The multidisciplinary approaches on facies developments and depositional systems of the Bahçecik travertines, Gümüşhane, NE-Turkey
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A carbonate build-up, 12 m thick, was formed with some interruptions, through the middle Pleistocene period. For this study, two travertine sections (F and D) were extensively used to figure out palaeoenvironmental and palaeoclimatic proxies. The main precipitation cycles, separated by palaeosol levels, have been described and interpreted from a sedimentological perspective. The carbonate deposits consist of shrubs, crystalline crust, reed, laminated (micritic), pisoids, oncoids, calcite thin rafts and coated gas bubbles, lithoclasts, and palaeosol levels.
Tìm kiếm theo từ khóa liên quan:
Journal of Earth Sciences Depositional system Radiometric dating Stable isotopes Middle PleistoceneTài liệu liên quan:
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