Matches in SemOpenAlex for { <https://semopenalex.org/work/W2109495746> ?p ?o ?g. }
Showing items 1 to 52 of
52
with 100 items per page.
- W2109495746 abstract "Triassic strata exposed along the flanks of the Nacimiento and Jemez uplifts (Sandoval County, northernNew Mexico) belong to the Middle Triassic Moenkopi Formation (Anton Chico Member) and the UpperTriassic Chinle Group (Agua Zarca, Salitral, Poleo, and Petrified Forest Formations). The Moenkopi Formation(strata previously assigned by most workers to the Permian Bernal Formation) is as much as 39 m thick and mostlygrayish red sandstone, siltstone, mudstone, and intraformational conglomerate. It disconformably overlies thePermian Glorieta Sandstone and is disconformably overlain by the Agua Zarca Formation. The Agua Zarca is asmuch as 61 m thick and mostly white to brown, trough-crossbedded, quartzose sandstone and siliceous conglomerate.The overlying Salitral Formation is as much as 102 m thick and mostly purplish, smectitic mudstone. ThePoleo Formation disconformably overlies the Salitral and is as much as 41 m thick and mostly grayish yellow,trough-crossbedded litharenite, subarkose and intrabasinal and siliceous conglomerate. Above the Poleo, the PetrifiedForest Formation is as much as 340 m thick and dominated by reddish brown, smectitic mudstone. South ofSan Miguel Canyon (T19, R1W), the Poleo Formation essentially pinches out, though thin (<20m), lenticularequivalents of the Poleo are locally present as far southeast as Vallecito Creek (T16N, R2E). Furthermore, throughoutSandoval County, the lower portion of the mudstone-dominated interval above theAgua Zarca Formation, evenwhere the Poleo Formation is absent, is dominated by purplish mudstone characteristic of the Salitral Formation.Therefore, to the south of San Miguel Canyon the Salitral and Poleo Formations can be recognized locally, but thethick, mudstone-dominated section above the Agua Zarca is assigned to the Petrified Forest Formation. The CorreoSandstone Bed crops out as a bench-forming sandstone up to 15 m thick at the top of the Petrified Forest Formationalong the southern flank of the Nacimiento uplift. Fossil vertebrates indicate the Petrified Forest Formation rangesin age from Adamanian to Revueltian (latest Carnian-Norian) and support lithostratigraphic correlation of theTriassic strata exposed in Sandoval County to nearby Triassic outcrops in the Chama basin, Lucero uplift, andHagan basin." @default.
- W2109495746 created "2016-06-24" @default.
- W2109495746 creator A5087097228 @default.
- W2109495746 date "1996-01-01" @default.
- W2109495746 modified "2023-10-14" @default.
- W2109495746 title "Stratigraphy and correlation of Triassic strata around the Nacimiento and Jemez uplifts, northern New Mexico" @default.
- W2109495746 cites W101642305 @default.
- W2109495746 cites W1508206411 @default.
- W2109495746 cites W1529772509 @default.
- W2109495746 cites W173712955 @default.
- W2109495746 cites W204356094 @default.
- W2109495746 cites W2210053752 @default.
- W2109495746 cites W2243390088 @default.
- W2109495746 cites W2917456392 @default.
- W2109495746 cites W3043444719 @default.
- W2109495746 cites W2741894446 @default.
- W2109495746 doi "https://doi.org/10.56577/ffc-47.199" @default.
- W2109495746 hasPublicationYear "1996" @default.
- W2109495746 type Work @default.
- W2109495746 sameAs 2109495746 @default.
- W2109495746 citedByCount "7" @default.
- W2109495746 countsByYear W21094957462014 @default.
- W2109495746 countsByYear W21094957462021 @default.
- W2109495746 crossrefType "proceedings-article" @default.
- W2109495746 hasAuthorship W2109495746A5087097228 @default.
- W2109495746 hasBestOaLocation W21094957462 @default.
- W2109495746 hasConcept C109281948 @default.
- W2109495746 hasConcept C127313418 @default.
- W2109495746 hasConcept C151730666 @default.
- W2109495746 hasConcept C77928131 @default.
- W2109495746 hasConceptScore W2109495746C109281948 @default.
- W2109495746 hasConceptScore W2109495746C127313418 @default.
- W2109495746 hasConceptScore W2109495746C151730666 @default.
- W2109495746 hasConceptScore W2109495746C77928131 @default.
- W2109495746 hasLocation W21094957461 @default.
- W2109495746 hasLocation W21094957462 @default.
- W2109495746 hasOpenAccess W2109495746 @default.
- W2109495746 hasPrimaryLocation W21094957461 @default.
- W2109495746 hasRelatedWork W1528207478 @default.
- W2109495746 hasRelatedWork W1969387894 @default.
- W2109495746 hasRelatedWork W1988826065 @default.
- W2109495746 hasRelatedWork W2080799689 @default.
- W2109495746 hasRelatedWork W2093776561 @default.
- W2109495746 hasRelatedWork W2137239952 @default.
- W2109495746 hasRelatedWork W2157439519 @default.
- W2109495746 hasRelatedWork W2328269999 @default.
- W2109495746 hasRelatedWork W2975723042 @default.
- W2109495746 hasRelatedWork W3116071315 @default.
- W2109495746 isParatext "false" @default.
- W2109495746 isRetracted "false" @default.
- W2109495746 magId "2109495746" @default.
- W2109495746 workType "article" @default.