9780521545730 - permo-triassic events in the eastern tethys: stratigraphy classification and relations with the western tethys (world and regional geology, 2, band 2) (3 Ergebnisse)
- Softcover
Anbieter: Ria Christie Collections, Uxbridge, Vereinigtes KönigreichRia Christie Collections
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Zustand: New. In.
- Softcover
Anbieter: Kennys Bookstore, Olney, USAKennys Bookstore
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Zustand: New. This book describes and interprets Upper Permian and Lower Triassic rocks and their fossils in the region of the eastern Tethys, bringing together information gathered in the International Geological Correlation Programme Project 203. Editor(s): Sweet, Walter C.; Zunyi, Yang (China University of Geosciences, Wukan)…; Dickins, J. M.; Hongfu, Yin (China University of Geosciences, Wukan). Series: World and Regional Geology. Num Pages: 196 pages, 117 b/w illus. 22 tables. BIC Classification: RBGH. Category: (P) Professional & Vocational. Dimension: 213 x 279 x 18. Weight in Grams: 472. . 2010. Revised ed. paperback. . . . . Books ship from the US and Ireland.
- Softcover
Anbieter: AHA-BUCH GmbH, Einbeck, DeutschlandAHA-BUCH GmbH
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Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Permian and Triassic rocks in the eastern Tethyan region form continuous marine sequences that record the waning phases of the Paleozoic and the early stages of the Mesozoic eras. This book describes and interprets these rocks, summarizing the distri…bution of major fossil groups in a way that will allow detailed comparison with strata of comparable age in the western Tethys and other parts of the world. The sixteen contributions by forty authors are the culmination of the five-year long International Geological Correlation Programme Project 203. The detailed information presented here is gathered from many areas in the eastern Tethyan region - from France to Australia - and will be of use in the evaluation of the major changes in the global marine biosphere known to have taken place at the end of the Paleozoic era. The stratigraphic record for this fascinating segment of Earth history is not widespread elsewhere in the world and is most continuous in the region covered by this book.
