FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1549511304> ?p ?o ?g. }

• W1549511304 abstract "Abstract The Maastrichtian age Brown Mountain Sandstone Member of the Panoche Formation is exposed in the southeastern Diablo Range along the west side of the San Joaquin Valley, California. The Brown Mountain Sandstone is one of many locally named, discontinuous sandstones that are stratigraphically near the top of the Mesozoic Great Valley Group, which crops out nearly continuously along the western edge of the San Joaquin and Sacramento Valleys. Sandstones with correlative foraminiferal assemblages and depositional facies include the gas-bearing upper Tracy submarine fan sandstones of the Sacramento Valley. Outcrop studies, regional stratigraphic correlation, subsurface mapping, and the vertical stratigraphic succession indicate that the Brown Mountain Sandstone was deposited in sand-rich submarine fan systems with source areas to the east and northeast. Subsurface isopach maps from well data depict fan-like geometries, and paleocurrent orientations from outcrop are predominantly toward the southwest. Paleontological data, including foraminifera species Bolivina incrassata and Gyroidina quadrata, were used for age control and to infer water depths of 600–1,500 feet. Arkose to lithic arkose sandstone compositions derived from petrographic analysis indicate an immature, granitic, Sierran provenance. Two distinctive lithofacies are present areally within the Brown Mountain Sandstone outcrops and are distinguished by abundance of shale interbeds, composition, grain size, and sequences of sedimentary structures. The Anticline Ridge lithofacies typically contains extensively amalgamated sandstone beds, has abundant ripple and parallel laminated structures, and is a very fine-grained, well-sorted, arkosic sandstone. The Cantua Creek lithofacies typically has less extensively amalgamated sandstones, contains shale interbeds, is locally graded including complete Bouma sequences, and is a very fine- to coarse-grained, poorly sorted, arkosic sandstone. The differences between the sedimentological characteristics of the Anticline Ridge and Cantua Creek lithofacies are related to grain size variations within the submarine fan systems. What actually controls the differences in grain size is speculative, but is probably related to the type of feeder system and/or coeval shelfal depositional systems. One model suggests that sand deposition occurred in at least two types of submarine fan systems that include: slope-fed fan systems with sediment supplied through ephemeral slope feeder channels (Anticline Ridge lithofacies); and canyon-fed fan systems with sediment supplied through established submarine gorges (Cantua Creek lithofacies). These Brown Mountain Sandstone submarine fan systems are interpreted as part of a southwesterly prograding Maastrichtian slope system within the late Cretaceous forearc basin." @default.
• W1549511304 created "2016-06-24" @default.
• W1549511304 creator A5085013075 @default.
• W1549511304 date "1990-01-01" @default.
• W1549511304 modified "2023-09-24" @default.
• W1549511304 title "Stratigraphy and Depositional Environments of the Upper Cretaceous Brown Mountain Sandstone Member of the Panoche Formation Near Coalinga, California" @default.
• W1549511304 doi "https://doi.org/10.32375/1990-gb65.23" @default.
• W1549511304 hasPublicationYear "1990" @default.
• W1549511304 type Work @default.
• W1549511304 sameAs 1549511304 @default.
• W1549511304 citedByCount "0" @default.
• W1549511304 crossrefType "book-chapter" @default.
• W1549511304 hasAuthorship W1549511304A5085013075 @default.
• W1549511304 hasConcept C109007969 @default.
• W1549511304 hasConcept C114793014 @default.
• W1549511304 hasConcept C12294951 @default.
• W1549511304 hasConcept C126753816 @default.
• W1549511304 hasConcept C127313418 @default.
• W1549511304 hasConcept C138170599 @default.
• W1549511304 hasConcept C138841024 @default.
• W1549511304 hasConcept C146588470 @default.
• W1549511304 hasConcept C151730666 @default.
• W1549511304 hasConcept C169212394 @default.
• W1549511304 hasConcept C193298577 @default.
• W1549511304 hasConcept C2780049196 @default.
• W1549511304 hasConcept C32277403 @default.
• W1549511304 hasConcept C59235061 @default.
• W1549511304 hasConcept C6494504 @default.
• W1549511304 hasConceptScore W1549511304C109007969 @default.
• W1549511304 hasConceptScore W1549511304C114793014 @default.
• W1549511304 hasConceptScore W1549511304C12294951 @default.
• W1549511304 hasConceptScore W1549511304C126753816 @default.
• W1549511304 hasConceptScore W1549511304C127313418 @default.
• W1549511304 hasConceptScore W1549511304C138170599 @default.
• W1549511304 hasConceptScore W1549511304C138841024 @default.
• W1549511304 hasConceptScore W1549511304C146588470 @default.
• W1549511304 hasConceptScore W1549511304C151730666 @default.
• W1549511304 hasConceptScore W1549511304C169212394 @default.
• W1549511304 hasConceptScore W1549511304C193298577 @default.
• W1549511304 hasConceptScore W1549511304C2780049196 @default.
• W1549511304 hasConceptScore W1549511304C32277403 @default.
• W1549511304 hasConceptScore W1549511304C59235061 @default.
• W1549511304 hasConceptScore W1549511304C6494504 @default.
• W1549511304 hasLocation W15495113041 @default.
• W1549511304 hasOpenAccess W1549511304 @default.
• W1549511304 hasPrimaryLocation W15495113041 @default.
• W1549511304 hasRelatedWork W1499563485 @default.
• W1549511304 hasRelatedWork W1604073772 @default.
• W1549511304 hasRelatedWork W1912846795 @default.
• W1549511304 hasRelatedWork W1980369820 @default.
• W1549511304 hasRelatedWork W2037963200 @default.
• W1549511304 hasRelatedWork W2050044567 @default.
• W1549511304 hasRelatedWork W2058039437 @default.
• W1549511304 hasRelatedWork W2063419028 @default.
• W1549511304 hasRelatedWork W2071422437 @default.
• W1549511304 hasRelatedWork W208497852 @default.
• W1549511304 hasRelatedWork W2095511055 @default.
• W1549511304 hasRelatedWork W2109657380 @default.
• W1549511304 hasRelatedWork W2184772172 @default.
• W1549511304 hasRelatedWork W2232511904 @default.
• W1549511304 hasRelatedWork W2241748427 @default.
• W1549511304 hasRelatedWork W2260654912 @default.
• W1549511304 hasRelatedWork W2263930744 @default.
• W1549511304 hasRelatedWork W2282690817 @default.
• W1549511304 hasRelatedWork W2293230269 @default.
• W1549511304 hasRelatedWork W2979226734 @default.
• W1549511304 isParatext "false" @default.
• W1549511304 isRetracted "false" @default.
• W1549511304 magId "1549511304" @default.
• W1549511304 workType "book-chapter" @default.