Global boundary stratotype section (6 Ergebnisse)

29pp, 13 figs, Printed Card Cover, VGC.

pp. 173-213, 1 pl., 2 figs., refs. Plain new wrs.

Taschenbuch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware 96 pp. Englisch.

Taschenbuch. Zustand: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. A Global Boundary Stratotype Section and Point, abbreviated GSSP, is an internationally agreed upon stratigraphic section which serves as the reference section for a particular boundary on the geologic time scale. The effort to define GSSPs is conducted by the International Commission on Stratigraphy, a part of the International Union of Geological Sciences. Most, but not all, GSSPs are based on paleontological changes. Hence GSSPs are usually described in terms of transitions between different faunal stages, though far more faunal stages have been described than GSSPs. The GSSP definition effort commenced in 1977. As of 2004, 45 of the 96 GSSPs required have been approved.…

Taschenbuch. Zustand: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Please note that the content of this book primarily consists of articlesavailable from Wikipedia or other free sources online. This is a list ofGlobal Boundary Stratotype Sections and Points. Since 1977, GlobalBoundary Stratotype Sections and Points (abbreviated GSSPs) areinternationally agreed upon stratigraphic sections of rock which serveas references for boundaries on the geologic time scale. They areselected by the International Commission on Stratigraphy based onmultiple factors, but their accessibility and the degree to which theyare representative of the same boundary on sections worldwide are amongthe most important. …

Taschenbuch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 96 pp. Englisch.