FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3037524286> ?p ?o ?g. }

• W3037524286 endingPage "103260" @default.
• W3037524286 startingPage "103260" @default.
• W3037524286 abstract "The occurrence of endorheic basins on the Tibetan Plateau, both in its Pleistocene history and (fewer in number) at the present day, has been attributed to the ‘basin-and-range’ character of the orogen; the understanding of their conversion to exorheic drainage is key to interpreting the evolution of the Yellow River and other river systems of the plateau. However, such basins also occur in areas of lower altitude and relief and can be observed to have been considerably more common in pre-Quaternary times. In many areas, for example the Mediterranean region, such basins, previously having accumulated stacked sedimentary sequences, typically ‘inverted’ in the late Pliocene or at around the Pliocene–Pleistocene transition, possibly as part of a response to the cooling of global climate and its effect on surface processes. Some basins have inverted later, at around the time of the Mid-Pleistocene Revolution, coinciding with the increased severity of climate resulting from the 100 ka Milankovich cycles that followed that change. The progressive incision into the fills of these inverted sedimentary basins has also been linked to this climatic influence, perhaps taking effect as a result of erosional isostatic uplift, which would have replaced the accumulation-induced subsidence (also isostatic) of the basins. NW Europe, including Britain, had sediment-accumulating basins in the Early Cenozoic; the timing of their inversion is poorly known as a result of the paucity of preserved evidence from the Late Cenozoic in such areas. Endorheic basins that survive at the present day are mainly in regions of relative aridity and are often controlled by active tectonic structures, such as the pull-apart basins of the Dead Sea Fault Zone and similar examples. This review discusses the evidence from different climatic regions, tectonic settings and areas of different crustal type, with a view to elucidating meaningful patterns that might throw light on this phenomenon." @default.
• W3037524286 created "2020-07-02" @default.
• W3037524286 creator A5013685647 @default.
• W3037524286 creator A5024127422 @default.
• W3037524286 creator A5050285080 @default.
• W3037524286 date "2020-10-01" @default.
• W3037524286 modified "2023-10-10" @default.
• W3037524286 title "Basin inversion: A worldwide Late Cenozoic phenomenon" @default.
• W3037524286 cites W1493546306 @default.
• W3037524286 cites W1500533402 @default.
• W3037524286 cites W1501196342 @default.
• W3037524286 cites W1516480294 @default.
• W3037524286 cites W1518561780 @default.
• W3037524286 cites W1525468096 @default.
• W3037524286 cites W1567259655 @default.
• W3037524286 cites W1572938283 @default.
• W3037524286 cites W1635581289 @default.
• W3037524286 cites W1751977707 @default.
• W3037524286 cites W183807806 @default.
• W3037524286 cites W1934540407 @default.
• W3037524286 cites W1963819174 @default.
• W3037524286 cites W1964641747 @default.
• W3037524286 cites W1964948888 @default.
• W3037524286 cites W1965390769 @default.
• W3037524286 cites W1967389310 @default.
• W3037524286 cites W1968721255 @default.
• W3037524286 cites W1969261790 @default.
• W3037524286 cites W1969743895 @default.
• W3037524286 cites W1970466639 @default.
• W3037524286 cites W1972694007 @default.
• W3037524286 cites W1975240730 @default.
• W3037524286 cites W1975577501 @default.
• W3037524286 cites W1975676133 @default.
• W3037524286 cites W1975813748 @default.
• W3037524286 cites W1976070788 @default.
• W3037524286 cites W1977013518 @default.
• W3037524286 cites W1978613040 @default.
• W3037524286 cites W1983126240 @default.
• W3037524286 cites W1985195204 @default.
• W3037524286 cites W1986562513 @default.
• W3037524286 cites W1987924913 @default.
• W3037524286 cites W1989322803 @default.
• W3037524286 cites W1989987275 @default.
• W3037524286 cites W1992837617 @default.
• W3037524286 cites W1995235969 @default.
• W3037524286 cites W1997591776 @default.
• W3037524286 cites W1998450920 @default.
• W3037524286 cites W1999824647 @default.
• W3037524286 cites W2003795761 @default.
• W3037524286 cites W2005960390 @default.
• W3037524286 cites W2005986282 @default.
• W3037524286 cites W2009218754 @default.
• W3037524286 cites W2009931505 @default.
• W3037524286 cites W2013457589 @default.
• W3037524286 cites W2015271100 @default.
• W3037524286 cites W2016850039 @default.
• W3037524286 cites W2018359976 @default.
• W3037524286 cites W2019335672 @default.
• W3037524286 cites W2022886555 @default.
• W3037524286 cites W2022939300 @default.
• W3037524286 cites W2022980126 @default.
• W3037524286 cites W2025390516 @default.
• W3037524286 cites W2029685759 @default.
• W3037524286 cites W2030145420 @default.
• W3037524286 cites W2030400694 @default.
• W3037524286 cites W2032130922 @default.
• W3037524286 cites W2032827003 @default.
• W3037524286 cites W2033982808 @default.
• W3037524286 cites W2034911751 @default.
• W3037524286 cites W2036853439 @default.
• W3037524286 cites W2038697026 @default.
• W3037524286 cites W2039030972 @default.
• W3037524286 cites W2040281292 @default.
• W3037524286 cites W2041774199 @default.
• W3037524286 cites W2042219694 @default.
• W3037524286 cites W2043339008 @default.
• W3037524286 cites W2045181013 @default.
• W3037524286 cites W2046278018 @default.
• W3037524286 cites W2046837339 @default.
• W3037524286 cites W2050585743 @default.
• W3037524286 cites W2052474254 @default.
• W3037524286 cites W2052563003 @default.
• W3037524286 cites W2052726527 @default.
• W3037524286 cites W2053607159 @default.
• W3037524286 cites W2054688467 @default.
• W3037524286 cites W2055220869 @default.
• W3037524286 cites W2061772198 @default.
• W3037524286 cites W2062797763 @default.
• W3037524286 cites W2063764726 @default.
• W3037524286 cites W2064420361 @default.
• W3037524286 cites W2065123927 @default.
• W3037524286 cites W2065505256 @default.
• W3037524286 cites W2065771995 @default.
• W3037524286 cites W2065997633 @default.
• W3037524286 cites W2066550909 @default.
• W3037524286 cites W2068891716 @default.
• W3037524286 cites W2070095213 @default.
• W3037524286 cites W2070272436 @default.

• next