Kaskapau Formation situated in northwestern Alberta, Canada.


File:Kaskapau media Commons.

The Cenomanian to earliest Turonian Upper Cretaceous Kaskapau Formation in northwestern Alberta and adjacent British Columbia contains. Allostratigraphic subdivision of the Upper Cretaceous Dunvegan. Middle Turonian dinosaur paleoenvironments in the Upper Cretaceous Kaskapau Formation, northeast British Columbia. Canadian Journal of Earth Sciences.


Fossil marine actinopterygian fishes from the Kaskapau Formation.

Bedload Transport of Mud Across A Wide, Storm Influenced Ramp: Cenomanian ​Turonian Kaskapau Formation, Western Canada Foreland Basin - Reply. Kaskapau Formation Landmark NA - explore top10places near you. Fossil marine actinopterygin fishes from the Kaskapau formation Upper. Cretaceous: Turonian near Watine, Alberta 1989. The Coelacanth.


Postfracture Formation Evaluation in the Valhalla Field, Alberta.

Sandstone Formation of the Kaimur Group, Son Valley, central India. storm ​influenced ramp: Cenomanian Turonian Kaskapau Formation,. Sedimentology and source rock potential of the lower kaskapau. ACROSS A COASTAL PLAIN: MIDDLE TURONIAN KASKAPAU FORMATION, BRITISH COLUMBIA, CANADA PALAIOS December 1, 2006 7 570.


Sequence stacking patterns in the Western Canada foredeep.

The Cenomanian Doe Creek Member comprises sand dominated units within the Kaskapau Formation shale. The sandstones are of reservoir. Geology of Alberta: Birch Mountains Kimberlite Field, Buffalo Head. KEYWORDS: Mud clasts, classification, formation, transport mechanisms storm​ influenced ramp: cenomanian–turonian kaskapau Formation,. Cardium Shale Cardium Oil Formation Cardium Shale Map. And Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin. 2019Bulletin of Canadian Petroleum Geology.





Depositional processes and environments of the GeoConvention.

Get this from a library! Cenomanian Turonian foraminifera from Kaskapau Formation, Peace River Area, Western Canada. John Hallett Wall University of. Publications – Lisa G. Buckley, Ph.D. This conversation with Bruce Hart is about fractures and folds in the Cardium Formation due to underlying Kaskapau faults, based on his study. Cenomanian Turonian Upper Cretaceous foraminifera from the. Title. Cenomanian Turonian foraminifera from Kaskapau Formation, Peace River Area,. Late Cenomanian Turonian Kaskapau Formation AGRIS fao. Middle Turonian dinosaur paleoenvironments in the Upper Cretaceous Kaskapau Formation, northeast British Columbia. J. R. Rylaarsdam, B. L. Varban, A. G.


Cenomanian Turonian foraminifera from Kaskapau Formation.

The Doe Creek sandstone unit is located in the lower part of the Kaskapau Formation, Upper Cretaceous. Doe Creek is a well known conventional light oil play. McCandless IKC Poster 20170828.cdr MCC Geoscience Inc. Cardium Formation. The Cardium sandstone and Muskiki shale are replacing the upper parts of the Kaskapau Formation in the south. On the Accumulation of Mud Science. The Kaskapau Formation is a geological formation in North America whose strata date back to the Late name derives from kaskapahtew. SEPM Strata. Kaskapau Formation northern foothills and of the Blackstone. Formation ​southern foothills, and the Fish Scales and Belle. Fourche formations southern.


A High Latitude Epilithozoan Fauna on Quartzite Clasts and JStor.

Abstract The Kaskapau and Cardium Formations span Late Cenomanian to Early The studied portion of the Kaskapau Formation spans ca. Circulation, salinity, and dissolved oxygen in the Cretaceous North. Palaeoenvironments, palaeogeography, and physiography of a large, shallow, muddy ramp: Late Cenomanian Turonian Kaskapau Formation, Western Canada​. A Large Ornithurine Bird Tingmiatornis arctica from the Turonian. Formation, Viking Formation, Grand Mesa, Stoddart Group, McMurray Formation, Kaskapau Formation, Columbia Icefield, Montney Formation, Mancos Shale,.


Free and no ads
no need to download or install

Pino - logical board game which is based on tactics and strategy. In general this is a remix of chess, checkers and corners. The game develops imagination, concentration, teaches how to solve tasks, plan their own actions and of course to think logically. It does not matter how much pieces you have, the main thing is how they are placement!

online intellectual game →