Matches in SemOpenAlex for { <https://semopenalex.org/work/W3001692606> ?p ?o ?g. }
Showing items 1 to 100 of
100
with 100 items per page.
- W3001692606 abstract "Abstract Late Quaternary fluvial deposits along the Janauri (JA; comprises Siwalik rocks) and Bhaddi (BA; dominantly of Quaternary deposits) anticlines over independent fault segments of the Himalayan Frontal Thrust (HFT), Kangra re-entrant, were studied to deduce the timing and causes of the Beas-Satluj rivers deflections. The deposits, 4–60 m thick, were documented from the northwestern fringe of the JA (Site-1), between JA and BA (Site-2) and entire BA (Site-3), and along the present course of the Satluj River (Site-4) in the piggyback Soan Dun. They comprise quartzite-bearing gravels and multistorey sheet sand bodies with large-scale trough cross-stratification and are deposited by the Beas (Site-1) and Satluj (Sites 2-4) rivers. The deposits at Sites 1-3 are uplifted, tilted or folded, whereas, horizontally bedded at Site-4. Based on quartz Optically Stimulated Luminescence chrono-stratigraphy, the aggradation phase is bracketed between >46.4±2.9 and 37.4±2.3 ka (Site-1), >69.9±4.5 and 26.1±2.6 ka (Site-2) and >55.2±1.7 and 50.3±3.5 ka (Site-3). The terrace deposits at Site-4 were formed around 26, 11 and 6 ka. The sedimentation (9.9 to 2.7 mm yr-1 between 61.8 and 26 ka) and uplift (3.4±0.3 mm yr-1 over a period of 44 ka) rates along HFT show that the latter exceeds the aggradation rate with time. It is envisaged that time variable tectonic movements along independent fault segments of the HFT forced river deflection and termination of deposition at Sites 1-3, however, the absence of any forced aggradation at the Site-4 concomitant with Site-2 termination suggests it is also governed by climate." @default.
- W3001692606 created "2020-01-30" @default.
- W3001692606 creator A5043061659 @default.
- W3001692606 creator A5056260117 @default.
- W3001692606 date "2020-04-01" @default.
- W3001692606 modified "2023-10-18" @default.
- W3001692606 title "Late Quaternary Deflections of the Beas-Satluj rivers at the Himalayan mountain front, Kangra re-entrant, India: Response to fold growth and climate" @default.
- W3001692606 cites W1964622405 @default.
- W3001692606 cites W1969704674 @default.
- W3001692606 cites W1973936656 @default.
- W3001692606 cites W1984475559 @default.
- W3001692606 cites W1984976383 @default.
- W3001692606 cites W1988111399 @default.
- W3001692606 cites W1990519987 @default.
- W3001692606 cites W1992472420 @default.
- W3001692606 cites W1994559058 @default.
- W3001692606 cites W1996937223 @default.
- W3001692606 cites W2005592976 @default.
- W3001692606 cites W2014451275 @default.
- W3001692606 cites W2014668597 @default.
- W3001692606 cites W2036635368 @default.
- W3001692606 cites W2037430119 @default.
- W3001692606 cites W2037453581 @default.
- W3001692606 cites W2047957907 @default.
- W3001692606 cites W2051187614 @default.
- W3001692606 cites W2051315307 @default.
- W3001692606 cites W2052493774 @default.
- W3001692606 cites W2056637650 @default.
- W3001692606 cites W2060320793 @default.
- W3001692606 cites W2072897088 @default.
- W3001692606 cites W2075686130 @default.
- W3001692606 cites W2076373896 @default.
- W3001692606 cites W2078619763 @default.
- W3001692606 cites W2085896233 @default.
- W3001692606 cites W2090031266 @default.
- W3001692606 cites W2091960592 @default.
- W3001692606 cites W2094408279 @default.
- W3001692606 cites W2114541080 @default.
- W3001692606 cites W2120248779 @default.
- W3001692606 cites W2139752032 @default.
- W3001692606 cites W2284105739 @default.
- W3001692606 cites W2346379268 @default.
- W3001692606 cites W2376149826 @default.
- W3001692606 cites W2755918039 @default.
- W3001692606 cites W2810123521 @default.
- W3001692606 cites W2811137025 @default.
- W3001692606 cites W2465879020 @default.
- W3001692606 cites W2504573185 @default.
- W3001692606 doi "https://doi.org/10.1016/j.jseaes.2020.104248" @default.
- W3001692606 hasPublicationYear "2020" @default.
- W3001692606 type Work @default.
- W3001692606 sameAs 3001692606 @default.
- W3001692606 citedByCount "1" @default.
- W3001692606 countsByYear W30016926062022 @default.
- W3001692606 crossrefType "journal-article" @default.
- W3001692606 hasAuthorship W3001692606A5043061659 @default.
- W3001692606 hasAuthorship W3001692606A5056260117 @default.
- W3001692606 hasConcept C109007969 @default.
- W3001692606 hasConcept C112959462 @default.
- W3001692606 hasConcept C114793014 @default.
- W3001692606 hasConcept C116637073 @default.
- W3001692606 hasConcept C127313418 @default.
- W3001692606 hasConcept C127413603 @default.
- W3001692606 hasConcept C142614818 @default.
- W3001692606 hasConcept C151730666 @default.
- W3001692606 hasConcept C160464908 @default.
- W3001692606 hasConcept C17409809 @default.
- W3001692606 hasConcept C206137718 @default.
- W3001692606 hasConcept C53942344 @default.
- W3001692606 hasConcept C78519656 @default.
- W3001692606 hasConceptScore W3001692606C109007969 @default.
- W3001692606 hasConceptScore W3001692606C112959462 @default.
- W3001692606 hasConceptScore W3001692606C114793014 @default.
- W3001692606 hasConceptScore W3001692606C116637073 @default.
- W3001692606 hasConceptScore W3001692606C127313418 @default.
- W3001692606 hasConceptScore W3001692606C127413603 @default.
- W3001692606 hasConceptScore W3001692606C142614818 @default.
- W3001692606 hasConceptScore W3001692606C151730666 @default.
- W3001692606 hasConceptScore W3001692606C160464908 @default.
- W3001692606 hasConceptScore W3001692606C17409809 @default.
- W3001692606 hasConceptScore W3001692606C206137718 @default.
- W3001692606 hasConceptScore W3001692606C53942344 @default.
- W3001692606 hasConceptScore W3001692606C78519656 @default.
- W3001692606 hasLocation W30016926061 @default.
- W3001692606 hasOpenAccess W3001692606 @default.
- W3001692606 hasPrimaryLocation W30016926061 @default.
- W3001692606 hasRelatedWork W14337237 @default.
- W3001692606 hasRelatedWork W16254256 @default.
- W3001692606 hasRelatedWork W20371962 @default.
- W3001692606 hasRelatedWork W37785191 @default.
- W3001692606 hasRelatedWork W44085452 @default.
- W3001692606 hasRelatedWork W54728290 @default.
- W3001692606 hasRelatedWork W58239965 @default.
- W3001692606 hasRelatedWork W62626962 @default.
- W3001692606 hasRelatedWork W84024659 @default.
- W3001692606 hasRelatedWork W90991457 @default.
- W3001692606 isParatext "false" @default.
- W3001692606 isRetracted "false" @default.
- W3001692606 magId "3001692606" @default.
- W3001692606 workType "article" @default.