About: Guaymas Fault

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The Guaymas Fault, named for the city of Guaymas, Sonora, Mexico, is a major right lateral-moving transform fault which runs along the seabed of the Gulf of California. It is an integral part of the Gulf of California Rift Zone, the northern extremity of the East Pacific Rise. The Guaymas Fault runs from the located at the southern end of the San Lorenzo Fault (the next transform to the north), and extends southward to the Guaymas Basin, a heavily sedimented rift which includes both continental and oceanic crust and contains numerous hydrothermal vents.

Attributes	Values
rdfs:label	Guaymas Fault (en) Faglia di Guaymas (it)
rdfs:comment	The Guaymas Fault, named for the city of Guaymas, Sonora, Mexico, is a major right lateral-moving transform fault which runs along the seabed of the Gulf of California. It is an integral part of the Gulf of California Rift Zone, the northern extremity of the East Pacific Rise. The Guaymas Fault runs from the located at the southern end of the San Lorenzo Fault (the next transform to the north), and extends southward to the Guaymas Basin, a heavily sedimented rift which includes both continental and oceanic crust and contains numerous hydrothermal vents. (en) La faglia di Guaymas è una la più grande delle faglie trasformi a movimento laterale destro presenti sul fondale marino del Golfo di California, nell'Oceano Pacifico, al largo della costa dello stato messicano di Sonora. La faglia, che prende il nome dalla città messicana di Guaymas, fa parte della zona di rift del Golfo di California, l'estensione settentrionale della dorsale del Pacifico orientale, e collega tra loro il , situato a all'estremità meridionale della , a nord, e il bacino di Guaymas, un rift ricco di sorgenti idrotermali, a sud. (it)
dcterms:subject	Gulf of California Geography of Mexico Strike-slip faults Geology of Mexico
Wikipage page ID	27081565 (xsd:integer)
Wikipage revision ID	1119410590 (xsd:integer)
Link from a Wikipage to another Wikipage	East Pacific Rise Continental crust Delfin Basin Fault (geology) Gulf of California Ballenas Fault Rift Guaymas Gulf of California Geography of Mexico Hydrothermal vent Strike-slip faults Geology of Mexico Transform fault Sonora Guaymas Basin Mexico Gulf of California Rift Zone Oceanic crust dbr:San_Pedro_Martir_Basin
Link from a Wikipage to an external page	http://search.datapages.com/data/open/offer.do%3Ftarget=%2Fspecpubs%2Fhistory1%2Fdata%2Fa114%2Fa114%2F0001%2F0700%2F0709.htm http://aem.asm.org/cgi/reprint/55/11/2832.pdf http://satori.geociencias.unam.mx/18-2/(1)Escalona.pdf http://www.data.scec.org/NARS-Baja/NARS-Baja.pdf https://books.google.com/books%3Fid=S6H6KVKdlzsC&pg=PA149
sameAs	Guaymas Fault Guaymas Fault Guaymas Fault Guaymas Fault Guaymas Fault
dbp:wikiPageUsesTemplate	dbt:Tectonics-stub dbt:Mexico-geo-stub dbt:Reflist dbt:Short_description dbt:Central_America_plates
has abstract	The Guaymas Fault, named for the city of Guaymas, Sonora, Mexico, is a major right lateral-moving transform fault which runs along the seabed of the Gulf of California. It is an integral part of the Gulf of California Rift Zone, the northern extremity of the East Pacific Rise. The Guaymas Fault runs from the located at the southern end of the San Lorenzo Fault (the next transform to the north), and extends southward to the Guaymas Basin, a heavily sedimented rift which includes both continental and oceanic crust and contains numerous hydrothermal vents. The Guaymas Fault is often grouped together with the three transform faults to its north as the Guaymas Transform Fault System. These faults are, from north to south, the Ballenas, Partida, San Lorenzo, and Guaymas. This system of fault extends some 325 km, linking the Delfin Basin in the north with the Guaymas Basin in the south. (en) La faglia di Guaymas è una la più grande delle faglie trasformi a movimento laterale destro presenti sul fondale marino del Golfo di California, nell'Oceano Pacifico, al largo della costa dello stato messicano di Sonora. La faglia, che prende il nome dalla città messicana di Guaymas, fa parte della zona di rift del Golfo di California, l'estensione settentrionale della dorsale del Pacifico orientale, e collega tra loro il , situato a all'estremità meridionale della , a nord, e il bacino di Guaymas, un rift ricco di sorgenti idrotermali, a sud. In letteratura la faglia di Guaymas è spesso raggruppata con altre tre faglie trasformi a nord di essa nel sistema di faglie chiamato sistema di faglia trasforme di Guaymas. Queste tre faglie sono, da nord a sud, la faglia di Ballenas, la e la ed il sistema di faglia che esse formano assieme alla faglia di Guaymas si estende per circa 325 km collegando il bacino di Delfin, a nord, con il bacino di Guaymas, a sud. Il terremoto di grande intensità più recente registrato lungo questa faglia è stato quello del 12 aprile 2012, che ha raggiunto una magnitudo momento di 6,9. (it)
prov:wasDerivedFrom	wikipedia-en:Guaymas_Fault?oldid=1119410590&ns=0
page length (characters) of wiki page	2550 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Guaymas_Fault
is Link from a Wikipage to another Wikipage of	List of fault zones List of seismic faults in Mexico Ballenas Fault Guaymas Basin Gulf of California Rift Zone Guaymas Transform Fault System
is Wikipage redirect of	Guaymas Transform Fault System
is foaf:primaryTopic of	wikipedia-en:Guaymas_Fault

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