Environmental change in the Early Permian of NE Svalbard: from a warm-water carbonate platform (Gipshuken Formation) to a temperate, mixed siliciclastic-carbonate ramp (Kapp Starostin Formation)
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چکیده
منابع مشابه
Sequence stratigraphy, basin morphology and sea-level history for the Permian Kapp Starostin Formation of Svalbard, Norway
Based on seven measured sections from Svalbard, the marine strata of the Permian Kapp Starostin Formation are arranged into seven transgressive–regressive sequences (TR1–TR7) of c. 4– 5 Ma average duration, each bound by a maximum regressive surface. Facies, including heterozoandominated limestones, spiculitic cherts, sandstones, siltstones and shales, record deposition within inner, middle and...
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Isotope data from bulk carbonates, micrite, marine calcite cements, non-skeletal grains and brachiopods indicate deposition of a wide spectrum of warm to cold water carbonates during the Ordovician and the Jurassic. This isotopic interpretation is supported by warm to cold climatic models proposed for the Ordovician and the Jurassic. These carbonates formed during the Greenhouse mode (condition...
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ژورنال
عنوان ژورنال: Facies
سال: 2010
ISSN: 0172-9179,1612-4820
DOI: 10.1007/s10347-010-0243-z