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Geosynclines
Geosynclines is devoted to the geosynclines concept, which states that the most elevated parts of the earth's crust-the mountains-had risen by a gigantic inversion of relief from the more depressed regions where they had originated. This book re-examines the concept in light of further geologic...
| Clasificación: | Libro Electrónico |
|---|---|
| Autor principal: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés Francés |
| Publicado: |
Amsterdam, New York,
Elsevier Pub. Co.,
1965.
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| Colección: | Developments in geotectonics ;
1. |
| Temas: | |
| Acceso en línea: | Texto completo Texto completo |
MARC
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| 100 | 1 | |a Aubouin, Jean. | |
| 245 | 1 | 0 | |a Geosynclines |c [Translated by Express Translation Service, London]. |
| 260 | |a Amsterdam, |a New York, |b Elsevier Pub. Co., |c 1965. | ||
| 300 | |a 1 online resource (xv, 335 pages) |b illustrations, maps (1) | ||
| 336 | |a text |b txt |2 rdacontent | ||
| 337 | |a computer |b c |2 rdamedia | ||
| 338 | |a online resource |b cr |2 rdacarrier | ||
| 490 | 1 | |a Developments in geotectonics ; |v 1 | |
| 504 | |a Includes bibliographical references (pages 289-309). | ||
| 506 | |3 Use copy |f Restrictions unspecified |2 star |5 MiAaHDL | ||
| 533 | |a Electronic reproduction. |b [Place of publication not identified] : |c HathiTrust Digital Library, |d 2010. |5 MiAaHDL | ||
| 538 | |a Master and use copy. Digital master created according to Benchmark for Faithful Digital Reproductions of Monographs and Serials, Version 1. Digital Library Federation, December 2002. |u http://purl.oclc.org/DLF/benchrepro0212 |5 MiAaHDL | ||
| 583 | 1 | |a digitized |c 2010 |h HathiTrust Digital Library |l committed to preserve |2 pda |5 MiAaHDL | |
| 588 | 0 | |a Print version record. | |
| 505 | 0 | |a Front Cover; Geosynclines; Copyright Page; Table of Contents; List of Figures and Tables; CHAPTER 1. Introduction; PART I: Historical Review: Birth and Development of the Geosynclinal Concept; CHAPTER 2. The Birth of the Geosynclinal Concept; J. HALL (1859); J.D. DANA (1866, 1873); E. HAUG (1900); CONCLUSIONS: THE AMERICAN AND EUROPEAN CONCEPTIONS OF THE GEOSYNCLINE; CHAPTER 3. The Attempts at Classification of Geosynclines; C. SCHUCHERT (1923); H. STILLE (1913-1940); M. KAY (1942-1951); A.V. PEYVE AND V.M. SINITZYN (1950); CONCLUSIONS | |
| 505 | 8 | |a PART II: The Geosynclinal Concept as Illustrated by the Mediterranean Chains of the Alpine CycleCHAPTER 4. The Hellenides; INTRODUCTION; PALAEOGEOGRAPHICAL AND STRUCTURAL FRAMEWORK; CONCLUSIONS; CHAPTER 5. The Organizational or Structural Pattern of a Geosyncline; INTRODUCTION; THE SIMPLE (OR ELEMENTARY) GEOSYNCLINE: THE EU-MIOGEO-SYNCLINE COUPLE; COMPLEX GEOSYNCLINES: DIVERGENT (CENTRIFUGAL) AND CONVERGENT (CENTRIPETAL) SYMMETRY; FURROWS, RIDGES, SIAL AND SIMA; CHAPTER 6. The Evolutionary Pattern of a Geosyncline; INTRODUCTION; THE EVOLUTIONARY PATTERN AT THE LEVEL OF THE FURROW | |
| 505 | 8 | |a THE EVOLUTIONARY PATTERN AT THE LEVEL OF THE ELEMENTARY GEOSYNCLINETHE EVOLUTIONARY PATTERN AT THE LEVEL OF THE COMPLEX GEOSYNCLINE; CHAPTER 7. Conclusions; GEOSYNCLINAL ORGANIZATION; GEOSYNCLINAL EVOLUTION; PART III: Some Characteristics of Geosynclines as Illustrated by the Mediterranean Chains of the Alpine Cycle; CHAPTER 8. Geosynclinal Sedimentation; THICKNESS OF GEOSYNCLINAL SEDIMENTS; GEOSYNCLINAL FACIES; GEOSYNCLINAL SUBSIDENCE; CHAPTER 9. Metamorphism and the Geosynclinal Concept; CHAPTER 10. Igneous Activity and the Geosynclinal Concept; GENERAL CONSIDERATIONS; THE OPHIOLITES | |
| 505 | 8 | |a CHAPTER 11. Geosynclinal TectonicsGENERAL CONSIDERATIONS; INTRACONTINENTAL CHAINS; GEOSYNCLINAL CHAINS; CLARIFICATION OF THE TERM NAPPE; CONCLUSIONS; CHAPTER 12. Geosynclinal Orogenesis (and Tectogenesis); GENERAL CONSIDERATIONS; GEOSYNCLINAL OROGENESIS; GEOSYNCLINAL TECTOGENESIS; THE PROBLEM OF EMBRYONIC TECTOGENESIS; CHAPTER 13. The Siting of Geosynclines; GENERAL CONSIDERATIONS; GEOSYNCLINAL MIGRATION; THE GENESIS OF GEOSYNCLINES; PART IV. Extension of the Geosynclinal Concept in the Alpine Sense in Space and Time; CHAPTER 14. The Geosynclinal Concept and the Present Epoch | |
| 505 | 8 | |a GENERAL CONSIDERATIONSTHE POST-GEOSYNCLINAL PERIOD: THE MEDITERRANEAN; THE LATE-GEOSYNCLINAL PERIOD: THE SUNDA ISLANDS; THE GEOSYNCLINAL PERIOD; CHAPTER 15. The Geosynclinal Concept and the Pre-Alpine Period; THE HERCYNIAN (VARISCAN) CHAIN IN EUROPE; GEOSYNCLINAL SERIES; LATE-GEOSYNCLINAL SERIES; POST-GEOSYNCLINAL SERIES; THE CALEDONIAN CHAIN IN EUROPE: SCANDINAVIA; THE PRECAMBRIAN CHAIN IN EUROPE: FINLAND; PART V: Synthesis; CHAPTER 16. General Conclusions; THE GEOSYNCLINAL PATTERN OF ORGANIZATION; THE GEOSYNCLINAL PATTERN OF EVOLUTION; COMPARISON WITH OLDER CHAINS; References; Index | |
| 520 | |a Geosynclines is devoted to the geosynclines concept, which states that the most elevated parts of the earth's crust-the mountains-had risen by a gigantic inversion of relief from the more depressed regions where they had originated. This book re-examines the concept in light of further geological evidence. The book is organized into four parts. Part I presents a detailed account of the birth and development of the geosynclinal concept. It shows that only the European (Alpine) concept of the geosyncline involves a fundamental palaeogeographical differentiation of mountain chains, and that it is. | ||
| 650 | 0 | |a Geosynclines. | |
| 650 | 0 | |a Folds (Geology) | |
| 650 | 6 | |a Plis (G�eologie) |0 (CaQQLa)201-0046742 | |
| 650 | 6 | |a G�eosynclinaux. |0 (CaQQLa)201-0117208 | |
| 650 | 7 | |a Folds (Geology) |2 fast |0 (OCoLC)fst00928555 | |
| 650 | 7 | |a Geosynclines |2 fast |0 (OCoLC)fst00941120 | |
| 650 | 1 | 7 | |a Geosynclinalen. |2 gtt |
| 776 | 0 | 8 | |i Print version: |a Aubouin, Jean. |t Geosynclines. |d Amsterdam, New York, Elsevier Pub. Co., 1965 |w (DLC) 64018517 |w (OCoLC)343358 |
| 830 | 0 | |a Developments in geotectonics ; |v 1. | |
| 856 | 4 | 0 | |u https://sciencedirect.uam.elogim.com/science/book/9781483229676 |z Texto completo |
| 856 | 4 | 0 | |u https://sciencedirect.uam.elogim.com/science/bookseries/04190254/1 |z Texto completo |