FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023172148> ?p ?o ?g. }

• W2023172148 endingPage "276" @default.
• W2023172148 startingPage "263" @default.
• W2023172148 abstract "A regional mapping program associated with radiometric age dating has provided evidence of seven deformation pulses in the Andean orogenic cycle in part of southern Peru. These are the Peruvian (Late Cretaceous), Incaic (Eocene), and five Quechua phases defined as D1 to D5. The D1 phase (early Oligocene) folded molasse deposits in the Western Cordillera; the D2 phase (late Oligocene to early Miocene) folded volcanics of the Western Cordillera; the D3 phase (middle Miocene) folded the molasse deposits in the Altiplano; the D4 (late Miocene) folded lacustrine sediments in the central part of the Western Cordillera; and the D5 phase was a major gravity slide in the Altiplano. Several faults and fault zones, known as the Chupa, Calapuja, Lagunillas, and Laraqueri Faults, are identified. They form the boundaries to Paleozoic basement blocks which appear to have acted as buttresses or barriers to the penetration of some deformation events. In the case of the D5 phase, the gravity slide was preceded by uplift and tilting of a Paleozoic block. Un programa regional de mapeo asociado con dataciones radiométricas ha proporcionado la evidencia de siete pulsos de deformación en el ciclo orogénico Andino en la parte sur del Perú. Estos ciclos incluyen el Peruano (Cretácico superior), Incaico (Eoceno) y cinco fases sel Quechua definidos como D1 a D5. La fase D1 (Oligoceno temprano) plegó los depósitos de molasa de la Cordillera Occidental; la fade D2 (Oligoceno tardío-Mioceno temprano) plegó las rocas volcánicas de la Cordillera Occidental; la fase D3 (Mioceno medio) plegó los depósitos de molasa del Altiplano; la fase D4 (Mioceno tardió) plegó los sedimentos lacustres de la parte occidental de la Cordillera Occidental; y fase D5 (Mioceno tardío) fue un deslizamiento gravitacional en el Altiplano. Varias fallas y zonas de falla, conocidas como las fallas de Chupa, Calapuja, Lagunillas y Laraqueri, fueron identificadas. Los límites de bloques Paleozoicos aparentan haber sido contrafuertes u obstáculos contra la penetración de algunos eventos de deformación. En el caso de la fase D5, el deslizamiento de gravedad fue antecedido por levantamiento y basculamiento de un bloque del basamento Paleozoico." @default.
• W2023172148 created "2016-06-24" @default.
• W2023172148 creator A5003721147 @default.
• W2023172148 creator A5075891680 @default.
• W2023172148 creator A5079702214 @default.
• W2023172148 date "1989-01-01" @default.
• W2023172148 modified "2023-10-14" @default.
• W2023172148 title "Deformation events in the Andean orogenic cycle in the Altiplano and Western Cordillera, southern Peru" @default.
• W2023172148 cites W1970920191 @default.
• W2023172148 cites W1973981261 @default.
• W2023172148 cites W1985528315 @default.
• W2023172148 cites W1985930163 @default.
• W2023172148 cites W1996222542 @default.
• W2023172148 cites W1998060081 @default.
• W2023172148 cites W2015077256 @default.
• W2023172148 cites W2025889286 @default.
• W2023172148 cites W2038114342 @default.
• W2023172148 cites W2054780375 @default.
• W2023172148 cites W2064542021 @default.
• W2023172148 cites W2088789223 @default.
• W2023172148 cites W2167167009 @default.
• W2023172148 cites W2317441075 @default.
• W2023172148 doi "https://doi.org/10.1016/0895-9811(89)90033-3" @default.
• W2023172148 hasPublicationYear "1989" @default.
• W2023172148 type Work @default.
• W2023172148 sameAs 2023172148 @default.
• W2023172148 citedByCount "18" @default.
• W2023172148 countsByYear W20231721482014 @default.
• W2023172148 countsByYear W20231721482018 @default.
• W2023172148 countsByYear W20231721482021 @default.
• W2023172148 countsByYear W20231721482023 @default.
• W2023172148 crossrefType "journal-article" @default.
• W2023172148 hasAuthorship W2023172148A5003721147 @default.
• W2023172148 hasAuthorship W2023172148A5075891680 @default.
• W2023172148 hasAuthorship W2023172148A5079702214 @default.
• W2023172148 hasConcept C109007969 @default.
• W2023172148 hasConcept C114793014 @default.
• W2023172148 hasConcept C12294951 @default.
• W2023172148 hasConcept C127313418 @default.
• W2023172148 hasConcept C13106087 @default.
• W2023172148 hasConcept C151730666 @default.
• W2023172148 hasConcept C166957645 @default.
• W2023172148 hasConcept C193748577 @default.
• W2023172148 hasConcept C205649164 @default.
• W2023172148 hasConcept C2779421809 @default.
• W2023172148 hasConcept C2781297371 @default.
• W2023172148 hasConcept C67422804 @default.
• W2023172148 hasConcept C77928131 @default.
• W2023172148 hasConceptScore W2023172148C109007969 @default.
• W2023172148 hasConceptScore W2023172148C114793014 @default.
• W2023172148 hasConceptScore W2023172148C12294951 @default.
• W2023172148 hasConceptScore W2023172148C127313418 @default.
• W2023172148 hasConceptScore W2023172148C13106087 @default.
• W2023172148 hasConceptScore W2023172148C151730666 @default.
• W2023172148 hasConceptScore W2023172148C166957645 @default.
• W2023172148 hasConceptScore W2023172148C193748577 @default.
• W2023172148 hasConceptScore W2023172148C205649164 @default.
• W2023172148 hasConceptScore W2023172148C2779421809 @default.
• W2023172148 hasConceptScore W2023172148C2781297371 @default.
• W2023172148 hasConceptScore W2023172148C67422804 @default.
• W2023172148 hasConceptScore W2023172148C77928131 @default.
• W2023172148 hasIssue "3" @default.
• W2023172148 hasLocation W20231721481 @default.
• W2023172148 hasOpenAccess W2023172148 @default.
• W2023172148 hasPrimaryLocation W20231721481 @default.
• W2023172148 hasRelatedWork W2022616238 @default.
• W2023172148 hasRelatedWork W2028466704 @default.
• W2023172148 hasRelatedWork W2072296979 @default.
• W2023172148 hasRelatedWork W2084903896 @default.
• W2023172148 hasRelatedWork W2266529721 @default.
• W2023172148 hasRelatedWork W2557783519 @default.
• W2023172148 hasRelatedWork W2762077784 @default.
• W2023172148 hasRelatedWork W3082404080 @default.
• W2023172148 hasRelatedWork W3169661906 @default.
• W2023172148 hasRelatedWork W4226033492 @default.
• W2023172148 hasVolume "2" @default.
• W2023172148 isParatext "false" @default.
• W2023172148 isRetracted "false" @default.
• W2023172148 magId "2023172148" @default.
• W2023172148 workType "article" @default.