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Titlebook: Kimberlites and Their Xenoliths; J. Barry Dawson Book 1980 Springer-Verlag Berlin • Heidelberg 1980 Kimberlit.Xenolith.carbonatite.chemist

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书目名称Kimberlites and Their Xenoliths
编辑J. Barry Dawson
视频videohttp://file.papertrans.cn/543/542730/542730.mp4
丛书名称Minerals, Rocks and Mountains
图书封面Titlebook: Kimberlites and Their Xenoliths;  J. Barry Dawson Book 1980 Springer-Verlag Berlin • Heidelberg 1980 Kimberlit.Xenolith.carbonatite.chemist
描述In these days of information explosion and high-cost publishing, it is perhaps only reasonable for an author to convince the reading public that it is getting something worth reading. After all, intense research into the upper mantle over the past two decades has already resulted in a number of volumes on kim­ berlites and their xenoliths. So why yet another one? First, in this book I have concentrated on kimberlite as an individual rock-type and a sampler of the upper mantle, in the hope of complementing such monographs as Deep seated inclusions in kimberlites and the problem of the composition of the upper mantle by N. V. Sobolev and Geologie du Diamant by M. G. Bardet, which have concentrated more on specific aspects of kimberlite and upper mantle geology; as a result I have not attempted to describe diamond prospecting and mining and, although I have attempted to give some of the up-to-date views on xenolith petrology, the confines of space have not permitted me to explore the complexities of the upper mantle as deeply as has Sobolev. Second, the literature is vast and I have tried to pull together for the reader the wide range of views and infor­ mation presented both in the r
出版日期Book 1980
关键词Kimberlit; Xenolith; carbonatite; chemistry; formation; geochemistry; geology; mineral; mineralogy; petrograp
版次1
doihttps://doi.org/10.1007/978-3-642-67742-7
isbn_softcover978-3-642-67744-1
isbn_ebook978-3-642-67742-7Series ISSN 0343-2181
issn_series 0343-2181
copyrightSpringer-Verlag Berlin • Heidelberg 1980
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Distribution and Tectonic Setting of Kimberlites,spect of the tectonic setting of kimberlite, Dawson (1970) established that, in the case of the kimberlites of Africa, most kimberlites are confined to the ancient cratons (or areas underlain by the cratons), and that relatively few are to be found in the circum-cratonic fold-belts. This general pri
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Geochemistry of Kimberlites,al xenoliths. Moreover, mode of emplacement and degree of interaction with groundwater are very variable from intrusion to intrusion. Since all these variables, together with the partial and variable degrees of melting within the upper mantle at the onset of kimberlite generation (and subsequent mod
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The Megacryst Suite,s megacrysts (the terminology adopted here) and discrete nodules (Nixon and Boyd 1973b). In considering this mineral suite, the assumption is that the minerals are so large that they could not have been derived by fragmentation of upper-mantle xenolith rock types, the grain-size of which is usually
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Kimberlite Genesis,tions of crystals derived from the fragmentation of upper mantle rock types together with crystals derived from the crystallization of an ultramafic magma, these being finally cemented by the late-crystallization products of the magma. Since many of the kimberlite phenocrysts are broadly similar in
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