FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3209456810> ?p ?o ?g. }

• W3209456810 endingPage "622" @default.
• W3209456810 startingPage "587" @default.
• W3209456810 abstract "AbstractStudy of Cretaceous (Barremian-Turonian) sediments within the Ariyalur-Pondicherry sub-basin, Cauvery Basin, India mirrors the deposition of fluvial-to-marine transition in a syn-rift setting during the Mesozoic breakup of east Gondwanaland. Within the investigated interval, fluvial Basal Siliciclastic Formation (Upper Gondwana equivalent), overlying the Archean Basement, is succeeded by the marine Dalmiapuram Formation (shallow water) and the Karai Shale Formation (offshore). However, both the marine formations demonstrate the lithocontact with the basement locally. Process-based sedimentary facies analysis identifies nine facies associations categorized in non-marine, shallow marine and deep marine super associations, cumulatively comprising forty sedimentary facies. Facies associations vary in its lithology, primary sedimentary structures, stratal geometry and pattern, paleocurrent direction, as well as in grain size and sorting. The present study reveals the depositional processes ensued across the environmental continuum of mountain front to the ocean. Basal Siliciclastic sediments are restricted in isolated outcrops, along the western margin of the basin. Within this formation, scree-alluvial fan and channel amalgamation are restricted at basin-margin while flood-plain governs in basin-interior. The depositional contextual shifted from continental to marine during Albian on the advent of marine transgression along the eastern passive margin of India. A carbonate (non-rimmed) ramp platform, evolving from homoclinal to distally steepened, shaped the pre-fall shelf by depositing carbonates (Dalmiapuram Formation) while, organic-rich glauconite, phosphate nodule bearing shale (Karai Shale Formation) settled in the basin center. The fluvial-to-marine transition surface records a sequence boundary with the overlying formations reflecting relative sea level change. Limestone to shale conversion is gradational in accord with the pronounced retrogradational trend. However, the basal part of the Dalmiapuram Formation displays a shallowing upward trend (aggradational or progradational). The maximum flooding condition is achieved during the Karai Shale sedimentation at the crowning of transgression.KeywordsContinental-to-marine transitionFaciesSequence stratigraphyRift basin Cretaceous Cauvery basin" @default.
• W3209456810 created "2021-11-08" @default.
• W3209456810 creator A5008577423 @default.
• W3209456810 creator A5023322938 @default.
• W3209456810 creator A5076944145 @default.
• W3209456810 date "2021-01-01" @default.
• W3209456810 modified "2023-09-27" @default.
• W3209456810 title "Continental-to-Marine Transition in an Ongoing Rift Setting: Barremian-Turonian Sediments of Cauvery Basin, India" @default.
• W3209456810 cites W1926099404 @default.
• W3209456810 cites W1963191475 @default.
• W3209456810 cites W1967976058 @default.
• W3209456810 cites W1972923278 @default.
• W3209456810 cites W1977530707 @default.
• W3209456810 cites W1984636731 @default.
• W3209456810 cites W1990594389 @default.
• W3209456810 cites W1996046999 @default.
• W3209456810 cites W1997252211 @default.
• W3209456810 cites W2004013023 @default.
• W3209456810 cites W2015318619 @default.
• W3209456810 cites W2015576107 @default.
• W3209456810 cites W2023263541 @default.
• W3209456810 cites W2024176565 @default.
• W3209456810 cites W2029742074 @default.
• W3209456810 cites W2032595816 @default.
• W3209456810 cites W2035677048 @default.
• W3209456810 cites W2041428625 @default.
• W3209456810 cites W2041752263 @default.
• W3209456810 cites W2043834298 @default.
• W3209456810 cites W2055118053 @default.
• W3209456810 cites W2055194575 @default.
• W3209456810 cites W2056730103 @default.
• W3209456810 cites W2069965073 @default.
• W3209456810 cites W2071394548 @default.
• W3209456810 cites W2088800839 @default.
• W3209456810 cites W2090145791 @default.
• W3209456810 cites W2109172037 @default.
• W3209456810 cites W2132001587 @default.
• W3209456810 cites W2136936714 @default.
• W3209456810 cites W2138960929 @default.
• W3209456810 cites W2143958474 @default.
• W3209456810 cites W2153462470 @default.
• W3209456810 cites W2158299643 @default.
• W3209456810 cites W2158754147 @default.
• W3209456810 cites W2180344755 @default.
• W3209456810 cites W2200214261 @default.
• W3209456810 cites W2212746637 @default.
• W3209456810 cites W2476623835 @default.
• W3209456810 cites W2503699615 @default.
• W3209456810 cites W2530999953 @default.
• W3209456810 cites W2547985954 @default.
• W3209456810 cites W2607349495 @default.
• W3209456810 cites W2783041431 @default.
• W3209456810 cites W2788172491 @default.
• W3209456810 cites W2790203849 @default.
• W3209456810 cites W2791706190 @default.
• W3209456810 cites W2792827805 @default.
• W3209456810 cites W282079439 @default.
• W3209456810 cites W2901772945 @default.
• W3209456810 cites W2939583391 @default.
• W3209456810 cites W3042944820 @default.
• W3209456810 cites W338939215 @default.
• W3209456810 cites W4246157246 @default.
• W3209456810 doi "https://doi.org/10.1007/978-3-030-71370-6_20" @default.
• W3209456810 hasPublicationYear "2021" @default.
• W3209456810 type Work @default.
• W3209456810 sameAs 3209456810 @default.
• W3209456810 citedByCount "1" @default.
• W3209456810 countsByYear W32094568102023 @default.
• W3209456810 crossrefType "book-chapter" @default.
• W3209456810 hasAuthorship W3209456810A5008577423 @default.
• W3209456810 hasAuthorship W3209456810A5023322938 @default.
• W3209456810 hasAuthorship W3209456810A5076944145 @default.
• W3209456810 hasConcept C109007969 @default.
• W3209456810 hasConcept C112959462 @default.
• W3209456810 hasConcept C126753816 @default.
• W3209456810 hasConcept C127313418 @default.
• W3209456810 hasConcept C127413603 @default.
• W3209456810 hasConcept C138841024 @default.
• W3209456810 hasConcept C146588470 @default.
• W3209456810 hasConcept C147176958 @default.
• W3209456810 hasConcept C151730666 @default.
• W3209456810 hasConcept C16565575 @default.
• W3209456810 hasConcept C2781297371 @default.
• W3209456810 hasConcept C6494504 @default.
• W3209456810 hasConcept C77271252 @default.
• W3209456810 hasConcept C93257316 @default.
• W3209456810 hasConceptScore W3209456810C109007969 @default.
• W3209456810 hasConceptScore W3209456810C112959462 @default.
• W3209456810 hasConceptScore W3209456810C126753816 @default.
• W3209456810 hasConceptScore W3209456810C127313418 @default.
• W3209456810 hasConceptScore W3209456810C127413603 @default.
• W3209456810 hasConceptScore W3209456810C138841024 @default.
• W3209456810 hasConceptScore W3209456810C146588470 @default.
• W3209456810 hasConceptScore W3209456810C147176958 @default.
• W3209456810 hasConceptScore W3209456810C151730666 @default.
• W3209456810 hasConceptScore W3209456810C16565575 @default.
• W3209456810 hasConceptScore W3209456810C2781297371 @default.
• W3209456810 hasConceptScore W3209456810C6494504 @default.

• next