Titlebook: Simulating the Earth; Experimental Geochem John R. Holloway,Bernard J. Wood Book 1988 John R. Holloway & Bernard J. Wood 1988 chemistry.con

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978-0-04-445255-3John R. Holloway & Bernard J. Wood 1988

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The machines,ed most of the commonly used types and some interesting ones seldom used. The descriptions are not meant to be exhaustive; references are given for more detailed information. The Appendix contains elaborations of some of the points mentioned in this chapter. Each description follows a common format for easy comparison.

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,Metamorphic experiments on solid—fluid reactions,influences the whole metamorphic process. The importance of such a fluid is not, of course, obvious from looking at the finished product of the process, which may be a dense, volatile-free rock with about zero porosity and permeability. There are, however, several reasons for our asserting its importance.

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Igneous experiments on melts and crystals,d lived on Hawaii or Iceland). Tuttle & Bowen (1958) had the same objective when they proved that granites could form from magmas containing significant amounts of H.O. The objectives of modern experimental igneous petrologists include the following:

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John R. Holloway,Bernard J. Wood made throughout the development of this text. We would also like to thank Bob Wells for sharing with us his extensive knowledge of CW-complexes, Morse theory, and singular homology. Chapters 3 and 6, in particular, benefited significantly from the many insightful conver­ sations we had with Bob Wel

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