This HTML5 document contains 95 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
dbohttp://dbpedia.org/ontology/
foafhttp://xmlns.com/foaf/0.1/
n4http://dbpedia.org/resource/File:
n16https://global.dbpedia.org/id/
dbthttp://dbpedia.org/resource/Template:
rdfshttp://www.w3.org/2000/01/rdf-schema#
n7http://commons.wikimedia.org/wiki/Special:FilePath/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
wikipedia-enhttp://en.wikipedia.org/wiki/
dbphttp://dbpedia.org/property/
dbchttp://dbpedia.org/resource/Category:
provhttp://www.w3.org/ns/prov#
xsdhhttp://www.w3.org/2001/XMLSchema#
wikidatahttp://www.wikidata.org/entity/
dbrhttp://dbpedia.org/resource/

Statements

Subject Item
dbr:Cook_Inlet_Basin
rdf:type
owl:Thing
rdfs:label
Cook Inlet Basin
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.
foaf:depiction
n7:Cook_Inlet_Basin_Alaska.jpg n7:Cook_Inlet_Major_Fault_Systems.jpg n7:Yakutat_Subduction.gif n7:Cook_Inlet_Oil_Fields.png n7:The_Cook_Inlet_Basin_Location.jpg n7:Annual-Alaska-South-Field-Production-of-Crude-Oil-20170327.png n7:Generalized_Stratigraphic_Column_of_the_Cook_Inlet_Basin,_Alaska.png
dcterms:subject
dbc:Bodies_of_water_of_Kenai_Peninsula_Borough,_Alaska dbc:Bodies_of_water_of_Anchorage,_Alaska dbc:Estuaries_of_Alaska
dbo:wikiPageID
53907418
dbo:wikiPageRevisionID
1091780287
dbo:wikiPageWikiLink
dbr:Miocene dbr:Kenai_Peninsula dbr:Abandoned_wells dbr:Mesozoic dbr:Kenai_Group dbr:Kenai_Mountains n4:The_Cook_Inlet_Basin_Location.jpg dbr:River_delta dbr:Normal_fault dbr:Gulf_of_Alaska dbr:Facies dbr:Susitna_River dbr:Triassic dbr:Flysch dbr:North_American_Plate dbr:Lithology n4:Annual-Alaska-South-Field-Production-of-Crude-Oil-20170327.png n4:Yakutat_Subduction.gif dbr:Fold_(geology) dbr:Matanuska_Valley dbr:Batholith dbr:Cretaceous dbr:Dike_(geology) dbr:Marine_transgression dbr:Estuary dbr:Hydrocarbon_exploration dbr:Tertiary_(geology) dbr:Pacific_Plate dbr:Stratigraphy dbr:Oligocene dbr:Shale dbr:Cook_Inlet dbr:Sedimentary_rock dbr:Quaternary dbr:Island_arc dbr:Chugach_Mountains dbr:Pluton dbr:Igneous_rock dbc:Bodies_of_water_of_Kenai_Peninsula_Borough,_Alaska dbr:Convergent_boundary dbr:Tertiary dbr:Cenozoic dbc:Bodies_of_water_of_Anchorage,_Alaska dbr:Tuff dbr:Anticline dbr:Turbidite dbr:Metamorphic_rock dbr:Aleutian_Trench dbr:Fault_(geology) dbr:Siltstone n4:Cook_Inlet_Oil_Fields.png dbr:Alaska_Peninsula dbr:Accretionary_wedge n4:Cook_Inlet_Basin_Alaska.jpg dbr:Alaska n4:Cook_Inlet_Major_Fault_Systems.jpg dbc:Estuaries_of_Alaska dbr:Alaska_Range dbr:Debris_flow dbr:Unconformity dbr:Conglomerate_(geology) dbr:Subduction dbr:Sill_(geology) dbr:Country_rock_(geology) dbr:Ring_of_Fire dbr:Permian dbr:Jurassic dbr:Becharof_Lake n4:Generalized_Stratigraphic_Column_of_the_Cook_Inlet_Basin,_Alaska.png dbr:Kachemak_Bay dbr:Sandstone
owl:sameAs
wikidata:Q30687670 n16:2qxFj
dbp:wikiPageUsesTemplate
dbt:Coord_missing dbt:Authority_control
dbo:thumbnail
n7:The_Cook_Inlet_Basin_Location.jpg?width=300
dbo: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.
prov:wasDerivedFrom
wikipedia-en:Cook_Inlet_Basin?oldid=1091780287&ns=0
dbo:wikiPageLength
17465
foaf:isPrimaryTopicOf
wikipedia-en:Cook_Inlet_Basin