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Statements

Subject Item
dbr:Maria_fold_and_thrust_belt
rdf:type
dbo:Dam dbo:AnatomicalStructure
rdfs:label
Maria fold and thrust belt Cinturó de plecs i falles de Maria
rdfs:comment
El cinturó de plecs i falles de Maria (MFTB per les seves inicials en anglès) és una part de l'orogen de la Serralada Nord-americana, les estructures geològiques del qual acomoden més o menys en l'eix nord–sud, amb vergència nord-oest - sud-est, un escurçament de l'escorça d'edat Mesozoica. En contrast amb la resta de la Serralada, en que l'escurçament és predominantment est–oest. Les seves estructures associades es troben exposades en una sèrie de serralades al sud-est de Califòrnia i a l'Arizona occidental. Moltes de les estructures profundes del MFTB han estat exposades a causa de l'extensió est–oest a nord-est-sud-oest durant el Cenozoic extensió d'edat i l'exhumació per l'erosió. The Maria fold and thrust belt (MFTB) is a portion of the North American Cordillera orogen in which geological structures accommodate roughly north–south to northwest-southeast vergent Mesozoic age crustal shortening. This lies in contrast to the remainder of the Cordillera, in which shortening is predominantly east–west. Structures associated with the Maria Fold and Thrust Belt are exposed in a series of mountain ranges in southeastern California and western Arizona. Many of the deep structures of the MFTB have been exposed due to east–west to northeast-southwest Cenozoic age extension and unroofing.
dbp:name
Maria Fold-and-Thrust-Belt
dcterms:subject
dbc:Geology_of_California dbc:Geology_of_Arizona dbc:Mountain_ranges_of_the_Colorado_Desert dbc:Mountain_ranges_of_the_Lower_Colorado_River_Valley dbc:Mountain_ranges_of_Mohave_County,_Arizona dbc:Mountain_ranges_of_Southern_California dbc:North_American_Cordillera dbc:Mountain_ranges_of_La_Paz_County,_Arizona dbc:Mountain_ranges_of_the_Mojave_Desert dbc:Orogeny dbc:Geography_of_San_Bernardino_County,_California dbc:Geography_of_Riverside_County,_California dbc:Mountain_ranges_of_the_Sonoran_Desert dbc:Basin_and_Range_Province dbc:Geography_of_Imperial_County,_California dbc:Mountain_ranges_of_Arizona
dbo:wikiPageID
19489765
dbo:wikiPageRevisionID
1071532344
dbo:wikiPageWikiLink
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dbo:wikiPageExternalLink
n17:index.html n18:tectonics.html
owl:sameAs
dbpedia-ca:Cinturó_de_plecs_i_falles_de_Maria n11:4rGdZ n12:ماريا_حزام_الطى_والدفع freebase:m.04n2wnx wikidata:Q6761704
dbp:wikiPageUsesTemplate
dbt:Infobox_landform dbt:Coord_missing dbt:Convert dbt:Reflist dbt:Short_description dbt:California_Faults dbt:Commons_category
dbp:location
San Bernardino County-CA Mohave County-AZ- La Paz County-AZ-, Mojave Desert-NW—Sonoran Desert-SE, California, United States
dbo:abstract
El cinturó de plecs i falles de Maria (MFTB per les seves inicials en anglès) és una part de l'orogen de la Serralada Nord-americana, les estructures geològiques del qual acomoden més o menys en l'eix nord–sud, amb vergència nord-oest - sud-est, un escurçament de l'escorça d'edat Mesozoica. En contrast amb la resta de la Serralada, en que l'escurçament és predominantment est–oest. Les seves estructures associades es troben exposades en una sèrie de serralades al sud-est de Califòrnia i a l'Arizona occidental. Moltes de les estructures profundes del MFTB han estat exposades a causa de l'extensió est–oest a nord-est-sud-oest durant el Cenozoic extensió d'edat i l'exhumació per l'erosió. The Maria fold and thrust belt (MFTB) is a portion of the North American Cordillera orogen in which geological structures accommodate roughly north–south to northwest-southeast vergent Mesozoic age crustal shortening. This lies in contrast to the remainder of the Cordillera, in which shortening is predominantly east–west. Structures associated with the Maria Fold and Thrust Belt are exposed in a series of mountain ranges in southeastern California and western Arizona. Many of the deep structures of the MFTB have been exposed due to east–west to northeast-southwest Cenozoic age extension and unroofing. In some parts of this fold-and-thrust-belt region, the extension resulted in the emplacement of metamorphic core complexes, the 'type example' of which is defined by the Whipple Mountains in southeastern California.
gold:hypernym
dbr:Portion
prov:wasDerivedFrom
wikipedia-en:Maria_fold_and_thrust_belt?oldid=1071532344&ns=0
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7805
foaf:isPrimaryTopicOf
wikipedia-en:Maria_fold_and_thrust_belt