FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2912051001> ?p ?o ?g. }

• W2912051001 endingPage "693" @default.
• W2912051001 startingPage "671" @default.
• W2912051001 abstract "The Pleistocene represents the youngest period of repeated widespread glaciation and interglacial intervals of both hemispheres. The Pleistocene–Holocene siliciclastics of the Peshawar Basin preserve a significant terrestrial record of palaeoclimatic fluctuations during this glacial time interval in northwest Pakistan at latitudes of 33–35°N. The sedimentological evidences indicate that the lower part of the stratal package consists of floodplain clay cycles overlain by lacustrine‐glaciofluvial rhythmites, that are followed by loess deposits and finally recent floodplain clays. The geochemical proxies demonstrate an overall cold‐arid climate with very low intensity of chemical weathering, whereas the clay mineralogy and related indices suggest intensifying physical erosion. The chemical index of alteration (CIA) reflects comparatively slightly higher (but still very low) intensity of chemical weathering for the lowermost part of the succession and uppermost loess deposits. The illite‐rich clay mineralogy of these two lithofacies associations also indicates the prevailing cold‐arid palaeoclimate. The low CIA and smectite‐rich clay mineralogy of the rhythmites, on the other hand, reflect deposition in poorly drained lakes. Multiple evidences for break‐out floods and the presence of ice‐rafted debris (IRD) within the rhythmites provide conclusive evidences for ice damming in the Peshawar Basin and drainage blockage due to the uplift of the Attock–Cherat Range. The floodplain clays indicate deposition in an interglacial semiarid–semihumid palaeoclimate preceding the Shanoz stage glaciation. The rhythmites correlate with the Shanoz, Yunz, and Borit Jheel glacial stages. The loess deposits indicate aeolian deposition in a cold, periglacial environment spanning over the late glacial maximum (LGM) interval." @default.
• W2912051001 created "2019-02-21" @default.
• W2912051001 creator A5004597504 @default.
• W2912051001 creator A5012173442 @default.
• W2912051001 creator A5037387669 @default.
• W2912051001 creator A5042058687 @default.
• W2912051001 creator A5071561016 @default.
• W2912051001 date "2019-01-21" @default.
• W2912051001 modified "2023-10-16" @default.
• W2912051001 title "Sedimentation and glaciations during the Pleistocene: Palaeoclimate reconstruction in the Peshawar Basin, Pakistan" @default.
• W2912051001 cites W1157801866 @default.
• W2912051001 cites W1593195006 @default.
• W2912051001 cites W1895219099 @default.
• W2912051001 cites W1925236180 @default.
• W2912051001 cites W1943346833 @default.
• W2912051001 cites W1957133103 @default.
• W2912051001 cites W1965701586 @default.
• W2912051001 cites W1968721411 @default.
• W2912051001 cites W1974107268 @default.
• W2912051001 cites W1976765694 @default.
• W2912051001 cites W1980600502 @default.
• W2912051001 cites W1981135957 @default.
• W2912051001 cites W1990519987 @default.
• W2912051001 cites W1994007098 @default.
• W2912051001 cites W2001908936 @default.
• W2912051001 cites W2005691090 @default.
• W2912051001 cites W2009896465 @default.
• W2912051001 cites W2013502789 @default.
• W2912051001 cites W2016223358 @default.
• W2912051001 cites W2016267276 @default.
• W2912051001 cites W2016437874 @default.
• W2912051001 cites W2016848487 @default.
• W2912051001 cites W2017307427 @default.
• W2912051001 cites W2027385173 @default.
• W2912051001 cites W2028436359 @default.
• W2912051001 cites W2029401070 @default.
• W2912051001 cites W2032078206 @default.
• W2912051001 cites W2035333480 @default.
• W2912051001 cites W2037799531 @default.
• W2912051001 cites W2041897281 @default.
• W2912051001 cites W2043998579 @default.
• W2912051001 cites W206199318 @default.
• W2912051001 cites W2063603732 @default.
• W2912051001 cites W2068180451 @default.
• W2912051001 cites W2075493516 @default.
• W2912051001 cites W2077351412 @default.
• W2912051001 cites W2077844996 @default.
• W2912051001 cites W2085826736 @default.
• W2912051001 cites W2086653430 @default.
• W2912051001 cites W2087411929 @default.
• W2912051001 cites W2098205785 @default.
• W2912051001 cites W2099900276 @default.
• W2912051001 cites W2113660406 @default.
• W2912051001 cites W2115518283 @default.
• W2912051001 cites W2115575384 @default.
• W2912051001 cites W2117839159 @default.
• W2912051001 cites W2120764192 @default.
• W2912051001 cites W2123741297 @default.
• W2912051001 cites W2127170577 @default.
• W2912051001 cites W2128497774 @default.
• W2912051001 cites W2140690888 @default.
• W2912051001 cites W2142230882 @default.
• W2912051001 cites W2144048660 @default.
• W2912051001 cites W2144276115 @default.
• W2912051001 cites W2145791900 @default.
• W2912051001 cites W2148518454 @default.
• W2912051001 cites W2154930938 @default.
• W2912051001 cites W2167767686 @default.
• W2912051001 cites W2238965603 @default.
• W2912051001 cites W2306724485 @default.
• W2912051001 cites W2310910365 @default.
• W2912051001 cites W2314646464 @default.
• W2912051001 cites W2342754432 @default.
• W2912051001 cites W2468668528 @default.
• W2912051001 cites W2498112629 @default.
• W2912051001 cites W2504586865 @default.
• W2912051001 cites W2513287867 @default.
• W2912051001 cites W2601207146 @default.
• W2912051001 cites W2607205254 @default.
• W2912051001 cites W2745544456 @default.
• W2912051001 cites W2893383556 @default.
• W2912051001 cites W297513218 @default.
• W2912051001 cites W4232403897 @default.
• W2912051001 cites W4241114923 @default.
• W2912051001 cites W4249069860 @default.
• W2912051001 cites W4252032443 @default.
• W2912051001 doi "https://doi.org/10.1002/gj.3445" @default.
• W2912051001 hasPublicationYear "2019" @default.
• W2912051001 type Work @default.
• W2912051001 sameAs 2912051001 @default.
• W2912051001 citedByCount "6" @default.
• W2912051001 countsByYear W29120510012019 @default.
• W2912051001 countsByYear W29120510012020 @default.
• W2912051001 countsByYear W29120510012021 @default.
• W2912051001 countsByYear W29120510012022 @default.
• W2912051001 crossrefType "journal-article" @default.
• W2912051001 hasAuthorship W2912051001A5004597504 @default.
• W2912051001 hasAuthorship W2912051001A5012173442 @default.

• next