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This book is mainly about the field geology of granites at all scales from that of a single outcrop to plutons and batholiths. All field geologists work initially at the scale of the outcrop, consequently most of the phenomena treated herein are those which are visible at outcrop scale. However, granites typically occur as plutons and batholiths, some of which are so large as to apparently defy any effort at systematic treatment. Having had the opportunity of mapping two very large and very different batholiths, namely the Coastal Batholith of Peru and the tin granites of Southeast Asia, I have found that it is possible to map large batholiths within a relatively short time, so that the geol...
Based on an international seminar, held Sept. 1986 in Cuzco, Peru, sponsored by Multiciencias (Peru) and Unesco.
The Geology of Ireland is about the island of Ireland as a physical whole and includes chapters on marine geology and the history of geology in Ireland. The text is intended for professional geologists and students of geology.
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Ernest J. Lanigan was the nephew of Sporting News founder Al Spink and one of three men in his immediate family to gain acclaim as a newspaperman. As sports editor for the New York Press and official scorer for a handful of World Series, he was the premier statistician of his day. Lanigan compiled the first baseball encyclopedia in 1922, and it is reprinted here with each of its twelve annual supplements. As the original publisher advertised on the book’s title page, it “[c]omprises a review of Professional Baseball, the history of all Major League Clubs, playing records and unique events, the batting, pitching and base running champions, World’s Series’ statistics and a carefully arranged alphabetical list of the records of more than 3500 Major League ball players, a feature never before attempted in print.”
''A voluminous encyclopedia of Tethyan geology and, as such, it provides an invaluable source of information for those interested in this region, and Earth history in general...The book is a must for the libraries of universities and geologic institutions.'' --- Palaios, October 1997 Volume 8 focuses on the Tethys oceanic realm and introduces new concepts such as 'transit plates' and 'seuils lithospheriques.' Contributors include new guides to understanding the distribution of Tethyan mineral and organic resources, and present insights into the role of carbonate platforms. Chapters are abundant with maps and illustrations.
courses more petrogenesis-orientated are im My main objective in writing this book has been to mediately confronted with a basic problem; the review the processes involved in present-day mag ma generation and their relationship to global average student does not have a strong enough tectonic processes. Clearly, these are fundamental background in geochemistry to understand the to our understanding of the petrogenesis of ancient finer points of most of the relevant publications in volcanic and plutonic sequences, the original tec scientific journals. It is virtually impossible to fmd tonic setting of which may have been obscured by suitable reading material for such students, as most subseque...
After a brief account of the stratigraphy in each case, the author summarises the structure of the main tectonic units of Western Europe, the units being defined within the framework of Precambrian, Caledonian, Hercynian and Alpine structures. The work provides accounts of these structural units both for geological study in general and for field visits for advanced school level and research students. A useful complementary volume to 'The Structure of the British Isles' (Anderson and Owen).
The origin of granite has for long fascinated geologists though serious debate on the topic may be said to date from a famous meeting of the Geological Society of France in 1847. My own introduction to the subject began exactly one hundred years later when, in an interview with Profes sor H. H. Read, I entered his study as an amateur fossil collector and left it as a committed granite petrologist - after just ten minutes! I can hardly aspire to convert my reader in so dramatic a way, yet this book is an attempt, however inadequate, to pass on the enthusiasm that I inherited, and which has been reinforced by innumerable discussions on the outcrop with granitologists of many nationalities and ...