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  • 152-914B; 152-915A; 152-918D; Age, dated; Age, dated material; Age, dated standard deviation; Age, maximum/old; Age, standard deviation; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Fission-track length, mean; Fission-track length, mean, standard deviation; Fission-tracks; Fission-tracks, density, counted in stan; Fission-tracks, induced; Fission-tracks, induced, density; Fission-tracks, spontaneous; Fission-tracks, spontaneous, density; Greenland Sea; Joides Resolution; Leg152; Number of observations; Number of tests; Ocean Drilling Program; ODP; Sample code/label; Standard deviation  (1)
  • PANGAEA  (1)
  • American Meteorological Society (AMS)
  • Blackwell Publishing Ltd
  • International Union of Crystallography
  • Nature Publishing Group
  • 1995-1999  (1)
  • 1990-1994
  • 1996  (1)
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  • PANGAEA  (1)
  • American Meteorological Society (AMS)
  • Blackwell Publishing Ltd
  • International Union of Crystallography
  • Nature Publishing Group
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  • 1996  (1)
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    PANGAEA
    In:  Supplement to: Clift, Peter D; Carter, Andrew; Hurford, Anthony J (1996): Constraints on the evolution of the East Greenland Margin: Evidence from detrital apatite in offshore sediments. Geology, 24(11), 1013-1016, https://doi.org/10.1130/0091-7613(1996)024%3C1013:COTEOT%3E2.3.CO;2
    Publikationsdatum: 2024-01-09
    Beschreibung: We test a new approach to understanding the tectonic evolution of passive margins by using fission-track analysis on detrital apatites from sediments deposited offshore East Greenland. These apatites have not undergone postdepositional track annealing and therefore reflect provenance. The apatites preserve a component of the source rocks' thermal history that otherwise may not be retained within the present-day outcrop. Fission-track derived denudational histories from samples at Ocean Drilling Program drill sites offshore East Greenland at lat 63°N are compared with data from the onshore Singertat Complex. Previous apatite fission-track studies and geomorphic mapping of the East Greenland coast have shown that locally up to 6 km of denudation may have occurred, implying significant tectonic or magmatic activity starting as much as 30 m.y. after breakup at 56 Ma. In contrast, apatite fission-track data presented here record 〈2 km of Cenozoic denudation in southeast Greenland, probably driven by magmatic underplating at the time of breakup. Large-magnitude, postrift denudation of East Greenland is restricted to the area around Kangerdlugssuaq (68°N). The timing (〈40-50 Ma) and magnitude are in accord with revised plume track models suggesting that the Iceland plume crossed the margin here during the late Eocene.
    Schlagwort(e): 152-914B; 152-915A; 152-918D; Age, dated; Age, dated material; Age, dated standard deviation; Age, maximum/old; Age, standard deviation; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Fission-track length, mean; Fission-track length, mean, standard deviation; Fission-tracks; Fission-tracks, density, counted in stan; Fission-tracks, induced; Fission-tracks, induced, density; Fission-tracks, spontaneous; Fission-tracks, spontaneous, density; Greenland Sea; Joides Resolution; Leg152; Number of observations; Number of tests; Ocean Drilling Program; ODP; Sample code/label; Standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 134 data points
    Standort Signatur Erwartet Verfügbarkeit
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