Matches in SemOpenAlex for { <https://semopenalex.org/work/W4321453177> ?p ?o ?g. }
- W4321453177 endingPage "19" @default.
- W4321453177 startingPage "1" @default.
- W4321453177 abstract "Late Quaternary landform evolution of the Karnajhora fan and its adjacent areas of the mid northern Bengal Basin, Bangladesh have been studied using remote sensing and pedogenic approach. Based on pedogenic characteristics, different soil-geomorphic units can be arranged according to their maturity as Hill > Distal Fan > Mid Fan > Proximal Fan. Soil-geomorphic units are further grouped into a three member soil-chronoassociation and approximated inferred ages are QGSK1 < 1 ka; QGSK2 < 3–4 ka; and QGSK3 > 27 ka. The weakly developed youngest member QGSK1 and the moderately developed member QGSK2 represents inceptisols at fersiallitisation weathering stage. While the oldest QGSK3 member represents alfisols and show relict nature and at the initial phase of ferrugination weathering stage. Neotectonics controls the configuration of the local catena. Paleoclimate and base-level fluctuations have also played significant roles in the development of soils and landforms of the study area. The parent materials of Member QGSK3 were deposited during 80–27 ka. Since the beginning of deposition of QGSK3 soils till the Last Glacial Maximum (LGM~18 ka), the climatic conditions gradually changed from warmer-moist to cooler-drier, and the area might experienced dominantly channel incision with minor aggradation. During this period, the land between the Jamalpur Terrace and Susang Hills might be eroded and washed away while the Sherpur Terrace survived as a remnant terrace. After the LGM, the climate changed from a cooler-dry condition to warmer-moist condition and the present Holocene floodplain started to develop. The parent materials of QGSK2 and QGSK1 members then started to deposit by the paleo-Karnajhora synchronously with the old Brahmaputra River. As the Karnajhora River presently shifted toward east, soils of QGSK2 member are not presently affected and are relatively better developed compared to QGSK1 member soils." @default.
- W4321453177 created "2023-02-22" @default.
- W4321453177 creator A5010986175 @default.
- W4321453177 creator A5026120892 @default.
- W4321453177 creator A5031133582 @default.
- W4321453177 creator A5060170807 @default.
- W4321453177 creator A5065767914 @default.
- W4321453177 creator A5088826085 @default.
- W4321453177 date "2023-02-21" @default.
- W4321453177 modified "2023-10-16" @default.
- W4321453177 title "Tectono-geomorphic evolution of an alluvial fan along the Dauki fault system, Bengal Basin, Bangladesh: remote sensing and pedogenic approach" @default.
- W4321453177 cites W1574193246 @default.
- W4321453177 cites W1665325899 @default.
- W4321453177 cites W180959961 @default.
- W4321453177 cites W1965335989 @default.
- W4321453177 cites W1968927056 @default.
- W4321453177 cites W1972768340 @default.
- W4321453177 cites W1975247044 @default.
- W4321453177 cites W1998939058 @default.
- W4321453177 cites W2011148182 @default.
- W4321453177 cites W2013878333 @default.
- W4321453177 cites W2022662209 @default.
- W4321453177 cites W2028677980 @default.
- W4321453177 cites W2028775319 @default.
- W4321453177 cites W2031516099 @default.
- W4321453177 cites W2049181841 @default.
- W4321453177 cites W2056282210 @default.
- W4321453177 cites W2056353824 @default.
- W4321453177 cites W2058250123 @default.
- W4321453177 cites W2076665156 @default.
- W4321453177 cites W2076872207 @default.
- W4321453177 cites W2080386298 @default.
- W4321453177 cites W2090640222 @default.
- W4321453177 cites W2090699423 @default.
- W4321453177 cites W2145591683 @default.
- W4321453177 cites W2166930832 @default.
- W4321453177 cites W2324132207 @default.
- W4321453177 cites W2536415503 @default.
- W4321453177 cites W2586325664 @default.
- W4321453177 cites W2746232140 @default.
- W4321453177 cites W2788422104 @default.
- W4321453177 cites W2898622743 @default.
- W4321453177 cites W2902479882 @default.
- W4321453177 cites W3003447948 @default.
- W4321453177 cites W3034867790 @default.
- W4321453177 cites W3037895019 @default.
- W4321453177 cites W3170252887 @default.
- W4321453177 cites W4224024170 @default.
- W4321453177 doi "https://doi.org/10.1080/24749508.2023.2178131" @default.
- W4321453177 hasPublicationYear "2023" @default.
- W4321453177 type Work @default.
- W4321453177 citedByCount "0" @default.
- W4321453177 crossrefType "journal-article" @default.
- W4321453177 hasAuthorship W4321453177A5010986175 @default.
- W4321453177 hasAuthorship W4321453177A5026120892 @default.
- W4321453177 hasAuthorship W4321453177A5031133582 @default.
- W4321453177 hasAuthorship W4321453177A5060170807 @default.
- W4321453177 hasAuthorship W4321453177A5065767914 @default.
- W4321453177 hasAuthorship W4321453177A5088826085 @default.
- W4321453177 hasBestOaLocation W43214531771 @default.
- W4321453177 hasConcept C100970517 @default.
- W4321453177 hasConcept C108497213 @default.
- W4321453177 hasConcept C109007969 @default.
- W4321453177 hasConcept C112959462 @default.
- W4321453177 hasConcept C114793014 @default.
- W4321453177 hasConcept C127313418 @default.
- W4321453177 hasConcept C140345934 @default.
- W4321453177 hasConcept C142614818 @default.
- W4321453177 hasConcept C151730666 @default.
- W4321453177 hasConcept C159390177 @default.
- W4321453177 hasConcept C159750122 @default.
- W4321453177 hasConcept C160464908 @default.
- W4321453177 hasConcept C166957645 @default.
- W4321453177 hasConcept C17409809 @default.
- W4321453177 hasConcept C184269829 @default.
- W4321453177 hasConcept C185515318 @default.
- W4321453177 hasConcept C205649164 @default.
- W4321453177 hasConcept C206137718 @default.
- W4321453177 hasConcept C2776638177 @default.
- W4321453177 hasConcept C32552466 @default.
- W4321453177 hasConcept C40724407 @default.
- W4321453177 hasConcept C69823785 @default.
- W4321453177 hasConcept C76123530 @default.
- W4321453177 hasConceptScore W4321453177C100970517 @default.
- W4321453177 hasConceptScore W4321453177C108497213 @default.
- W4321453177 hasConceptScore W4321453177C109007969 @default.
- W4321453177 hasConceptScore W4321453177C112959462 @default.
- W4321453177 hasConceptScore W4321453177C114793014 @default.
- W4321453177 hasConceptScore W4321453177C127313418 @default.
- W4321453177 hasConceptScore W4321453177C140345934 @default.
- W4321453177 hasConceptScore W4321453177C142614818 @default.
- W4321453177 hasConceptScore W4321453177C151730666 @default.
- W4321453177 hasConceptScore W4321453177C159390177 @default.
- W4321453177 hasConceptScore W4321453177C159750122 @default.
- W4321453177 hasConceptScore W4321453177C160464908 @default.
- W4321453177 hasConceptScore W4321453177C166957645 @default.
- W4321453177 hasConceptScore W4321453177C17409809 @default.
- W4321453177 hasConceptScore W4321453177C184269829 @default.