Matches in SemOpenAlex for { <https://semopenalex.org/work/W2549366908> ?p ?o ?g. }
- W2549366908 endingPage "389" @default.
- W2549366908 startingPage "377" @default.
- W2549366908 abstract "Cryostratigraphy involves the description, interpretation and correlation of ground-ice structures (cryostructures) and their relationship to the host deposits. Recent advances in the study of ground ice and cryostratigraphy concern permafrost aggradation and degradation, massive-ice formation and evaluation of ground-ice content. Field studies have increased our knowledge of cryostructures and massive ground ice in epigenetic and syngenetic permafrost. Epigenetic permafrost deposits are relatively ice-poor and composed primarily of pore-filled cryostructures, apart from an ice-enriched upper section and intermediate layer. Syngenetic permafrost deposits are commonly identified from cryostructures indicative of an aggrading permafrost table and are characterised by a high ice content, ice-rich cryofacies and nested wedge ice. Degradation of ice-rich permafrost can be marked by thaw unconformities, truncated buried ice wedges, ice-wedge pseudomorphs and organic-rich ‘forest beds’. Studies of massive ground ice have focused on wedge ice, thermokarst-cave ice, intrusive ice and buried ice. Significant advances have been made in methods for differentiating between tabular massive-ice bodies of glacier and intrasedimental origin. Recent studies have utilised palynology, isotope geochemistry and hydrochemistry, in addition to sedimentary and cryostratigraphic analyses. The application of remote sensing techniques and laboratory methods such as computed tomography scanning has improved estimations of the ice content of frozen sediments. Copyright © 2016 John Wiley & Sons, Ltd." @default.
- W2549366908 created "2016-11-30" @default.
- W2549366908 creator A5006151779 @default.
- W2549366908 creator A5069872394 @default.
- W2549366908 creator A5079384381 @default.
- W2549366908 date "2016-08-08" @default.
- W2549366908 modified "2023-10-12" @default.
- W2549366908 title "Recent Advances (2008-2015) in the Study of Ground Ice and Cryostratigraphy" @default.
- W2549366908 cites W1490077097 @default.
- W2549366908 cites W1498807814 @default.
- W2549366908 cites W1508480791 @default.
- W2549366908 cites W1579757024 @default.
- W2549366908 cites W1630186597 @default.
- W2549366908 cites W1750884694 @default.
- W2549366908 cites W1882544065 @default.
- W2549366908 cites W1903775371 @default.
- W2549366908 cites W1909503148 @default.
- W2549366908 cites W1933340339 @default.
- W2549366908 cites W1945055045 @default.
- W2549366908 cites W1968029756 @default.
- W2549366908 cites W1968085013 @default.
- W2549366908 cites W1971211309 @default.
- W2549366908 cites W1976128787 @default.
- W2549366908 cites W1977977622 @default.
- W2549366908 cites W1985116337 @default.
- W2549366908 cites W1985862162 @default.
- W2549366908 cites W1987339341 @default.
- W2549366908 cites W1988767078 @default.
- W2549366908 cites W1990450660 @default.
- W2549366908 cites W1991004730 @default.
- W2549366908 cites W1994407221 @default.
- W2549366908 cites W1997471749 @default.
- W2549366908 cites W2000877125 @default.
- W2549366908 cites W2000948538 @default.
- W2549366908 cites W2003539462 @default.
- W2549366908 cites W2010634068 @default.
- W2549366908 cites W2011277092 @default.
- W2549366908 cites W2015952487 @default.
- W2549366908 cites W2025836343 @default.
- W2549366908 cites W2029603846 @default.
- W2549366908 cites W2030405636 @default.
- W2549366908 cites W2030434408 @default.
- W2549366908 cites W2048104745 @default.
- W2549366908 cites W2057551940 @default.
- W2549366908 cites W2060017624 @default.
- W2549366908 cites W2060267335 @default.
- W2549366908 cites W2063606729 @default.
- W2549366908 cites W2065847387 @default.
- W2549366908 cites W2072961858 @default.
- W2549366908 cites W2077425516 @default.
- W2549366908 cites W2082205233 @default.
- W2549366908 cites W2082817601 @default.
- W2549366908 cites W2082946325 @default.
- W2549366908 cites W2083100204 @default.
- W2549366908 cites W2089099577 @default.
- W2549366908 cites W2089554855 @default.
- W2549366908 cites W2096391605 @default.
- W2549366908 cites W2101765891 @default.
- W2549366908 cites W2112108348 @default.
- W2549366908 cites W2112822244 @default.
- W2549366908 cites W2113122118 @default.
- W2549366908 cites W2126183909 @default.
- W2549366908 cites W2129275591 @default.
- W2549366908 cites W2135283895 @default.
- W2549366908 cites W2136400902 @default.
- W2549366908 cites W2145593462 @default.
- W2549366908 cites W2149850102 @default.
- W2549366908 cites W2159204983 @default.
- W2549366908 cites W2186620552 @default.
- W2549366908 cites W2287050067 @default.
- W2549366908 cites W2293608471 @default.
- W2549366908 cites W52810790 @default.
- W2549366908 cites W99853961 @default.
- W2549366908 doi "https://doi.org/10.1002/ppp.1912" @default.
- W2549366908 hasPublicationYear "2016" @default.
- W2549366908 type Work @default.
- W2549366908 sameAs 2549366908 @default.
- W2549366908 citedByCount "37" @default.
- W2549366908 countsByYear W25493669082017 @default.
- W2549366908 countsByYear W25493669082018 @default.
- W2549366908 countsByYear W25493669082019 @default.
- W2549366908 countsByYear W25493669082020 @default.
- W2549366908 countsByYear W25493669082021 @default.
- W2549366908 countsByYear W25493669082022 @default.
- W2549366908 countsByYear W25493669082023 @default.
- W2549366908 crossrefType "journal-article" @default.
- W2549366908 hasAuthorship W2549366908A5006151779 @default.
- W2549366908 hasAuthorship W2549366908A5069872394 @default.
- W2549366908 hasAuthorship W2549366908A5079384381 @default.
- W2549366908 hasBestOaLocation W25493669082 @default.
- W2549366908 hasConcept C100970517 @default.
- W2549366908 hasConcept C111368507 @default.
- W2549366908 hasConcept C114793014 @default.
- W2549366908 hasConcept C127313418 @default.
- W2549366908 hasConcept C15098985 @default.
- W2549366908 hasConcept C1965285 @default.
- W2549366908 hasConcept C205649164 @default.
- W2549366908 hasConceptScore W2549366908C100970517 @default.