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An international team of over forty stratigraphic experts have helped to build the most up-to-date international stratigraphic framework for the Precambrian and Phanerozoic. This successor to A Geologic Time Scale 1989 by W. Brian Harland et al. (CUP 0521 387655) begins with an introduction to the theory and methodology behind the construction of the new time scale. The main part of the book is devoted to the scale itself, systematically presenting the standard subdivisions at all levels using a variety of correlation markers. Extensive use is made of isotope geochronology, geomathematics and orbital tuning to produce a standard geologic scale of unprecedented detail and accuracy with a full error analysis. A wallchart summarising the whole time scale, with paleogeographic reconstructions throughout the Phanerozoic, is included in the back of the book. The time scale will be an invaluable reference source for academic and professional researchers and students.
Geological time. --- Age of rocks --- Geochronology --- Geochrony --- Rocks --- Time, Geological --- Chronology --- Historical geology --- Sequence stratigraphy --- Age
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A successor to A Geologic Time Scale 1989 (Cambridge, 1990), this volume introduces the theory and methodology behind the construction of the new time scale, before presenting the scale itself in extensive detail. An international team of over forty stratigraphic experts develops the most up-to-date international stratigraphic framework for the Precambrian and Phanerozoic eras. A large wallchart summarizing the time scale at the back of the book completes this invaluable reference for researchers and students.
Geological time --- Temps géologique --- Géologie --- Geology --- Évolution --- evolution --- 551.7 --- Historical geology. Stratigraphy --- Geological time. --- 551.7 Historical geology. Stratigraphy --- Temps géologique --- Age of rocks --- Geochronology --- Geochrony --- Rocks --- Time, Geological --- Chronology --- Historical geology --- Sequence stratigraphy --- Age --- evolution.
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