Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017307427> ?p ?o ?g. }
- W2017307427 endingPage "1096" @default.
- W2017307427 startingPage "1080" @default.
- W2017307427 abstract "We have determined the timing of glaciations in the Pamir (Tajikistan) and the Alay–Turkestan Range (Kyrgyzstan) using 10Be surface exposure dating. Glacial advances in the area have occurred >93–136, ∼60–80, (40–55), ∼27–25, ∼22–20, ∼19–17, ∼16–15, ∼15–13, and 11–9 cal ka BP. All Late Pleistocene glaciers in the Pamir, and the Alay–Turkestan Ranges have been valley glaciers except for the most extended glaciers on the Pamir plateau, which have formed local piedmont glaciations. In the eastern Pamir, these are characterized by ELA depressions of ∼370–380 m (THAR 0.5). In the Turkestan Range and Alay Range, ELA depressions at the same time were >750 and 600 m, respectively. Late Pleistocene glacier advances all over western High Asia were contemporaneous with climatic cold phases rather than monsoonal maxima. Their maximum extent and that of the western hemisphere ice sheets were asynchronous, due to increasing aridity in the region over the course of the Last Glacial. Late Pleistocene climate in Central Asia seems to have been influenced by the interplay of the westerly circulation and the Siberian anticyclone. Some indirect monsoonal influence in the eastern Pamir may be responsible for the existence of some of the Lateglacial moraine stages in this area. High altitude glaciers seem to have reached their maximum extent earlier (MIS 5–4) than low altitude glaciers (first half of MIS 3), possibly due to prolonged glacial aridity imparting with moisture advection onto high altitude sites, inducing glacial retreat, but prolonged cold during the same time imparting with glacier ablation at lower altitude sites, inducing glacial advance." @default.
- W2017307427 created "2016-06-24" @default.
- W2017307427 creator A5018217346 @default.
- W2017307427 creator A5024350939 @default.
- W2017307427 creator A5027366737 @default.
- W2017307427 creator A5044548235 @default.
- W2017307427 creator A5046876247 @default.
- W2017307427 creator A5073733406 @default.
- W2017307427 creator A5075826369 @default.
- W2017307427 creator A5084656266 @default.
- W2017307427 date "2006-05-01" @default.
- W2017307427 modified "2023-10-03" @default.
- W2017307427 title "Pleistocene glaciations of Central Asia: results from 10Be surface exposure ages of erratic boulders from the Pamir (Tajikistan), and the Alay–Turkestan range (Kyrgyzstan)" @default.
- W2017307427 cites W1580206559 @default.
- W2017307427 cites W1654234791 @default.
- W2017307427 cites W1966794661 @default.
- W2017307427 cites W1968010757 @default.
- W2017307427 cites W1968073064 @default.
- W2017307427 cites W1974474794 @default.
- W2017307427 cites W1975197770 @default.
- W2017307427 cites W1979258342 @default.
- W2017307427 cites W1983005920 @default.
- W2017307427 cites W1990613401 @default.
- W2017307427 cites W1991732208 @default.
- W2017307427 cites W2001629311 @default.
- W2017307427 cites W2002473398 @default.
- W2017307427 cites W2002643490 @default.
- W2017307427 cites W2003149311 @default.
- W2017307427 cites W2006646375 @default.
- W2017307427 cites W2008730403 @default.
- W2017307427 cites W2009425598 @default.
- W2017307427 cites W2012108278 @default.
- W2017307427 cites W2013878295 @default.
- W2017307427 cites W2014981382 @default.
- W2017307427 cites W2016518261 @default.
- W2017307427 cites W2016671909 @default.
- W2017307427 cites W2021333251 @default.
- W2017307427 cites W2022155332 @default.
- W2017307427 cites W2023705587 @default.
- W2017307427 cites W2024081263 @default.
- W2017307427 cites W2024532862 @default.
- W2017307427 cites W2025657816 @default.
- W2017307427 cites W2031790426 @default.
- W2017307427 cites W2033987981 @default.
- W2017307427 cites W2051536168 @default.
- W2017307427 cites W2054573382 @default.
- W2017307427 cites W2057946541 @default.
- W2017307427 cites W2066922084 @default.
- W2017307427 cites W2067202934 @default.
- W2017307427 cites W2070155641 @default.
- W2017307427 cites W2071818709 @default.
- W2017307427 cites W2076681545 @default.
- W2017307427 cites W2080960014 @default.
- W2017307427 cites W2082898543 @default.
- W2017307427 cites W2084688930 @default.
- W2017307427 cites W2093433348 @default.
- W2017307427 cites W2096484028 @default.
- W2017307427 cites W2104132498 @default.
- W2017307427 cites W2124588256 @default.
- W2017307427 cites W2131980920 @default.
- W2017307427 cites W2146062656 @default.
- W2017307427 cites W2158918602 @default.
- W2017307427 cites W307558897 @default.
- W2017307427 cites W4255199317 @default.
- W2017307427 doi "https://doi.org/10.1016/j.quascirev.2005.10.003" @default.
- W2017307427 hasPublicationYear "2006" @default.
- W2017307427 type Work @default.
- W2017307427 sameAs 2017307427 @default.
- W2017307427 citedByCount "111" @default.
- W2017307427 countsByYear W20173074272012 @default.
- W2017307427 countsByYear W20173074272013 @default.
- W2017307427 countsByYear W20173074272014 @default.
- W2017307427 countsByYear W20173074272015 @default.
- W2017307427 countsByYear W20173074272016 @default.
- W2017307427 countsByYear W20173074272017 @default.
- W2017307427 countsByYear W20173074272018 @default.
- W2017307427 countsByYear W20173074272019 @default.
- W2017307427 countsByYear W20173074272020 @default.
- W2017307427 countsByYear W20173074272021 @default.
- W2017307427 countsByYear W20173074272022 @default.
- W2017307427 countsByYear W20173074272023 @default.
- W2017307427 crossrefType "journal-article" @default.
- W2017307427 hasAuthorship W2017307427A5018217346 @default.
- W2017307427 hasAuthorship W2017307427A5024350939 @default.
- W2017307427 hasAuthorship W2017307427A5027366737 @default.
- W2017307427 hasAuthorship W2017307427A5044548235 @default.
- W2017307427 hasAuthorship W2017307427A5046876247 @default.
- W2017307427 hasAuthorship W2017307427A5073733406 @default.
- W2017307427 hasAuthorship W2017307427A5075826369 @default.
- W2017307427 hasAuthorship W2017307427A5084656266 @default.
- W2017307427 hasConcept C100834320 @default.
- W2017307427 hasConcept C100970517 @default.
- W2017307427 hasConcept C127313418 @default.
- W2017307427 hasConcept C134306372 @default.
- W2017307427 hasConcept C136996986 @default.
- W2017307427 hasConcept C151730666 @default.
- W2017307427 hasConcept C15739521 @default.
- W2017307427 hasConcept C15785411 @default.