About: Lotena Formation

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The Lotena Formation is a geologic formation dated from the Late Callovian to Early Oxfordian in the Neuquén Basin in Mendoza Province, Argentina. The formation, first defined by Weaver in 1931 and named after Cerro Lotena, consists of fluvial conglomerates, calcareous sandstones and marine limestones and shales. The Lotena Formation is overlain by the and overlies the of the . Initially, the fossil find of the pterosaur Herbstosaurus pigmaeus was reported from the formation, but this fossil was found in the younger Vaca Muerta. The formation is a reservoir rock in the Neuquén Basin.

Property	Value
dbo:abstract	La Formación Lotena es una formación geológica definida por Charles E. Weaver, que se encuentra en la provincia de Mendoza. Está compuesta por conglomerados, areniscas, pelitas y limolitas. mediante análisis estratigráficos, paleoambientales y secuenciales de la Formación se reconocieron tres intervalos con características distintivas, que se denominan, Miembro La Estrechura, Miembro Pichanal y Miembro El Vado. Sobre la base al análisis micropaleontológico ( y ) y estratigráfico, se estima que la edad de la Formación Lotena en la Subcuenca de Picún Leufú abarcaría desde el Caloviano medio hasta el Oxfordiano Tardío- Kimmeridgiano Temprano. (es) The Lotena Formation is a geologic formation dated from the Late Callovian to Early Oxfordian in the Neuquén Basin in Mendoza Province, Argentina. The formation, first defined by Weaver in 1931 and named after Cerro Lotena, consists of fluvial conglomerates, calcareous sandstones and marine limestones and shales. The Lotena Formation is overlain by the and overlies the of the . Initially, the fossil find of the pterosaur Herbstosaurus pigmaeus was reported from the formation, but this fossil was found in the younger Vaca Muerta. The formation is a reservoir rock in the Neuquén Basin. (en)
dbo:wikiPageExternalLink	https://www.researchgate.net/profile/H_Leanza/publication/262934512_Hoja_Geologica_3972-II_LONCOPUE_provincia_del_Neuquen/links/00b7d5395e4e634a10000000/Hoja-Geologica-3972-II-LONCOPUE-provincia-del-Neuquen.pdf http://www.scielo.cl/pdf/andgeol/v38n1/art09.pdf
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dbp:age	dbr:Callovian dbr:Oxfordian_(stage) ~ (en)
dbp:country	Argentina (en)
dbp:name	Lotena Formation (en)
dbp:namedby	Weaver (en)
dbp:namedfor	Cerro Lotena (en)
dbp:otherlithology	dbr:Limestone dbr:Shale
dbp:overlies	dbr:Cuyo_Group,_Argentina Lajas Formation (en)
dbp:period	Oxfordian (en)
dbp:prilithology	dbr:Conglomerate_(geology) dbr:Sandstone
dbp:region	dbr:Neuquén_Basin Mendoza Province & Neuquén Province (en) Northern Patagonia (en)
dbp:subunits	La Estrechura, El Pichanal & El Vado Members (en)
dbp:type	dbr:Geological_formation
dbp:underlies	dbr:La_Manga_Formation
dbp:unitof	dbr:Lotena_Group
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dbp:yearTs	1931 (xsd:integer)
dcterms:subject	dbc:Oxfordian_Stage dbc:Jurassic_System_of_South_America dbc:Late_Jurassic_South_America dbc:Middle_Jurassic_South_America dbc:Conglomerate_formations dbc:Jurassic_Argentina dbc:Geology_of_Neuquén_Province dbc:Geology_of_Patagonia dbc:Neuquén_Basin dbc:Callovian_Stage dbc:Geologic_formations_of_Argentina dbc:Geology_of_Mendoza_Province dbc:Sandstone_formations dbc:Fluvial_deposits dbc:Limestone_formations dbc:Shale_formations dbc:Reservoir_rock_formations
gold:hypernym	dbr:Formation
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rdfs:comment	The Lotena Formation is a geologic formation dated from the Late Callovian to Early Oxfordian in the Neuquén Basin in Mendoza Province, Argentina. The formation, first defined by Weaver in 1931 and named after Cerro Lotena, consists of fluvial conglomerates, calcareous sandstones and marine limestones and shales. The Lotena Formation is overlain by the and overlies the of the . Initially, the fossil find of the pterosaur Herbstosaurus pigmaeus was reported from the formation, but this fossil was found in the younger Vaca Muerta. The formation is a reservoir rock in the Neuquén Basin. (en) La Formación Lotena es una formación geológica definida por Charles E. Weaver, que se encuentra en la provincia de Mendoza. Está compuesta por conglomerados, areniscas, pelitas y limolitas. mediante análisis estratigráficos, paleoambientales y secuenciales de la Formación se reconocieron tres intervalos con características distintivas, que se denominan, Miembro La Estrechura, Miembro Pichanal y Miembro El Vado. (es)
rdfs:label	Formación Lotena (es) Lotena Formation (en)
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geo:lat	-38.599998 (xsd:float)
geo:long	-70.199997 (xsd:float)
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