Geochemical records of a bentonitic acid-tuff succession related to a transgressive systems tract-indication of changes in the volcanic sedimentation rate

A detailed stratigraphic and facies reconstruction of a bentonitized acid-tuff succession, deposited within the transgressive systems tract of the Upper Miocene-Sarmatian Ser-3 eustatic cycle, at Sajobabony, northern Hungary, was performed via petrographic, mineralogical and geochemical analyses. Th...

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Veröffentlicht in:	Clays and clay minerals 2008-02, Vol.56 (1), p.23-38
Hauptverfasser:	Puspoki, Z, Kozak, M, Kovacs-Palffy, P, Szepesi, J, McIntosh, R, Konya, P, Vincze, L, Gyula, G
Format:	Artikel
Sprache:	eng
Schlagworte:	Acid-Tuff Sedimentation bentonite Bentonites Biogeosciences Borsod Basin Cenozoic Central Europe chemical ratios clastic rocks clay mineralogy clay minerals Crystalline rocks Earth and Environmental Science Earth Sciences Earth, ocean, space Europe Exact sciences and technology geochemical indicators Geochemistry Hungary Igneous and metamorphic rocks petrology, volcanic processes, magmas igneous rocks lithofacies marine sedimentation Medicinal Chemistry Mineralogy Miocene montmorillonite Nanoscale Science and Technology Neogene pyroclastics reconstruction rock, sediment, soil Sajonabony Hungary Sarmatian sea-level changes sed rocks, sediments Sediment Condensation Sedimentary petrology sedimentary rocks sedimentation sedimentation rates SEQUENCE STRATIGRAPHY sheet silicates Silicates smectite Soil Science & Conservation Tertiary transgression tuff upper Miocene volcanic rocks
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