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Titlebook: Kimberlites, Orangeites, and Related Rocks; Roger Howard Mitchell Book 1995 Springer Science+Business Media New York 1995 Petrogenesis.che

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书目名称Kimberlites, Orangeites, and Related Rocks
编辑Roger Howard Mitchell
视频videohttp://file.papertrans.cn/543/542731/542731.mp4
图书封面Titlebook: Kimberlites, Orangeites, and Related Rocks;  Roger Howard Mitchell Book 1995 Springer Science+Business Media New York 1995 Petrogenesis.che
出版日期Book 1995
关键词Petrogenesis; chemistry; classification; geochemistry; mineral; mineralogy; petrology; solid solution; coast
版次1
doihttps://doi.org/10.1007/978-1-4615-1993-5
isbn_softcover978-1-4613-5822-0
isbn_ebook978-1-4615-1993-5
copyrightSpringer Science+Business Media New York 1995
The information of publication is updating

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Kimberlites and Orangeites,een termed “micaceous kimberlites” or “group II kimberlites.” The discussion, in conjunction with detailed mineralogical studies described in Chapter 2, will demonstrate conclusively that kimberlites and orangeites cannot be derived from the same parental magma and thus are not genetically related.
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Petrogenesis of Orangeites and Kimberlites,ing from a stance of promoting their own particular bias, be it geophysical, experimental, geochemical, or tectonic, have devised contradictory models for a given magma type. Once introduced, such models are commonly promoted by their originators without impartial reflection on all aspects of the problem or consideration of competing hypotheses.
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Kimberlites and Orangeites,group I kimberlites, with those of the group of diamond-bearing rocks which, in this work, are termed “orangeites.” The latter rocks have previously been termed “micaceous kimberlites” or “group II kimberlites.” The discussion, in conjunction with detailed mineralogical studies described in Chapter
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Mineralogy of Orangeites,s, previous studies did not attempt to delineate mineral assemblages and compositional trends which could be used to discriminate between each group of rocks. This chapter is based upon many new analyses of minerals in archetypal kimberlites and orangeites. The study of the latter is far from defini
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