Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006402605> ?p ?o ?g. }
- W2006402605 endingPage "154" @default.
- W2006402605 startingPage "135" @default.
- W2006402605 abstract "The paper describes Late Quaternary pedosedimentary sequences of the alluvial fans from the Kangra basin of NW Himalayas for tectonic and paleoclimatic implications. In the proximal part of the Kangra basin three coalescing alluvial fans, namely Rait-Rihlu fans (~ 65 km2), Kangra fans (~ 200 km2), and Palampur fans (~ 170 km2) from west to east evolved due to reactivation of longitudinal and transverse faults and climatic changes during the Late Quaternary. The fans are characterised by subsidence of Rait-Rihlu fans, uplift of Kangra fans and tilting of Palampur fans. The thick (~ 90 m) pedosedimentary sequences exposed along the rivers characterise the dominant formative processes over the fans. The stream flow sediments dominate the Rait-Rihlu fans, whereas the debris flow sediments dominate the Kangra and Palampur fans. The fan sequences are also marked by the formation of strongly developed paleosols on loess (L1–L3 loess paleosols) and weakly developed paleosols on fluvial deposits in response to the tectonics and climate change in NW Himalayas. Formation of the loess in proximal and distal settings of the alluvial fans is related to the cool–dry climates during the advance of glaciers in the adjoining areas at 78 ka, 44 ka, 30 ka and 20 ka when climate was approaching towards the last glacial maxima. Field characters, micromorphology, grain size and clay minerals of these loessic deposits suggest strong pedogenesis of the loess during a warm–humid climate after the retreat of glaciers in the NW Himalayan region and are likely related to marine isotope stages (MIS4/5 in proximal and MIS2/3 in distal). The loess-paleosols show some degree of syndepositional pedogenesis in upper horizons and are accretionary in nature. Weakly expressed pedogenic features in fluvial and debris flow deposits suggest rapid sedimentation over unstable surfaces related to the reactivation of Main Boundary Thrust (MBT) and other regional faults." @default.
- W2006402605 created "2016-06-24" @default.
- W2006402605 creator A5040782684 @default.
- W2006402605 creator A5050511591 @default.
- W2006402605 creator A5067030119 @default.
- W2006402605 date "2009-01-01" @default.
- W2006402605 modified "2023-09-30" @default.
- W2006402605 title "Late Quaternary alluvial fans and paleosols of the Kangra basin, NW Himalaya: Tectonic and paleoclimatic implications" @default.
- W2006402605 cites W1964145151 @default.
- W2006402605 cites W1965621039 @default.
- W2006402605 cites W1969403464 @default.
- W2006402605 cites W1970988563 @default.
- W2006402605 cites W1973535507 @default.
- W2006402605 cites W1974461150 @default.
- W2006402605 cites W1975183604 @default.
- W2006402605 cites W1975280725 @default.
- W2006402605 cites W1977711728 @default.
- W2006402605 cites W1984042406 @default.
- W2006402605 cites W1987962922 @default.
- W2006402605 cites W1990069172 @default.
- W2006402605 cites W1995062385 @default.
- W2006402605 cites W1995852274 @default.
- W2006402605 cites W1996437630 @default.
- W2006402605 cites W1996937223 @default.
- W2006402605 cites W2002325302 @default.
- W2006402605 cites W2005040507 @default.
- W2006402605 cites W2006103490 @default.
- W2006402605 cites W2008730403 @default.
- W2006402605 cites W2016437874 @default.
- W2006402605 cites W2018043648 @default.
- W2006402605 cites W2019665722 @default.
- W2006402605 cites W2020383293 @default.
- W2006402605 cites W2021333251 @default.
- W2006402605 cites W2023013227 @default.
- W2006402605 cites W2024047478 @default.
- W2006402605 cites W2024541711 @default.
- W2006402605 cites W2024901067 @default.
- W2006402605 cites W2028598879 @default.
- W2006402605 cites W2034600181 @default.
- W2006402605 cites W2037047850 @default.
- W2006402605 cites W2042148223 @default.
- W2006402605 cites W2043998579 @default.
- W2006402605 cites W2044952811 @default.
- W2006402605 cites W2045384364 @default.
- W2006402605 cites W2047661207 @default.
- W2006402605 cites W2050593833 @default.
- W2006402605 cites W2054576636 @default.
- W2006402605 cites W2055792591 @default.
- W2006402605 cites W2059342627 @default.
- W2006402605 cites W2060700378 @default.
- W2006402605 cites W2062393489 @default.
- W2006402605 cites W2062905267 @default.
- W2006402605 cites W2065505256 @default.
- W2006402605 cites W2065839082 @default.
- W2006402605 cites W2066572987 @default.
- W2006402605 cites W2072435302 @default.
- W2006402605 cites W2075236450 @default.
- W2006402605 cites W2076372859 @default.
- W2006402605 cites W2076462940 @default.
- W2006402605 cites W2076624485 @default.
- W2006402605 cites W2077452367 @default.
- W2006402605 cites W2079491771 @default.
- W2006402605 cites W2082511160 @default.
- W2006402605 cites W2085112425 @default.
- W2006402605 cites W2086576154 @default.
- W2006402605 cites W2089605952 @default.
- W2006402605 cites W2092821744 @default.
- W2006402605 cites W2094107565 @default.
- W2006402605 cites W2099265637 @default.
- W2006402605 cites W2100526905 @default.
- W2006402605 cites W2107211406 @default.
- W2006402605 cites W2109459276 @default.
- W2006402605 cites W2114541080 @default.
- W2006402605 cites W2115803110 @default.
- W2006402605 cites W2120248779 @default.
- W2006402605 cites W2123741297 @default.
- W2006402605 cites W2125023880 @default.
- W2006402605 cites W2130591901 @default.
- W2006402605 cites W2136797395 @default.
- W2006402605 cites W2139752032 @default.
- W2006402605 cites W2143826758 @default.
- W2006402605 cites W2157509621 @default.
- W2006402605 cites W2172236306 @default.
- W2006402605 cites W3046503776 @default.
- W2006402605 cites W4236383427 @default.
- W2006402605 doi "https://doi.org/10.1016/j.catena.2008.10.004" @default.
- W2006402605 hasPublicationYear "2009" @default.
- W2006402605 type Work @default.
- W2006402605 sameAs 2006402605 @default.
- W2006402605 citedByCount "36" @default.
- W2006402605 countsByYear W20064026052013 @default.
- W2006402605 countsByYear W20064026052014 @default.
- W2006402605 countsByYear W20064026052015 @default.
- W2006402605 countsByYear W20064026052016 @default.
- W2006402605 countsByYear W20064026052017 @default.
- W2006402605 countsByYear W20064026052018 @default.
- W2006402605 countsByYear W20064026052020 @default.
- W2006402605 countsByYear W20064026052021 @default.