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Titlebook: Volcanic Successions Modern and Ancient; A geological approac R. A. F. Cas,J. V. Wright Book 1988 Springer Science+Business Media Dordrecht

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发表于 2025-3-21 18:16:59 | 显示全部楼层 |阅读模式
书目名称Volcanic Successions Modern and Ancient
副标题A geological approac
编辑R. A. F. Cas,J. V. Wright
视频video
概述Takes an original approach in using the method of facies and analysis and interpretation derived from sedimentology to integrate studies of both ancient and modern volcanic activity
图书封面Titlebook: Volcanic Successions Modern and Ancient; A geological approac R. A. F. Cas,J. V. Wright Book 1988 Springer Science+Business Media Dordrecht
描述.One of our aims in the book is to provide geologists with a sound basis for making their own well founded interpretations. For that reason we cover not only concepts about processes, and the nature of the products, but also methods and approaches that may be useful in analysing both modern and ancient successions. Most importantly, we treat the diversity of products in volcanic terrains as facies, and we use the method of facies analysis and interpretation as a means of constructing facies models for different volcanic settings. These models will, we hope, be useful as norms for comparison for workers in ancient terrains..The idea for this book came into being between 1981 and 1982 when J. V. W. came to Monash University to take up a Monash Postdoctoral Fellowship. During this period a short course on facies analysis in modern and ancient successions was put together, integrating J.V.W.‘s extensive volcanological experience in numerous modern volcanic terrains with R.A.F.C.‘s extensive sedimentological and volcanological experience in older volcanic and associated sedimentary successions in the Palaeozoic and Precambrian of Australia. The enthusiastic response from the participant
出版日期Book 1988
关键词classification; crystal; environment; facies; formation; gas; geology; igneous rock; metamorphism; water
版次1
doihttps://doi.org/10.1007/978-94-009-3167-1
isbn_ebook978-94-009-3167-1
copyrightSpringer Science+Business Media Dordrecht 1988
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发表于 2025-3-22 00:03:36 | 显示全部楼层
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R. A. F. Cas,J. V. Wrighter Markos/Kyrillosanaphora als dritte nur die Gregoriosanaphora halten konnte,. waren daneben am Ausgang der Spätantike, in einem kulturellen Rückzugsgebiet wie Nubien sogar noch bis ans Ende des ersten Jahrtausends, noch zahlreiche andere Formulare im Gebrauch, aus deren Vielfalt nicht nur die beid
发表于 2025-3-22 04:44:22 | 显示全部楼层
R. A. F. Cas,J. V. Wrights mythische Denken als eine Form der geistigen Auseinandersetzung mit diesen Problemen eine präzise Funktion. Eine Gesamtdarstellung der von griechischen Mythen wie auch von den Mythenbildern thematisierten Fragen käme somit einer Art Problemgeschichte der griechischen Zivilisation gleich.
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R. A. F. Cas,J. V. Wrightgskette, in ihrem nördlichen Teile Parnon genannt, im Süden weit über die Flufsmündung hinaus in das Vorgebirge Malea auslaufend. Weit höher, bis zu 2400 m steigend, ist der den Flufs im Westen begleitende Taygetos, welcher gleichfalls viel südlicher als die Flufsmündung im Vorgebirge Tainaron endet
发表于 2025-3-22 19:26:31 | 显示全部楼层
R. A. F. Cas,J. V. Wrightextent of the event, above all be consistently geared to this and limits are certainly always reached, possibly even exceeded, where this goal is no longer or only insufficiently achieved or this is even directly or indirectly counteracted or acted upon or correspondingly counterproductive effects u
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R. A. F. Cas,J. V. Wrightapters have, for the most part, explored separately: the world of combat and the world of home; the physical trauma to the combatant body, and the psychological trauma of grief. Its context is a nurse’s story that itself parades injured bodies in an act of remembrance and demonstrates the intimate c
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Subaqueous pyroclastic flows and deep-sea ash layers,or in very shallow water. We also consider many examples of widely dispersed deep-sea ash layers, which result from the distal fall-out of large-magnitude continental silicic eruptions. Marine processes which affect their distribution and accumulation are discussed, as well as a method for determini
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