Matches in SemOpenAlex for { <https://semopenalex.org/work/W2038697026> ?p ?o ?g. }
- W2038697026 endingPage "38" @default.
- W2038697026 startingPage "5" @default.
- W2038697026 abstract "IGCP 449 (2000–2004) amassed data on fluvial systems world-wide, concentrating on key sequences, especially those benefiting from multiple lines of dating evidence. These archives are preserved either in terraced or stacked sequences, the latter confined to areas of subsidence. Terrace staircases record repeated incision (in response to progressive surface uplift), which, alternately with aggradation, is thought to have been climatically triggered. This triggering can be attributed to Quaternary (Milankovitch) climatic fluctuation, but the number of terraces produced in each Middle–Late Pleistocene 100 ka climatic cycle varies significantly between different systems. An unexpected result of this data collection has been the recognition of differing patterns of fluvial sedimentation and valley evolution over Neogene and Quaternary timescales, apparently related to different types of continental crust with different uplift/subsidence histories. These fall into three groups: (1) a typical uplifting pattern, with extensive terrace staircases of the type that dominate the global fluvial archive; (2) a subsiding pattern, with stacked fluvial sediments, usually coinciding with major depocentres; and (3) a stable pattern, with preservation of deposits related to channel diversion rather than significant incision. The third type, in which Early and pre-Quaternary deposits occur within a few metres of modern river level, is generally restricted to ancient cratonic or shield areas, which have apparently experienced minimal Late Cenozoic uplift, in marked contrast with most continental areas on more recently formed crust. There is also an intermediate situation, in Early Proterozoic crust, involving alternations of uplift and subsidence, with little resultant net vertical motion." @default.
- W2038697026 created "2016-06-24" @default.
- W2038697026 creator A5024127422 @default.
- W2038697026 creator A5050285080 @default.
- W2038697026 date "2008-10-01" @default.
- W2038697026 modified "2023-09-30" @default.
- W2038697026 title "Preservation patterns of Late Cenozoic fluvial deposits and their implications: Results from IGCP 449" @default.
- W2038697026 cites W119777211 @default.
- W2038697026 cites W1483030409 @default.
- W2038697026 cites W150431993 @default.
- W2038697026 cites W1560821745 @default.
- W2038697026 cites W1575335495 @default.
- W2038697026 cites W1678730710 @default.
- W2038697026 cites W176958342 @default.
- W2038697026 cites W179320619 @default.
- W2038697026 cites W1919635784 @default.
- W2038697026 cites W1963819174 @default.
- W2038697026 cites W1964924189 @default.
- W2038697026 cites W1964948888 @default.
- W2038697026 cites W1966265779 @default.
- W2038697026 cites W1967719167 @default.
- W2038697026 cites W1968515708 @default.
- W2038697026 cites W1969282238 @default.
- W2038697026 cites W1969627190 @default.
- W2038697026 cites W1969743895 @default.
- W2038697026 cites W1970645353 @default.
- W2038697026 cites W1972892880 @default.
- W2038697026 cites W1974743957 @default.
- W2038697026 cites W1975062784 @default.
- W2038697026 cites W1975577501 @default.
- W2038697026 cites W1976393269 @default.
- W2038697026 cites W1976894260 @default.
- W2038697026 cites W1977191667 @default.
- W2038697026 cites W1977693233 @default.
- W2038697026 cites W1978488084 @default.
- W2038697026 cites W1978532102 @default.
- W2038697026 cites W1978613040 @default.
- W2038697026 cites W1979148632 @default.
- W2038697026 cites W1980285440 @default.
- W2038697026 cites W1980994901 @default.
- W2038697026 cites W1981500141 @default.
- W2038697026 cites W1981819665 @default.
- W2038697026 cites W1984755569 @default.
- W2038697026 cites W1985855893 @default.
- W2038697026 cites W1987748614 @default.
- W2038697026 cites W1988043480 @default.
- W2038697026 cites W1988469793 @default.
- W2038697026 cites W1990104050 @default.
- W2038697026 cites W1993165032 @default.
- W2038697026 cites W1998450920 @default.
- W2038697026 cites W1999346157 @default.
- W2038697026 cites W2001948682 @default.
- W2038697026 cites W2002264489 @default.
- W2038697026 cites W2004131007 @default.
- W2038697026 cites W2004232151 @default.
- W2038697026 cites W2005626484 @default.
- W2038697026 cites W2006327284 @default.
- W2038697026 cites W2009873015 @default.
- W2038697026 cites W2009922693 @default.
- W2038697026 cites W2009968162 @default.
- W2038697026 cites W2010655199 @default.
- W2038697026 cites W2011939763 @default.
- W2038697026 cites W2012878705 @default.
- W2038697026 cites W2014131495 @default.
- W2038697026 cites W2022341298 @default.
- W2038697026 cites W2022474371 @default.
- W2038697026 cites W2022886555 @default.
- W2038697026 cites W2023275844 @default.
- W2038697026 cites W2023844609 @default.
- W2038697026 cites W2024139976 @default.
- W2038697026 cites W2025390516 @default.
- W2038697026 cites W2025411818 @default.
- W2038697026 cites W2026240099 @default.
- W2038697026 cites W2027601047 @default.
- W2038697026 cites W2027996875 @default.
- W2038697026 cites W2030309825 @default.
- W2038697026 cites W2032888676 @default.
- W2038697026 cites W2033570295 @default.
- W2038697026 cites W2036457311 @default.
- W2038697026 cites W2037281537 @default.
- W2038697026 cites W2038783157 @default.
- W2038697026 cites W2040501896 @default.
- W2038697026 cites W2040734165 @default.
- W2038697026 cites W2040944118 @default.
- W2038697026 cites W2042219694 @default.
- W2038697026 cites W2044135599 @default.
- W2038697026 cites W2045038743 @default.
- W2038697026 cites W2045377808 @default.
- W2038697026 cites W2045775785 @default.
- W2038697026 cites W2046117687 @default.
- W2038697026 cites W2046837339 @default.
- W2038697026 cites W2048268896 @default.
- W2038697026 cites W2050065049 @default.
- W2038697026 cites W2051362518 @default.
- W2038697026 cites W2051577255 @default.
- W2038697026 cites W2051787286 @default.
- W2038697026 cites W2052981078 @default.
- W2038697026 cites W2053118559 @default.