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Titlebook: Carbonate Facies in Geologic History; James L. Wilson Textbook 1975 Springer-Verlag Berlin · Heidelberg 1975 Fazies.Gestein.Jura.Karbonatg

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Device Modeling and Circuit Elementsdescribes a variety of carbonate facies complexes given more or less in order of geologic age. These examples serve as documentation for many of the ideas expressed in the first three Chapters. The facies occur in many diverse tectonic settings and are found in shelf cycles, mounds and patch reefs o
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Fernando Corinto,Mauro Forti,Leon O. Chuapes of carbonate buildups produced in the clear and shallow seas around the southern extension of the North American craton. The sections containing these buildups remain lithologically varied because this was a time of general tectonic instability and considerable terrigenous sedimentation. Many of
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Fernando Corinto,Mauro Forti,Leon O. Chuaistically cyclic sediments are found in shelf areas although regular changes in sedimentary conditions may be reflected in many types of basinal sediments (evaporites, flysch, carbonate-shale rhythms). Cyclic shelf deposits are particularly common in the Late Paleozoic of the northern hemisphere. Th
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A simple model of DNA dynamics,ome of the significant and distinctive rock types in these strata include: coral-sponge reefs, Purbeckian fresh-water beds, Solnhofen platy limestone and the geosynclinal red nodular Ammonitico Rosso and pelagic Aptychus limestones.
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