FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2193408970> ?p ?o ?g. }

• W2193408970 endingPage "162" @default.
• W2193408970 startingPage "147" @default.
• W2193408970 abstract "Detailed field mapping of glacial and paraglacial landforms supported by optical and radiocarbon dating is used to reconstruct the history of late Quaternary glaciation and landform evolution in the Trans Himalayan region of the upper Dhauliganga valley. The study identifies four events of glaciations with decreasing magnitude which are termed as Purvi Kamet Stage -Ia (PKS-Ia), PKS-Ib, PKS-II, PKS-III and PKS-IV respectively. The oldest PKS-Ia and Ib are assigned the Marine Isotopic Stgae-3 (MIS-3), the PKS-II to the Last Glacial Maximum (MIS-2), PKS-III dated to 7.9 ± 0.7 ka, and the PKS-IV is dated to 3.4 ± 0.3 ka and 1.9 ± 0.2 ka respectively. The largest valley glaciations viz. the (PKS-Ia) occurred during the strengthened summer monsoon corresponding to the MIS-3, following this, the recessional moraines (PKS-Ib) represent the gradual decline in summer monsoon towards the later part of MIS-3. The valley responded to the global Last Glacial Maximum (LGM), which is represented by the PKS-II moraine implying the influence of strengthened mid-latitude westerlies during the LGM. The post-LGM deglaciation was associated with the onset of summer monsoon and is represented by the deposition of four distinct outwash gravel terraces. The early Holocene PKS-III glaciation occurred around 7.9 ± 0.7 ka and broadly coincides with the early Holocene cooling event (8.2 ka). This was followed by the deposition of stratified scree deposits and the alluvial fan (between 5.5 ka and 3 ka) during the mid to late Holocene aridity. This was followed by marginal re-advancement of the valley glacier (viz. PKS-IV) during the late Holocene cool and moist climate. Although glaciers respond to a combination of temperature and precipitation changes, however during the Holocene it seems that temperature played a major role in driving the glaciation." @default.
• W2193408970 created "2016-06-24" @default.
• W2193408970 creator A5010187163 @default.
• W2193408970 creator A5010758021 @default.
• W2193408970 creator A5012550172 @default.
• W2193408970 creator A5013094342 @default.
• W2193408970 creator A5051393618 @default.
• W2193408970 creator A5051699027 @default.
• W2193408970 creator A5054615362 @default.
• W2193408970 date "2015-12-01" @default.
• W2193408970 modified "2023-10-07" @default.
• W2193408970 title "Chronology of late Quaternary glaciation and landform evolution in the upper Dhauliganga valley, (Trans Himalaya), Uttarakhand, India" @default.
• W2193408970 cites W1646758270 @default.
• W2193408970 cites W1964639623 @default.
• W2193408970 cites W1965081522 @default.
• W2193408970 cites W1965240347 @default.
• W2193408970 cites W1965426804 @default.
• W2193408970 cites W1966794661 @default.
• W2193408970 cites W1968859838 @default.
• W2193408970 cites W1980425636 @default.
• W2193408970 cites W1981175426 @default.
• W2193408970 cites W1983699392 @default.
• W2193408970 cites W1985357586 @default.
• W2193408970 cites W1986442196 @default.
• W2193408970 cites W1991233930 @default.
• W2193408970 cites W1994191822 @default.
• W2193408970 cites W1994958984 @default.
• W2193408970 cites W1995083616 @default.
• W2193408970 cites W1996227144 @default.
• W2193408970 cites W1998970305 @default.
• W2193408970 cites W2002431247 @default.
• W2193408970 cites W2002699130 @default.
• W2193408970 cites W2004028082 @default.
• W2193408970 cites W2008730403 @default.
• W2193408970 cites W2011546530 @default.
• W2193408970 cites W2011601507 @default.
• W2193408970 cites W2012428664 @default.
• W2193408970 cites W2014341121 @default.
• W2193408970 cites W2014411114 @default.
• W2193408970 cites W2014829762 @default.
• W2193408970 cites W2014981382 @default.
• W2193408970 cites W2021102809 @default.
• W2193408970 cites W2021760823 @default.
• W2193408970 cites W2022187256 @default.
• W2193408970 cites W2023092830 @default.
• W2193408970 cites W2040993341 @default.
• W2193408970 cites W2053161685 @default.
• W2193408970 cites W2053332071 @default.
• W2193408970 cites W2054573382 @default.
• W2193408970 cites W2059677625 @default.
• W2193408970 cites W2060700378 @default.
• W2193408970 cites W2062610572 @default.
• W2193408970 cites W2062840728 @default.
• W2193408970 cites W2065839082 @default.
• W2193408970 cites W2066948374 @default.
• W2193408970 cites W2069744895 @default.
• W2193408970 cites W2071818709 @default.
• W2193408970 cites W2072598175 @default.
• W2193408970 cites W2074568669 @default.
• W2193408970 cites W2075394653 @default.
• W2193408970 cites W2075892097 @default.
• W2193408970 cites W2076338628 @default.
• W2193408970 cites W2077126986 @default.
• W2193408970 cites W2084226571 @default.
• W2193408970 cites W2089487604 @default.
• W2193408970 cites W2093161738 @default.
• W2193408970 cites W2094408279 @default.
• W2193408970 cites W2096484028 @default.
• W2193408970 cites W2100581187 @default.
• W2193408970 cites W2104132498 @default.
• W2193408970 cites W2117839159 @default.
• W2193408970 cites W2118168128 @default.
• W2193408970 cites W2128672385 @default.
• W2193408970 cites W2131980920 @default.
• W2193408970 cites W2143980021 @default.
• W2193408970 cites W2157332957 @default.
• W2193408970 cites W2159491279 @default.
• W2193408970 cites W2159506618 @default.
• W2193408970 cites W2159767807 @default.
• W2193408970 cites W2165166287 @default.
• W2193408970 cites W2165622380 @default.
• W2193408970 cites W2167268384 @default.
• W2193408970 cites W2168832818 @default.
• W2193408970 cites W2335382901 @default.
• W2193408970 cites W4242839126 @default.
• W2193408970 cites W4249751050 @default.
• W2193408970 doi "https://doi.org/10.1016/j.quascirev.2015.10.017" @default.
• W2193408970 hasPublicationYear "2015" @default.
• W2193408970 type Work @default.
• W2193408970 sameAs 2193408970 @default.
• W2193408970 citedByCount "45" @default.
• W2193408970 countsByYear W21934089702016 @default.
• W2193408970 countsByYear W21934089702017 @default.
• W2193408970 countsByYear W21934089702018 @default.
• W2193408970 countsByYear W21934089702019 @default.
• W2193408970 countsByYear W21934089702020 @default.
• W2193408970 countsByYear W21934089702021 @default.
• W2193408970 countsByYear W21934089702022 @default.

• next