Titlebook: Quantitative Geology of Late Jurassic Epicontinental Sediments in the Jura Mountains of Switzerland; Reinhart A. Gygi Book 2012 Springer B

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Previous Work, 338 of an unabridged, undated reprint, second edition by Dover, New York). According to ., on p. 344 of this reprint, A. L. ., the founder of modern chemistry, distinguished on p. 350, Pl. 7 of a study published in 1789 on marine strata preserved on land, “littoral banks” from “pelagic banks” which

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Paleogeography and Paleoclimate,e Bohemian Massif (. 2000a, Fig. 2, adapted and simplified after . 1988, Pl. 13, and refigured here as Fig. 1.1). Sediment was then shed from the island south- and southeastward into the epicontinental, Rhodano-Swabian Basin (Fig. 2). The epicontinental basin was filled in the process in northwester

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Hermatypic Coral Assemblages: Growth Form, Spatial Distribution, and Paleobathymetry, most widespread coral biostromes are those in the Liesberg Member with a matrix which was primarily a mixture of calcareous and argillaceous mud. Coral biostromes in a matrix of primarily pure calcareous mud occur at the basinward margin of the St-Ursanne Formation and in the Olten Member at the ba

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Rates of Sedimentation Varying Between Positive (Net), Zero, and Negative (Erosion), Basin was in the deposits investigated probably less than 5 m of now compacted sediment thickness per 10,000 years. The lower limit to a normal rate of sedimentation in a given deposit is where fossils of distinct biozones, like for instance ammonite casts, are still vertically separate, but not ye

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