Titlebook: Basalts and Phase Diagrams; An Introduction to t Stearns A. Morse Textbook 2024Latest edition Springer Nature Switzerland AG 2024 Anorthite

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Forsterite-Anorthite-Silica: Incongruent Melting in a Ternary System,the role of the plane of silica saturation, modelled in this system by the line An-En. This role is like that of a check valve: liquids which pierce the plane towards SiO. cannot return, at atmospheric pressure, because of the incongruent melting of En to Fo +

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,Nepheline–Silica and the Rest of the Basalt Tetrahedron,ntal basalt tetrahedron. This review will serve as the background for examination, in succeeding chapters, of the effects of other components and of pressure on the phase relations of basaltic systems.

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Textbook 2024Latest editionnd equilibrium crystallization are rigorously examined. Examples of the use of phase diagrams are drawn from the literature of layered intrusions, redox equilibria in iron-bearing systems, and the high pressure equilibria of melting in the mantle.

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Inference and Empirical Examples,ur study model, the basalt tetrahedron (Chap. .). The present chapter explores a phase diagram containing iron-free olivine, namely forsterite, thereby illuminating some important principles of rock genesis as well as some simple but useful new principles of phase diagrams.

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Dealing with extremal independenceerved that will meet the upward layering rocks in what has been pleasantly named a sandwich horizon. Layered intrusions have important ways of revealing to us examples of phase equilibria that are fundamental. We only have to discover what these principles are.