FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2079708607> ?p ?o ?g. }

• W2079708607 endingPage "33" @default.
• W2079708607 startingPage "1" @default.
• W2079708607 abstract "Abstract This paper provides a description and evaluation of the sedimentary facies and environments associated with a range of glacier thermal and dynamic regimes, with additional consideration given to the tectonic context. New and previously published data are evaluated together, and are presented from modern terrestrial and marine glacial sedimentary environments in order to identify a set of criteria that can be used to discriminate between different glacier thermal regimes and dynamic styles in the sedimentary record. Sedimentological data are presented from a total of 28 glaciers in 11 geographical areas that represent a wide range of contemporary thermal, dynamic and topographic regimes. In the context of “landsystems”, representatives from terrestrial environments include temperate glaciers in the European Alps, Patagonia, New Zealand, the Cordillera Blanca (Peru), cold glaciers in the Dry Valleys of Antarctica and the Antarctic Peninsula region, and polythermal valley glaciers in Svalbard, northern Sweden, the Yukon and the Khumbu Himal (Nepal). The glaciomarine environment is illustrated by data from cold and polythermal glacier margins on the East Antarctic continental shelf, and from a polythermal tidewater glacier in Svalbard, along with general observations from temperate glaciers in Alaska. These data show that temperate glacial systems, particularly in high-relief areas, are dominated by rockfall and avalanche processes, although sediments are largely reworked by glaciofluvial processes. Debris in polythermal glaciers is both thermally and topographically influenced. In areas of moderate relief, debris is mainly of basal glacial origin, and the resulting facies association is dominated by diamicton. In high-relief areas such as the Himalaya, the debris load in polythermal glaciers is dominated by rockfall and avalanche inputs, resulting in extensive accumulations of sandy boulder-gravel. Cold glaciers are dominated by basal debris-entrainment, but sediments are little modified from the source materials, which are typically sandy boulder-gravel from older till, and sand (from glaciofluvial, glaciolacustrine and aeolian sources). Similar facies associations, but with different facies geometry and thickness occur in equivalent glaciomarine settings. Application of these concepts can aid the interpretation of glacier thermal regime (and hence palaeoclimate) in Quaternary and ancient glacial systems." @default.
• W2079708607 created "2016-06-24" @default.
• W2079708607 creator A5059302618 @default.
• W2079708607 creator A5077838693 @default.
• W2079708607 date "2012-04-01" @default.
• W2079708607 modified "2023-09-29" @default.
• W2079708607 title "Discriminating glacier thermal and dynamic regimes in the sedimentary record" @default.
• W2079708607 cites W103267741 @default.
• W2079708607 cites W117493860 @default.
• W2079708607 cites W119587578 @default.
• W2079708607 cites W121244430 @default.
• W2079708607 cites W138184290 @default.
• W2079708607 cites W1436164 @default.
• W2079708607 cites W146953555 @default.
• W2079708607 cites W1511978764 @default.
• W2079708607 cites W1517978855 @default.
• W2079708607 cites W1527877727 @default.
• W2079708607 cites W1539981755 @default.
• W2079708607 cites W154649817 @default.
• W2079708607 cites W1556373907 @default.
• W2079708607 cites W1610356470 @default.
• W2079708607 cites W1617305328 @default.
• W2079708607 cites W1618673441 @default.
• W2079708607 cites W1635176114 @default.
• W2079708607 cites W1649616784 @default.
• W2079708607 cites W1652942762 @default.
• W2079708607 cites W1653241865 @default.
• W2079708607 cites W1656984195 @default.
• W2079708607 cites W1660744633 @default.
• W2079708607 cites W1661079537 @default.
• W2079708607 cites W1679179159 @default.
• W2079708607 cites W17188232 @default.
• W2079708607 cites W1773940553 @default.
• W2079708607 cites W1964142413 @default.
• W2079708607 cites W1965397651 @default.
• W2079708607 cites W1966118118 @default.
• W2079708607 cites W1970103104 @default.
• W2079708607 cites W1970645671 @default.
• W2079708607 cites W197118189 @default.
• W2079708607 cites W1972738781 @default.
• W2079708607 cites W1973160310 @default.
• W2079708607 cites W1973388129 @default.
• W2079708607 cites W1973668598 @default.
• W2079708607 cites W1974217503 @default.
• W2079708607 cites W1975212188 @default.
• W2079708607 cites W1975375220 @default.
• W2079708607 cites W1975536541 @default.
• W2079708607 cites W1978135243 @default.
• W2079708607 cites W1978836813 @default.
• W2079708607 cites W1979182231 @default.
• W2079708607 cites W1981719985 @default.
• W2079708607 cites W1982492550 @default.
• W2079708607 cites W1983950903 @default.
• W2079708607 cites W1984576625 @default.
• W2079708607 cites W1985470701 @default.
• W2079708607 cites W1991647533 @default.
• W2079708607 cites W1991732208 @default.
• W2079708607 cites W1993366640 @default.
• W2079708607 cites W1993585594 @default.
• W2079708607 cites W1993625011 @default.
• W2079708607 cites W1997884508 @default.
• W2079708607 cites W1999599895 @default.
• W2079708607 cites W2004203706 @default.
• W2079708607 cites W2005413889 @default.
• W2079708607 cites W2010205085 @default.
• W2079708607 cites W2010244876 @default.
• W2079708607 cites W2010608057 @default.
• W2079708607 cites W2011365368 @default.
• W2079708607 cites W2011830548 @default.
• W2079708607 cites W2013929551 @default.
• W2079708607 cites W2014398088 @default.
• W2079708607 cites W2014815515 @default.
• W2079708607 cites W2015066187 @default.
• W2079708607 cites W2017289858 @default.
• W2079708607 cites W2017514145 @default.
• W2079708607 cites W2018725137 @default.
• W2079708607 cites W2019928287 @default.
• W2079708607 cites W2020143766 @default.
• W2079708607 cites W2020184437 @default.
• W2079708607 cites W2021506221 @default.
• W2079708607 cites W2022269782 @default.
• W2079708607 cites W2023010184 @default.
• W2079708607 cites W2025881432 @default.
• W2079708607 cites W2026602853 @default.
• W2079708607 cites W2028796508 @default.
• W2079708607 cites W2030452761 @default.
• W2079708607 cites W2031026465 @default.
• W2079708607 cites W2032053405 @default.
• W2079708607 cites W2032185735 @default.
• W2079708607 cites W2034593721 @default.
• W2079708607 cites W2038270595 @default.
• W2079708607 cites W2043067765 @default.
• W2079708607 cites W2044583965 @default.
• W2079708607 cites W2044712975 @default.
• W2079708607 cites W2045100596 @default.
• W2079708607 cites W2047732929 @default.
• W2079708607 cites W2047811221 @default.
• W2079708607 cites W2049531708 @default.

• next