• DocumentCode
    494400
  • Title

    Coastal-Open Marine Depositional System in the Kalpingtag Group of the Upper Silurian-Lower Ordovician in Kalping, Northwest Tarim Basin, China

  • Author

    Liu Xiaolin ; Zhang Jinliang

  • Author_Institution
    Coll. of Marine Geol., Ocean Univ. of China, Qingdao
  • Volume
    1
  • fYear
    2008
  • fDate
    21-22 Dec. 2008
  • Firstpage
    520
  • Lastpage
    524
  • Abstract
    The Upper Silurian-Lower Ordovician Kalpingtag Group, exposed in Kalping area, records part of the infill of the Tarim basin. The Kalpingtag Group has been subdivided into three informal lithologic units: lower, middle and upper, from field observations. Six facies associations (offshore, lower shoreface-offshore, lower shoreface, middle shoreface, upper shoreface, upper shoreface, foreshore) are recognized within the Kalpingtag Group. The sequence records that the Kalpingtag area has grown a complete transgression and regression process of deposition. The lower member of the Kalpingtag Group forms a reprogradational sequence in vertical, and the upper member of the Kalpingtag Group forms a progradation sequence in vertical.
  • Keywords
    geophysics computing; marine systems; sediments; China; Northwest Tarim Basin; Upper Silurian-Lower Ordovician Kalpingtag Group; coastal-open marine depositional system; regression process; Displays; Educational institutions; Educational technology; Geology; Geoscience and remote sensing; History; Marine technology; Oceans; Sea level; Storms; Kalpingtag Group; Tarim basin; sedimentary system;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    Education Technology and Training, 2008. and 2008 International Workshop on Geoscience and Remote Sensing. ETT and GRS 2008. International Workshop on
  • Conference_Location
    Shanghai
  • Print_ISBN
    978-0-7695-3563-0
  • Type

    conf

  • DOI
    10.1109/ETTandGRS.2008.102
  • Filename
    5070210