Matches in SemOpenAlex for { <https://semopenalex.org/work/W1764871215> ?p ?o ?g. }
Showing items 1 to 70 of
70
with 100 items per page.
- W1764871215 endingPage "238" @default.
- W1764871215 startingPage "217" @default.
- W1764871215 abstract "Abstract Deposition in the Oquirrh Basin of northwestern Utah produced up to 7.5 km thickness of late Paleozoic limestone and sandstone. Study of Upper Pennsylvanian and Lower Permian lithofacies, trace fossils, and body fossils relative to a time framework determined by fusulinid biostratigraphy reveals a spectrum of depositional environments, which shifted through time. Shallow-water, organically productive marine environments were recorded in accumulation of a great thickness of Middle Pennsylvanian limestone and sandstone. In the Late Pennsylvanian, vast quantities of subarkosic sand and increased water depth reflect a significant change in basin morphology. A northwest-trending trough developed from the northwest part of the basin during the Late Pennsylvanian, extending the length of the basin by early to middle Wolfcampian. Water depths may have reached 300-400 m (1000-1300 ft), and stagnant water in the northwest part of the basin ultimately became poorly oxygenated. Shallower water siltstones capped the sequence in the late Wolfcampian to Leonardian. Coarse conglomerates, commonly composed of older clasts from the Oquirrh Group, are common in the uppermost Pennsylvanian and lower Wolfcampian deep-water deposits. They record rapid lithification, uplift, and erosion of the margins of the trough, and imply that the Oquirrh Basin was bounded by active northwest-trending high-angle faults at this time. These faults were apparently initiated in the Late Pennsylvanian and became inactive by the late Wolfcampian. Sedimentary rocks near the upper limits of the Oquirrh Group record passive filling of the remnant graben-like trough. The evolution of the Oquirrh Basin is similar to that of basement uplifts and yoked basins throughout the region to the south and east. The basin’s northwest trend, high-angle fault margins, and rapid structural development in the latest Pennsylvanian and early Wolfcampian demonstrate a tectonic association with the regional deformation which formed the Ancestral Rocky Mountains." @default.
- W1764871215 created "2016-06-24" @default.
- W1764871215 creator A5026265136 @default.
- W1764871215 creator A5051151570 @default.
- W1764871215 date "1980-01-01" @default.
- W1764871215 modified "2023-09-23" @default.
- W1764871215 title "Paleogeography and Structural Development of the Late Pennsylvanian to Early Permian Oquirrh Basin, Northwestern Utah" @default.
- W1764871215 hasPublicationYear "1980" @default.
- W1764871215 type Work @default.
- W1764871215 sameAs 1764871215 @default.
- W1764871215 citedByCount "7" @default.
- W1764871215 countsByYear W17648712152018 @default.
- W1764871215 crossrefType "journal-article" @default.
- W1764871215 hasAuthorship W1764871215A5026265136 @default.
- W1764871215 hasAuthorship W1764871215A5051151570 @default.
- W1764871215 hasConcept C106804226 @default.
- W1764871215 hasConcept C109007969 @default.
- W1764871215 hasConcept C126753816 @default.
- W1764871215 hasConcept C127313418 @default.
- W1764871215 hasConcept C13106087 @default.
- W1764871215 hasConcept C138170599 @default.
- W1764871215 hasConcept C139719470 @default.
- W1764871215 hasConcept C151730666 @default.
- W1764871215 hasConcept C162324750 @default.
- W1764871215 hasConcept C2779650180 @default.
- W1764871215 hasConcept C32239851 @default.
- W1764871215 hasConcept C6494504 @default.
- W1764871215 hasConcept C83365034 @default.
- W1764871215 hasConceptScore W1764871215C106804226 @default.
- W1764871215 hasConceptScore W1764871215C109007969 @default.
- W1764871215 hasConceptScore W1764871215C126753816 @default.
- W1764871215 hasConceptScore W1764871215C127313418 @default.
- W1764871215 hasConceptScore W1764871215C13106087 @default.
- W1764871215 hasConceptScore W1764871215C138170599 @default.
- W1764871215 hasConceptScore W1764871215C139719470 @default.
- W1764871215 hasConceptScore W1764871215C151730666 @default.
- W1764871215 hasConceptScore W1764871215C162324750 @default.
- W1764871215 hasConceptScore W1764871215C2779650180 @default.
- W1764871215 hasConceptScore W1764871215C32239851 @default.
- W1764871215 hasConceptScore W1764871215C6494504 @default.
- W1764871215 hasConceptScore W1764871215C83365034 @default.
- W1764871215 hasLocation W17648712151 @default.
- W1764871215 hasOpenAccess W1764871215 @default.
- W1764871215 hasPrimaryLocation W17648712151 @default.
- W1764871215 hasRelatedWork W124507661 @default.
- W1764871215 hasRelatedWork W1496180975 @default.
- W1764871215 hasRelatedWork W1507611069 @default.
- W1764871215 hasRelatedWork W1564303008 @default.
- W1764871215 hasRelatedWork W1868110995 @default.
- W1764871215 hasRelatedWork W1995428043 @default.
- W1764871215 hasRelatedWork W2012406415 @default.
- W1764871215 hasRelatedWork W2021318188 @default.
- W1764871215 hasRelatedWork W2038527458 @default.
- W1764871215 hasRelatedWork W2054563590 @default.
- W1764871215 hasRelatedWork W2091261714 @default.
- W1764871215 hasRelatedWork W2094196683 @default.
- W1764871215 hasRelatedWork W2095996144 @default.
- W1764871215 hasRelatedWork W2145034466 @default.
- W1764871215 hasRelatedWork W2154208178 @default.
- W1764871215 hasRelatedWork W2170479132 @default.
- W1764871215 hasRelatedWork W2185510027 @default.
- W1764871215 hasRelatedWork W2903731627 @default.
- W1764871215 hasRelatedWork W3124574880 @default.
- W1764871215 hasRelatedWork W2092397573 @default.
- W1764871215 isParatext "false" @default.
- W1764871215 isRetracted "false" @default.
- W1764871215 magId "1764871215" @default.
- W1764871215 workType "article" @default.