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  • Articles
  • Other Sources  (2)
  • Articles (OceanRep)  (2)
  • GSA, Geological Society of America  (2)
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  • 1986  (2)
  • 1
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    Rhythmic bedding in Upper Cretaceous pelagic carbonate sequences: Varying sedimentary response to climatic forcing (1986)
    GSA, Geological Society of America
    In:  Geology, 14 (2). pp. 153-156.
    Details
    Publication Date: 2016-10-24
    Description: Rhythmic bedding is a prominent feature of North American and European Upper Cretaceous pelagic carbonate sequences deposited in epicontinental and continental-edge settings. Such bedding rhythms can result from variations in carbonate productivity, terrigenous dilution, redox conditions, or bottom currents. Each type of bedding cycle is expressed differently in the stratigraphic record but probably was caused by climatic cycles that are linked to variations in the Earth's orbital characteristics (Milankovitch cycles). Thus, pelagic carbonates of Cretaceous age acted as particularly sensitive recorders of orbitally induced changes in climate. Documentation of these bedding rhythms will permit detailed chronostratigraphic and lithostratigraphic correlations and will further illuminate depositional processes in Upper Cretaceous carbonate sequences.
    Type: Article , PeerReviewed
    Format: text
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  • 2
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    Oblique subduction and collision: Forearc tectonics of the Kuril arc (1986)
    GSA, Geological Society of America
    In:  Geology, 14 (5). pp. 404-407.
    Details
    Publication Date: 2019-05-24
    Description: The tectonics of the southwestern Kuril arc are a result of the oblique subduction of the Pacific plate at the Kuril Trench. In association with forearc sliver migration caused by the oblique subduction, collision tectonics occur at the leading margin of the sliver and tensional tectonics take place at the tapering margin. As a result of the collision, a deep crustal section of island arc is observed at the leading margin of the forearc sliver. Tectonics of the Kuril arc related to oblique subduction are different from those of the western Sunda arc, where backarc spreading occurs at the leading margin. This difference is due to margin morphology of the oblique subduction zone.
    Type: Article , PeerReviewed
    Format: text
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