Titlebook: Absolute Age Determination; Physical and Chemica Mebus A. Geyh,Helmut Schleicher Book 1990 Springer-Verlag Berlin Heidelberg 1990 Geochrono

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Literature,ktion mit Proze?partikeln. Bei ihrer Anwendung wird der Umfang der zu verarbeitenden Informationen vervielfacht, da über das reine Organisations-planungsergebnis hinaus die Proze?partikel, die Essenz, die Modellkonstruktionsschritte in Form der Versionen und die Begründungen für die Schritte zu verw

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geochronology is to calibrate and standardize chronostrati- graphic scales, to develop geological time scales that have a sensitive or at least useful resolution in order to place the geological events in the correct chronological order, and to assign their proper time spans. In practice, the application of g978-3-540-51276-9978-3-642-74826-4

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Book 1990morphology and composition of the Earth‘s crust, geologists have become increasingly interested in determination of absolute ages. A rela- tive geochronology was established on the basis of the lithostratigraphic and biostratigraphic principles developed during the last century. With the discovery o

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anged the morphology and composition of the Earth‘s crust, geologists have become increasingly interested in determination of absolute ages. A rela- tive geochronology was established on the basis of the lithostratigraphic and biostratigraphic principles developed during the last century. With the d

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E. Y. K. Ng,Leonard Jun Cong LooiNd (Sect. 6.1.6) methods. For example, only with these methods can time relationships be determined for the Precambrian. This is also true for younger basement rocks, for instance, for deciphering the development of an orogen, especially where there are no associated sediments that can be dated by other means.

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