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001 978-3-030-97882-2
003 DE-He213
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020 _a9783030978822
_9978-3-030-97882-2
024 7 _a10.1007/978-3-030-97882-2
_2doi
050 4 _aQE514-516.5
072 7 _aRBGK
_2bicssc
072 7 _aSCI013000
_2bisacsh
072 7 _aRBGK
_2thema
100 1 _aMorse, Stearns A.
_eauthor.
_4aut
_4http://id.loc.gov/vocabulary/relators/aut
_970589
245 1 0 _aBasalts and Phase Diagrams
_h[electronic resource] :
_bAn Introduction to the Quantitative Use of Phase Diagrams in Igneous Petrology /
_cby Stearns A. Morse.
250 _a2nd ed. 2024.
264 1 _aCham :
_bSpringer International Publishing :
_bImprint: Springer,
_c2024.
300 _aXVI, 417 p. 252 illus., 11 illus. in color.
_bonline resource.
336 _atext
_btxt
_2rdacontent
337 _acomputer
_bc
_2rdamedia
338 _aonline resource
_bcr
_2rdacarrier
347 _atext file
_bPDF
_2rda
505 0 _a- Introduction -- Mineralogy and Chemistry of Basalts -- Crystals and Melts -- The Phase Rule as a Tool -- Diopside and Anorthite: Supposedly a Binary Eutectic System -- Plagioclase: The System An-Ab -- Diopside-Albite: A Complex System -- Diopside-Anorthite-Albite -- Forsterite-Diopside-Anorthite: A Basaltic Analog -- lncongruent Melting: The System Forsterite - Silica -- Forsterite-Anorthite-Silica: Incongruent Melting in a Ternary System -- Forsterite-Diopside-Silica: Pyroxenes and Their Reactions -- Layered Intrusions -- Nepheline-Silica and the Rest of the Basalt Tetrahedron -- Potassium: Petrogeny's Residua System and Ternary Feldspars -- Iron and Oxygen -- Iron-Bearing Olivines and Pyroxenes -- The Effects of High Pressure -- Effects of Volatiles at High Pressure -- Leftovers.
520 _aIn this newly revised and expanded edition the reader finds both an introduction to igneous petrology and an exposition of the quantitative use of phase diagrams in understanding the origin and crystallization history of basic magmas. The book provides a step-by- step analysis of crystallization and melting in a limited number of geologically significant phase diagrams. The limiting processes of fractional and equilibrium melting and fractional and 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.
650 0 _aGeochemistry.
_970590
650 0 _aEarth sciences.
_965010
650 0 _aGeology.
_965838
650 0 _aPhysical chemistry.
_965285
650 0 _aPlanetary science.
_970591
650 1 4 _aGeochemistry.
_970590
650 2 4 _aEarth Sciences.
_965010
650 2 4 _aGeology.
_965838
650 2 4 _aPhysical Chemistry.
_965285
650 2 4 _aPlanetary Science.
_970592
710 2 _aSpringerLink (Online service)
773 0 _tSpringer Nature eBook
776 0 8 _iPrinted edition:
_z9783030978808
776 0 8 _iPrinted edition:
_z9783030978815
856 4 0 _uhttps://doi.org/10.1007/978-3-030-97882-2
912 _aZDB-2-CMS
912 _aZDB-2-SXC
999 _c57484
_d57484