FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2135047613> ?p ?o ?g. }

• W2135047613 abstract "Triassic strata in the Chama Basin of Rio Arriba County, New Mexico, pertain to the Upper Triassic Chinle Group (in ascending order, the Zuni Mountains, Shinarump, Salitral, Poleo, Petrified Forest and Rock Point formations). The base of the Chinle Group locally is the Zuni Mountains Formation (formerly mottled strata), a pedogenic weathering profile as much as 7 m thick, developed in the top of the Pennsylvanian-Permian Cutler Group. Where the Zuni Mountains Formation is absent, the base of the Chinle Group is the Shinarump Formation. In the Chama Basin, the Shinarump Formation (= Agua Zarca Formation of previous usage) is as much as 13 m thick and consists mostly of trough-crossbedded, quartzose sandstone and siliceous conglomerate. The Salitral Formation is as much as 31 m of mostly greenish and reddish brown, bentonitic mudstone. The Salitral Formation is divided into two members: a lower, Piedra Lumbre Member of greenish mudstone with a peristent sandstone bed (the El Cerrito Bed) at its top, and an upper, Youngsville Member, which mostly consists of reddish-brown mud- stone. The Poleo Formation is up to 41 m thick and is mostly grayish yellow, trough-crossbedded litharenitic and subarkosic sandstone with minor amounts of both intrabasinal and siliceous conglomerate. Above the Poleo Formation, as much as 200 m of strata, dominated by reddish brown, bentonitic mudstone, constitute the Petrified Forest Formation. In the Chama Basin, the Petrified Forest Formation consists of two members, the lower Mesa Montosa Member, up to 24 m of thin-bedded sandstone, siltstone and mudstone, which is overlain by up to 176 m of the bentonitic mudstone-dominated Painted Desert Member. The Rock Point Formation in the Chama Basin disconformably overlies the Petrified Forest Formation and is as much as 70 m thick and mostly laterally persistent, repetitive beds of reddish brown and grayish red siltstone and ripple-laminar sandstone that essentially lack volcanic detritus. In the Chama Basin, unionid bivalves from the Petrified Forest Formation are consistent with a Revueltian age, and paly- nomorphs from the Painted Desert Member of the Petrified Forest Formation and from the Rock Point Formation are of Norian age. Three formations of the Chinle Group in the Chama Basin contain biochronologically important vertebrate fossils, notably the aetosaur Desmatosuchus haplocerus (Adamanian) in the Salitral Formation, the aetosaurs Typothorax coccinarum and Desmatosuchus chamaensis and the phytosaur Pseudopalatus buceros (Revueltian) in the Petrified Forest Formation, and the phytosaur Redondasaurus (Apachean) in the Rock Point Formation. These fossils and lithostratigraphy allow precise correla- tion of the Chinle Group strata exposed in north-central New Mexico with other Upper Triassic strata in New Mexico." @default.
• W2135047613 created "2016-06-24" @default.
• W2135047613 creator A5055134079 @default.
• W2135047613 creator A5080729648 @default.
• W2135047613 creator A5087097228 @default.
• W2135047613 creator A5089393068 @default.
• W2135047613 date "2005-01-01" @default.
• W2135047613 modified "2023-09-26" @default.
• W2135047613 title "Review of Upper Triassic stratigraphy and biostratigraphy in the Chama Basin, northern New Mexico" @default.
• W2135047613 cites W101642305 @default.
• W2135047613 cites W1142135155 @default.
• W2135047613 cites W1520212962 @default.
• W2135047613 cites W1521572564 @default.
• W2135047613 cites W1529772509 @default.
• W2135047613 cites W1568909421 @default.
• W2135047613 cites W1601848820 @default.
• W2135047613 cites W1837366428 @default.
• W2135047613 cites W1905588488 @default.
• W2135047613 cites W1965245037 @default.
• W2135047613 cites W1970514942 @default.
• W2135047613 cites W2003902509 @default.
• W2135047613 cites W2025999730 @default.
• W2135047613 cites W2055157801 @default.
• W2135047613 cites W2058415084 @default.
• W2135047613 cites W207080895 @default.
• W2135047613 cites W2088492438 @default.
• W2135047613 cites W2103168917 @default.
• W2135047613 cites W2109148366 @default.
• W2135047613 cites W2109430624 @default.
• W2135047613 cites W2109495746 @default.
• W2135047613 cites W2114127035 @default.
• W2135047613 cites W2117711486 @default.
• W2135047613 cites W2121114265 @default.
• W2135047613 cites W2138523818 @default.
• W2135047613 cites W2140687624 @default.
• W2135047613 cites W2153423047 @default.
• W2135047613 cites W2162691110 @default.
• W2135047613 cites W2182615466 @default.
• W2135047613 cites W2182656171 @default.
• W2135047613 cites W2185629599 @default.
• W2135047613 cites W2186123243 @default.
• W2135047613 cites W2188703311 @default.
• W2135047613 cites W2271755357 @default.
• W2135047613 cites W2276807728 @default.
• W2135047613 cites W246851402 @default.
• W2135047613 cites W2506461557 @default.
• W2135047613 cites W2509431517 @default.
• W2135047613 cites W2562946506 @default.
• W2135047613 cites W2614040025 @default.
• W2135047613 cites W2798964194 @default.
• W2135047613 cites W2917456392 @default.
• W2135047613 cites W297304068 @default.
• W2135047613 cites W2994977351 @default.
• W2135047613 cites W3043444719 @default.
• W2135047613 cites W3175991846 @default.
• W2135047613 cites W368818824 @default.
• W2135047613 cites W47323572 @default.
• W2135047613 cites W592776550 @default.
• W2135047613 cites W757459052 @default.
• W2135047613 cites W2296791292 @default.
• W2135047613 doi "https://doi.org/10.56577/ffc-56.170" @default.
• W2135047613 hasPublicationYear "2005" @default.
• W2135047613 type Work @default.
• W2135047613 sameAs 2135047613 @default.
• W2135047613 citedByCount "5" @default.
• W2135047613 countsByYear W21350476132013 @default.
• W2135047613 countsByYear W21350476132016 @default.
• W2135047613 countsByYear W21350476132021 @default.
• W2135047613 crossrefType "proceedings-article" @default.
• W2135047613 hasAuthorship W2135047613A5055134079 @default.
• W2135047613 hasAuthorship W2135047613A5080729648 @default.
• W2135047613 hasAuthorship W2135047613A5087097228 @default.
• W2135047613 hasAuthorship W2135047613A5089393068 @default.
• W2135047613 hasConcept C109007969 @default.
• W2135047613 hasConcept C109281948 @default.
• W2135047613 hasConcept C127313418 @default.
• W2135047613 hasConcept C151730666 @default.
• W2135047613 hasConcept C61721801 @default.
• W2135047613 hasConcept C77928131 @default.
• W2135047613 hasConceptScore W2135047613C109007969 @default.
• W2135047613 hasConceptScore W2135047613C109281948 @default.
• W2135047613 hasConceptScore W2135047613C127313418 @default.
• W2135047613 hasConceptScore W2135047613C151730666 @default.
• W2135047613 hasConceptScore W2135047613C61721801 @default.
• W2135047613 hasConceptScore W2135047613C77928131 @default.
• W2135047613 hasLocation W21350476131 @default.
• W2135047613 hasOpenAccess W2135047613 @default.
• W2135047613 hasPrimaryLocation W21350476131 @default.
• W2135047613 hasRelatedWork W1522402857 @default.
• W2135047613 hasRelatedWork W1964969003 @default.
• W2135047613 hasRelatedWork W2025416224 @default.
• W2135047613 hasRelatedWork W2080799689 @default.
• W2135047613 hasRelatedWork W2093776561 @default.
• W2135047613 hasRelatedWork W2370517764 @default.
• W2135047613 hasRelatedWork W2417219621 @default.
• W2135047613 hasRelatedWork W2767943074 @default.
• W2135047613 hasRelatedWork W2781702993 @default.
• W2135047613 hasRelatedWork W3195800700 @default.
• W2135047613 isParatext "false" @default.
• W2135047613 isRetracted "false" @default.

• next