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)
Facies - Germany
doi 10.1007/s10347-010-0243-z
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Date
November 4, 2010
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Springer Science and Business Media LLC