Conodont Biostratigraphy Og the Great Basin and Rocky Mountains

Conodont Biostratigraphy Og the Great Basin and Rocky Mountains PDF Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 190

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Conodont Biostratigraphy Og the Great Basin and Rocky Mountains

Conodont Biostratigraphy Og the Great Basin and Rocky Mountains PDF Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 190

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Conodont Biostratigraphy of the Great Basin and Rocky Mountains

Conodont Biostratigraphy of the Great Basin and Rocky Mountains PDF Author: Charles Albert Sandberg
Publisher:
ISBN:
Category : Conodonts
Languages : en
Pages : 190

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Conodont Biofacies and Provincialism

Conodont Biofacies and Provincialism PDF Author: David Leigh Clark
Publisher: Geological Society of America
ISBN: 0813721962
Category : Science
Languages : en
Pages : 347

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Paleozoic sequence stratigraphy, biostratigraphy, and biogeography

Paleozoic sequence stratigraphy, biostratigraphy, and biogeography PDF Author: John A
Publisher: Geological Society of America
ISBN: 9780813723211
Category : Science
Languages : en
Pages : 414

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Silurian Conodont Biostratigraphy of the Southwestern Great Basin

Silurian Conodont Biostratigraphy of the Southwestern Great Basin PDF Author: Richard Harry Miller
Publisher:
ISBN:
Category : Conodonts
Languages : en
Pages : 228

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Tectonic and Stratigraphic Studies in the Eastern Great Basin

Tectonic and Stratigraphic Studies in the Eastern Great Basin PDF Author: David MacArthur Miller
Publisher: Geological Society of America
ISBN: 0813711576
Category : Geology
Languages : en
Pages : 337

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Permian-Triassic Evolution of Tethys and Western Circum-Pacific

Permian-Triassic Evolution of Tethys and Western Circum-Pacific PDF Author: Yin Yin Hongfu
Publisher: Elsevier
ISBN: 0080538657
Category : Science
Languages : en
Pages : 413

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Permian and Triassic are the interval known for the integration and separation of Pangea, the closure of the Palaeotethys and the opening of Mesotethys. They were associated with a series of worldwide events including the Late Palaeozoic glaciation and succeeding extensive evaporatic and reef formations, the end-Palaeozoic regression, strong orogenies and widespread volcanism and magmatism, and finally, the Permo-Triassic biotic macro-extinction. These events resulted in the formation of enormous reserves of coal, petroleum, evaporites, phosphorites and metal resources. The Permian and Triassic thus constitutes a time interval particularly important both for understanding the Earth's history and for exploration of mineral resources.The book aims to reconstruct the Permian-Triassic history of Pangea, Palaeo-Tethys and Palaeo-Pacific through stratigraphic, palaeogeographic and other interdisciplinary approaches. It consists of two parts. Part 1 deals with regional stratigraphy of Tethyan and western Circum-Pacific countries which is the basis for interregional correlation, and palaeogeography. Part 2 deals with the biotic evolution at the Permian-Triassic transition, focusing on the major invertebrate groups: foraminifers, radiolarians, brachiopods, ammonoids and conodonts.

Conodonts and Zonation of the Upper Devonian in the Great Basin

Conodonts and Zonation of the Upper Devonian in the Great Basin PDF Author: David Leigh Clark
Publisher: Geological Society of America
ISBN: 0813711037
Category : Conodonts
Languages : en
Pages : 114

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Geologic and Hydrologic Characterization and Evaluation of the Basin and Range Province Relative to the Disposal of High-level Radioactive Waste

Geologic and Hydrologic Characterization and Evaluation of the Basin and Range Province Relative to the Disposal of High-level Radioactive Waste PDF Author: Betty M. Miller
Publisher:
ISBN:
Category : Arid regions
Languages : en
Pages : 472

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Conodont Biostratigraphy of Member A (Lower to Lower Middle Ordovician) Mountain Springs Formation, Southern Great Basin

Conodont Biostratigraphy of Member A (Lower to Lower Middle Ordovician) Mountain Springs Formation, Southern Great Basin PDF Author: Ann Louise Tirrell
Publisher:
ISBN:
Category : Conodonts
Languages : en
Pages : 360

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