LEADER 03536nam  22006735  450 
001 9910831007703321
005 20240307115756.0
010   $a3-030-97882-6
024 7 $a10.1007/978-3-030-97882-2
035   $a(MiAaPQ)EBC31124751
035   $a(Au-PeEL)EBL31124751
035   $a(MiAaPQ)EBC31132532
035   $a(Au-PeEL)EBL31132532
035   $a(DE-He213)978-3-030-97882-2
035   $a(CKB)30305843300041
035   $a(EXLCZ)9930305843300041
100   $a20240205d2024      u|         0
101 0 $aeng
135   $aurcnu||||||||
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 10$aBasalts and Phase Diagrams $eAn Introduction to the Quantitative Use of Phase Diagrams in Igneous Petrology /$fby Stearns A. Morse
205   $a2nd ed. 2024.
210  1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2024.
215   $a1 online resource (417 pages)
311 08$aPrint version: Morse, Stearns A. Basalts and Phase Diagrams Cham : Springer International Publishing AG,c2024 9783030978808 
320   $aIncludes bibliographical references.
327   $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.
330   $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.
606   $aGeochemistry
606   $aEarth sciences
606   $aGeology
606   $aPhysical chemistry
606   $aPlanetary science
606   $aGeochemistry
606   $aEarth Sciences
606   $aGeology
606   $aPhysical Chemistry
606   $aPlanetary Science
615  0$aGeochemistry.
615  0$aEarth sciences.
615  0$aGeology.
615  0$aPhysical chemistry.
615  0$aPlanetary science.
615 14$aGeochemistry.
615 24$aEarth Sciences.
615 24$aGeology.
615 24$aPhysical Chemistry.
615 24$aPlanetary Science.
676   $a552.26028
700   $aMorse$b Stearns A.$f1931-$01772004
801  0$bMiAaPQ
801  1$bMiAaPQ
801  2$bMiAaPQ
906   $aBOOK
912   $a9910831007703321
996   $aBasalts and Phase Diagrams$94269596
997   $aUNINA