FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2917774420> ?p ?o ?g. }

• W2917774420 endingPage "362" @default.
• W2917774420 startingPage "335" @default.
• W2917774420 abstract "The Albian–lower Cenomanian Comanchean Series on the Comanche Shelf, Texas and northern Mexico is a laboratory to calibrate the numerical ages of mixed carbonate-siliciclastic cycles. The stratigraphic contacts of the long-term cycles formed during subaerial exposure followed by marine drowning. Correlation of these cycle contacts in different basins tests their synchroneity and the hypothesis of eustasy. Petrographic and geochemical evidence of Early Cretaceous meteoric diagenesis differs across the shelf because the Comanche Shelf spanned the subtropical arid belt and the mid-latitude warm humid zone. The contact between the Fredericksburg and Washita groups is Al SB Wa1, which is a composite subaerial unconformity and transgressive drowning surface that is traced from southeastern Oklahoma to El Paso and down-dip to the shelf margin. Chronostratigraphy of the Comanchean Series Fredericksburg and Washita groups is constrained by multiple biostratigraphic data of ammonites, caprinid rudists, and foraminifers. The lower upper Albian Al SB Wa1 is dated by the Dipoloceras cristatum Zone below and the Mortoniceras pricei Zone above. Caprinid zones in carbonate facies are integrated with ammonites and foraminifers to provide a complementary correlation criterion. This contact is coeval with a condensed interval in Europe and flooding sequences in western Asia and northern Africa. Depleted carbon isotope ratios indicate subaerial exposure below sequence boundaries at base of Washita Group, at base of the lower Cenomanian Del Rio Formation and base of the Cenomanian Woodbine-Eagle Ford groups. These contacts are coeval with sequences in Europe, Africa, Asia, and South America. Late Albian–early Cenomanian sea-level changes provide a chronologic scale for significant oceanic plate reorganization dated at about 100 Ma." @default.
• W2917774420 created "2019-03-02" @default.
• W2917774420 creator A5011329194 @default.
• W2917774420 creator A5019601878 @default.
• W2917774420 creator A5028900650 @default.
• W2917774420 creator A5034624196 @default.
• W2917774420 creator A5039507114 @default.
• W2917774420 creator A5044171145 @default.
• W2917774420 creator A5047023224 @default.
• W2917774420 creator A5048850343 @default.
• W2917774420 creator A5064526204 @default.
• W2917774420 creator A5071290665 @default.
• W2917774420 creator A5073628866 @default.
• W2917774420 creator A5083381282 @default.
• W2917774420 date "2019-06-01" @default.
• W2917774420 modified "2023-10-15" @default.
• W2917774420 title "Regional upper Albian–lower Cenomanian sequence boundaries, Texas Comanche shelf: Is timing related to oceanic tectonics?" @default.
• W2917774420 cites W1942528694 @default.
• W2917774420 cites W1967108155 @default.
• W2917774420 cites W1971938134 @default.
• W2917774420 cites W1979381341 @default.
• W2917774420 cites W1984985823 @default.
• W2917774420 cites W1986335132 @default.
• W2917774420 cites W1986657975 @default.
• W2917774420 cites W1991884817 @default.
• W2917774420 cites W1994469950 @default.
• W2917774420 cites W1997252211 @default.
• W2917774420 cites W2000169668 @default.
• W2917774420 cites W2000252225 @default.
• W2917774420 cites W2013278698 @default.
• W2917774420 cites W2014072913 @default.
• W2917774420 cites W2021267266 @default.
• W2917774420 cites W2033460630 @default.
• W2917774420 cites W2036698119 @default.
• W2917774420 cites W2040404162 @default.
• W2917774420 cites W2041269880 @default.
• W2917774420 cites W2045076192 @default.
• W2917774420 cites W2045622541 @default.
• W2917774420 cites W2061342595 @default.
• W2917774420 cites W2061680126 @default.
• W2917774420 cites W2061999061 @default.
• W2917774420 cites W2066113217 @default.
• W2917774420 cites W2067971827 @default.
• W2917774420 cites W2069985759 @default.
• W2917774420 cites W2071924487 @default.
• W2917774420 cites W2088182320 @default.
• W2917774420 cites W2089962601 @default.
• W2917774420 cites W2092159112 @default.
• W2917774420 cites W2093615995 @default.
• W2917774420 cites W2093879665 @default.
• W2917774420 cites W2094144922 @default.
• W2917774420 cites W2101432322 @default.
• W2917774420 cites W2109095792 @default.
• W2917774420 cites W2109482546 @default.
• W2917774420 cites W2112459206 @default.
• W2917774420 cites W2126571524 @default.
• W2917774420 cites W2153985161 @default.
• W2917774420 cites W2155279703 @default.
• W2917774420 cites W2162605305 @default.
• W2917774420 cites W2165007742 @default.
• W2917774420 cites W2171093075 @default.
• W2917774420 cites W2494170617 @default.
• W2917774420 cites W2494927002 @default.
• W2917774420 cites W2547646793 @default.
• W2917774420 cites W2740520330 @default.
• W2917774420 cites W2795005270 @default.
• W2917774420 cites W296898659 @default.
• W2917774420 cites W4211104294 @default.
• W2917774420 cites W4248512079 @default.
• W2917774420 cites W4380435203 @default.
• W2917774420 doi "https://doi.org/10.1016/j.cretres.2019.02.007" @default.
• W2917774420 hasPublicationYear "2019" @default.
• W2917774420 type Work @default.
• W2917774420 sameAs 2917774420 @default.
• W2917774420 citedByCount "3" @default.
• W2917774420 countsByYear W29177744202020 @default.
• W2917774420 countsByYear W29177744202021 @default.
• W2917774420 countsByYear W29177744202023 @default.
• W2917774420 crossrefType "journal-article" @default.
• W2917774420 hasAuthorship W2917774420A5011329194 @default.
• W2917774420 hasAuthorship W2917774420A5019601878 @default.
• W2917774420 hasAuthorship W2917774420A5028900650 @default.
• W2917774420 hasAuthorship W2917774420A5034624196 @default.
• W2917774420 hasAuthorship W2917774420A5039507114 @default.
• W2917774420 hasAuthorship W2917774420A5044171145 @default.
• W2917774420 hasAuthorship W2917774420A5047023224 @default.
• W2917774420 hasAuthorship W2917774420A5048850343 @default.
• W2917774420 hasAuthorship W2917774420A5064526204 @default.
• W2917774420 hasAuthorship W2917774420A5071290665 @default.
• W2917774420 hasAuthorship W2917774420A5073628866 @default.
• W2917774420 hasAuthorship W2917774420A5083381282 @default.
• W2917774420 hasConcept C109007969 @default.
• W2917774420 hasConcept C12294951 @default.
• W2917774420 hasConcept C127313418 @default.
• W2917774420 hasConcept C146588470 @default.
• W2917774420 hasConcept C151730666 @default.
• W2917774420 hasConcept C189473229 @default.
• W2917774420 hasConcept C192797867 @default.

• next