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Titlebook: Aspects of a Stratigraphic System; Devonian D. L. Dineley Textbook 1984Latest edition Macmillan Publishers Limited 1984 Devonian.stratigrap

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https://doi.org/10.1007/978-3-642-84425-6ut an extensive Devonian continental record. This distinctive magnafacies is, however, also found in Late Silurian strata (Britain, Canada) and may extend into the Carboniferous in many regions (Europe, Greenland, U.S.A.).
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Theory of Flexible Systems Management different model. This is not to deny the usefulness of the original concept but it serves to emphasise that interpretations need to be regarded as temporary, to be changed as improvements in knowledge continue. Since most of what is on the previous pages of this book is culled from the literature i
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The Materials of Stratigraphy,canic deposits. Investigation starts with litho-logical and stratigraphical (or structural) features, proceeds to sedimentology and palaeontology, perhaps to experimental and comparative studies, and hopefully reaches a point where hypotheses can be put up like ‘Aunt Sallys’.
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Stratigraphy and the World Tectonic Model, and mountain belts is striking. Isostatic adjustment by uplift following orogeny explains the long-continuing role of orogenic belts as sources of sediment for new basins of deposition, but the initiation of the orogenic cycle has presented a problem. In recent years the new plate-tectonic models o
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Devonian Geography, different model. This is not to deny the usefulness of the original concept but it serves to emphasise that interpretations need to be regarded as temporary, to be changed as improvements in knowledge continue. Since most of what is on the previous pages of this book is culled from the literature i
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https://doi.org/10.1007/978-1-349-17663-2Devonian; stratigraphy; system; historical geology
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