About: Cook Inlet Basin

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The Cook Inlet Basin is a northeast-trending collisional forearc basin that stretches from the Gulf of Alaska into South central Alaska, just east of the Matanuska Valley. It is located in the arc-trench gap between the Alaska-Aleutian Range batholith and contains roughly 80,000 cubic miles of sedimentary rocks. These sediments are mainly derived from Triassic, Jurassic and Cretaceous sediments.

Attributes	Values
rdf:type	Thing
rdfs:label	Cook Inlet Basin (en)
rdfs:comment	The Cook Inlet Basin is a northeast-trending collisional forearc basin that stretches from the Gulf of Alaska into South central Alaska, just east of the Matanuska Valley. It is located in the arc-trench gap between the Alaska-Aleutian Range batholith and contains roughly 80,000 cubic miles of sedimentary rocks. These sediments are mainly derived from Triassic, Jurassic and Cretaceous sediments. (en)
foaf:depiction
dcterms:subject	Estuaries of Alaska Bodies of water of Kenai Peninsula Borough, Alaska Bodies of water of Anchorage, Alaska
Wikipage page ID	53907418 (xsd:integer)
Wikipage revision ID	1091780287 (xsd:integer)
Link from a Wikipage to another Wikipage	Quaternary Metamorphic rock Becharof Lake Anticline Permian Ring of Fire Debris flow Sedimentary rock Cook Inlet Cretaceous Chugach Mountains Miocene Conglomerate (geology) Estuaries of Alaska Convergent boundary Batholith Fault (geology) Igneous rock Pluton Tuff Cenozoic Bodies of water of Kenai Peninsula Borough, Alaska Triassic Alaska Alaska Range Facies North American Plate Pacific Plate Dike (geology) Flysch Fold (geology) Island arc Kenai Group Kenai Mountains Kenai Peninsula Unconformity River delta Marine transgression Gulf of Alaska Country rock (geology) Hydrocarbon exploration Subduction Siltstone Accretionary wedge Alaska Peninsula Aleutian Trench Jurassic Kachemak Bay Susitna River Tertiary Turbidite Tertiary (geology) Mesozoic Oligocene Bodies of water of Anchorage, Alaska Sandstone Shale Sill (geology) Estuary Lithology Stratigraphy Normal fault Matanuska Valley Abandoned wells
sameAs	Cook Inlet Basin Cook Inlet Basin
dbp:wikiPageUsesTemplate	dbt:Authority_control dbt:Coord_missing
thumbnail	wiki-commons:Special:FilePath/The_Cook_Inlet_Basin_Location.jpg?width=300
has abstract	The Cook Inlet Basin is a northeast-trending collisional forearc basin that stretches from the Gulf of Alaska into South central Alaska, just east of the Matanuska Valley. It is located in the arc-trench gap between the Alaska-Aleutian Range batholith and contains roughly 80,000 cubic miles of sedimentary rocks. These sediments are mainly derived from Triassic, Jurassic and Cretaceous sediments. The region is heavily influenced by two major tectonic elements which are still active in the area today. The western side of the basin lies directly above the Aleutian subduction zone where the Pacific Plate is subducting beneath the North American Plate. However the eastern side of the basin overlays the subduction of the Yakutat microplate beneath the North American plate. Active subduction along various sides of the basin produce regional compression that lead to major folding, faulting and the formation of anticline structures within the sediments. Anticline structures provide ideal hydrocarbon traps, and so the Cook Inlet Basin is widely known for its hydrocarbon accumulations and its overall production of oil and gas. (en)
prov:wasDerivedFrom	wikipedia-en:Cook_Inlet_Basin?oldid=1091780287&ns=0
page length (characters) of wiki page	17465 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Cook_Inlet_Basin
is Link from a Wikipage to another Wikipage of	Denise M. Stone The Cook Inlet Basin Alaska blackfish
is Wikipage redirect of	The Cook Inlet Basin
is foaf:primaryTopic of	wikipedia-en:Cook_Inlet_Basin

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