FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1566140969> ?p ?o ?g. }

• W1566140969 endingPage "150" @default.
• W1566140969 startingPage "123" @default.
• W1566140969 abstract "Abstaract Jurassic and Early Cretaceous stratigraphic data from terranes in Central Mexico situated southwest of the Walper Megashear demonstrate similar records of paleobathymetry and tectonic transport. In general, each of these terranes shows the same paleobathymetric fingerprint: (1) marine deposition at inner neritic depths during the Callovian to early Oxfordian (Middle to Late Jurassic); (2) marine deposition at outer neritic depths during the late Oxfordian (Late Jurassic); (3) sudden deepening to bathyal or upper abyssal depths (ACD = aragonite compensation level) from the early Kimmeridgian (Late Jurassic) until the end of the Cretaceous. This paleobathymetric fingerprint differs markedly from that occurring to the east-northeast of the Walper Megashear in the Coahuiltecano terrane (emended herein: Sierra Madre Oriental terrane). In the Coahuiltecano terrane (e.g., Peregrina Canyon near C. Victoria, Tamps.), no Mesozoic marine deposits older than late Oxfordian occur. The paleobathymetric fingerprint of this terrane was (1) inner neritic during the late Oxfordian (Late Jurassic) to Barremian (Early Cretaceous) and (2) bathyal to abyssal during the remainder of the Cretaceous (Aptian to Maastrichtian). Though varying in detail, each succession that has been examined in the mosaic of suspect terranes to the southwest of the Walper Megashear shows evidence of tectonic transport from higher latitudes to lower latitudes during the late Middle Jurassic, the Late Jurassic, and the Early Cretaceous. For example, the paleolatitudinal signature of the San Pedro del Gallo terrane (Durango) supplied by faunal data (radiolarians and megafossils) and preliminary paleomagnetic data indicates that this terrane was transported tectonically from higher paleolatitudes (Southern Boreal Province: 40°N) during the Late Jurassic (Oxfordian) to lower paleolatitudes (Tethyan Realm: Northern Tethyan Province) by the Early Cretaceous (Berriasian). The Jurassic and Lower Cretaceous successions at Mazapil (Zacatecas), Sierra de la Caja (Zacatecas), Sierra de Zuloaga (Zacatecas), Symon (Durango), and Sierra de Catorce (San Luis Potosi) are all genetically related to that at San Pedro del Gallo. They are regarded as representing dismembered remnants of the San Pedro del Gallo terrane. Faunal data (radiolarians and megafossils) from the Mazapil succession (Sierra Santa Rosa) indicate that this remnant of the San Pedro del Gallo terrane was situated at Southern Boreal paleolatitudes (>30°N) during the Oxfordian and Kimmeridgian and at Northern Tethyan paleolatitudes (22 to 29°N) during the Tithonian and Berriasian. Preliminary paleomagnetic data from the upper Tithonian to Berriasian part of the Mazapil succession indicates 25°N. Farther to the southeast (San Luis Potosi, Hidalgo, Veracruz, Puebla) in the Huayacocotla segment of the Sierra Madre Oriental, previous investigations indicate tectonic transport from Southern Boreal paleolatitudes (>30°N) during the Callovian to Northern Tethyan paleolatitudes (22° to 29°N) during the Kimmeridgian and Tithonian and to Central Tethyan paleolatitudes ( Jurassic and Early Cretaceous successions in western Cuba (Sierra del Rosario and Sierra de los Organos, Pinar del Rio Province) show lithostratigraphic, paleobathymetric, and paleolatitudinal signatures which are nearly identical to those of San Pedro del Gallo terrane remnants in central Mexico. They clearly represent portions of the North American Plate and are treated as remnants of the San Pedro del Gallo terrane herein. The Cuban remnants of the San Pedro del Gallo terrane were carried to eastern Yucatan by the Walper Megashear. By the Middle Cretaceous terrane amalgamation had occurred between the San Pedro del Gallo and Coahuiltecana terranes and all movement along the Walper Megashear had ceased. Subsequent southwest to northeast movement of the Caribbean Plate during the Late Cretaceous and Early Tertiary bulldozed the Cuban remnants of the San Pedro del Gallo terrane into their present position. Once the Cuban San Pedro del Gallo remnants were carried northward by the advancing Caribbean Plate, it is likely that they became part of an Atlantic-type margin." @default.
• W1566140969 created "2016-06-24" @default.
• W1566140969 creator A5005933224 @default.
• W1566140969 creator A5008291129 @default.
• W1566140969 creator A5008862294 @default.
• W1566140969 creator A5031804795 @default.
• W1566140969 creator A5034739565 @default.
• W1566140969 creator A5035399221 @default.
• W1566140969 creator A5044995585 @default.
• W1566140969 creator A5065116343 @default.
• W1566140969 creator A5075376886 @default.
• W1566140969 creator A5078925074 @default.
• W1566140969 date "1999-01-01" @default.
• W1566140969 modified "2023-10-14" @default.
• W1566140969 title "Chapter 5 Stratigraphic evidence for northwest to southeast tectonic transport of jurassic terranes in central Mexico and the caribbean (western Cuba)" @default.
• W1566140969 cites W1963710445 @default.
• W1566140969 cites W1964408423 @default.
• W1566140969 cites W1971249318 @default.
• W1566140969 cites W1971308886 @default.
• W1566140969 cites W1985832034 @default.
• W1566140969 cites W1993014054 @default.
• W1566140969 cites W2035131635 @default.
• W1566140969 cites W2036810711 @default.
• W1566140969 cites W2037657507 @default.
• W1566140969 cites W2049620395 @default.
• W1566140969 cites W2053439268 @default.
• W1566140969 cites W2062024970 @default.
• W1566140969 cites W2064995699 @default.
• W1566140969 cites W2094938772 @default.
• W1566140969 cites W2106162082 @default.
• W1566140969 cites W2127485798 @default.
• W1566140969 cites W2129192242 @default.
• W1566140969 cites W2147888187 @default.
• W1566140969 cites W2154362075 @default.
• W1566140969 cites W2170280089 @default.
• W1566140969 cites W2314882648 @default.
• W1566140969 cites W2320263682 @default.
• W1566140969 cites W2323565804 @default.
• W1566140969 cites W2326850436 @default.
• W1566140969 cites W2327398901 @default.
• W1566140969 cites W2478716650 @default.
• W1566140969 cites W4297677661 @default.
• W1566140969 doi "https://doi.org/10.1016/s1874-5997(99)80039-2" @default.
• W1566140969 hasPublicationYear "1999" @default.
• W1566140969 type Work @default.
• W1566140969 sameAs 1566140969 @default.
• W1566140969 citedByCount "12" @default.
• W1566140969 countsByYear W15661409692014 @default.
• W1566140969 countsByYear W15661409692015 @default.
• W1566140969 countsByYear W15661409692021 @default.
• W1566140969 crossrefType "book-chapter" @default.
• W1566140969 hasAuthorship W1566140969A5005933224 @default.
• W1566140969 hasAuthorship W1566140969A5008291129 @default.
• W1566140969 hasAuthorship W1566140969A5008862294 @default.
• W1566140969 hasAuthorship W1566140969A5031804795 @default.
• W1566140969 hasAuthorship W1566140969A5034739565 @default.
• W1566140969 hasAuthorship W1566140969A5035399221 @default.
• W1566140969 hasAuthorship W1566140969A5044995585 @default.
• W1566140969 hasAuthorship W1566140969A5065116343 @default.
• W1566140969 hasAuthorship W1566140969A5075376886 @default.
• W1566140969 hasAuthorship W1566140969A5078925074 @default.
• W1566140969 hasConcept C127313418 @default.
• W1566140969 hasConcept C150999391 @default.
• W1566140969 hasConcept C151730666 @default.
• W1566140969 hasConcept C165205528 @default.
• W1566140969 hasConcept C77928131 @default.
• W1566140969 hasConceptScore W1566140969C127313418 @default.
• W1566140969 hasConceptScore W1566140969C150999391 @default.
• W1566140969 hasConceptScore W1566140969C151730666 @default.
• W1566140969 hasConceptScore W1566140969C165205528 @default.
• W1566140969 hasConceptScore W1566140969C77928131 @default.
• W1566140969 hasLocation W15661409691 @default.
• W1566140969 hasOpenAccess W1566140969 @default.
• W1566140969 hasPrimaryLocation W15661409691 @default.
• W1566140969 hasRelatedWork W2007066315 @default.
• W1566140969 hasRelatedWork W2009183070 @default.
• W1566140969 hasRelatedWork W2055663875 @default.
• W1566140969 hasRelatedWork W2056563437 @default.
• W1566140969 hasRelatedWork W2057268528 @default.
• W1566140969 hasRelatedWork W2067002397 @default.
• W1566140969 hasRelatedWork W2373125536 @default.
• W1566140969 hasRelatedWork W2378578933 @default.
• W1566140969 hasRelatedWork W2706115034 @default.
• W1566140969 hasRelatedWork W4309582884 @default.
• W1566140969 isParatext "false" @default.
• W1566140969 isRetracted "false" @default.
• W1566140969 magId "1566140969" @default.
• W1566140969 workType "book-chapter" @default.