LEADER 05087nam 2200613Ia 450 001 9910437940703321 005 20200520144314.0 010 $a1-283-61186-4 010 $a9786613924315 010 $a3-642-28394-2 024 7 $a10.1007/978-3-642-28394-9 035 $a(CKB)2560000000090922 035 $a(EBL)972380 035 $a(OCoLC)809767527 035 $a(SSID)ssj0000738369 035 $a(PQKBManifestationID)11483817 035 $a(PQKBTitleCode)TC0000738369 035 $a(PQKBWorkID)10790639 035 $a(PQKB)10779444 035 $a(DE-He213)978-3-642-28394-9 035 $a(MiAaPQ)EBC972380 035 $a(PPN)168311895 035 $a(EXLCZ)992560000000090922 100 $a20120821h20122013 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aMetasomatism and the chemical transformation of rock $ethe role of fluids in terrestrial and extraterrestrial processes /$fDaniel E. Harlov, Hakon Austrheim 205 $a1st ed. 2013. 210 $aBerlin ;$aHeidleberg $cSpringer-Verlag$d2012, c2013 215 $a1 online resource (804 p.) 225 0 $aLecture notes in earth system sciences 300 $aDescription based upon print version of record. 311 $a3-642-28393-4 320 $aIncludes bibliographical references and index. 327 $a1.  Metasomatism and the chemical transformation of rock: Rock-mineral-fluid interaction in terrestrial and extraterrestrial environments. -2. The Chemical Composition of Metasomatic Fluids in the Crust -- 3. Thermodynamic modeling and thermobarometry of metasomatized rocks -- 4. Structural controls of metasomatism on a regional scale -- 5. Mechanisms of metasomatism and metamorphism on the local mineral scale: The role of dissolution-reprecipitation during mineral re-equilibration. - 6. Geochronology of metasomatic events.-7. Effects of metasomatism on mineral systems and their host rocks: alkali metasomatism, skarns, greisens, tourmalinites, rodingites, black-wall alteration and listevenites -- 8. Metasomatism within the ocean crust -- 9. Metasomatism in subduction zones of subducted oceanic slabs, mantle wedges, and the slab-mantle interface -- 10. Metasomatism during High-Pressure Metamorphism: Eclogites and Blueschist-Facies Rocks -- 11. Prograde, peak and retrograde metamorphic fluids and associated metasomatism in upper amphibolite to granulite facies transition zones -- 12.  Mantle Metasomatism -- 13.   Mapping the distribution of fluids in the crust and lithospheric mantle utilizing geophysical methods -- 14. A Hydromechanical Model for Lower Crustal Fluid Flow -- 15. Metasomatism in the early solar sysem: The record fron Chondritic meteorites. 330 $aFluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth?s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle. 410 0$aLecture Notes in Earth System Sciences,$x2193-8571 606 $aMetasomatism (Mineralogy) 606 $aMineralogy 615 0$aMetasomatism (Mineralogy) 615 0$aMineralogy. 676 $a612.799 700 $aHarlov$b Daniel E$01763361 701 $aAustrheim$b H$g(Hakon)$01763362 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910437940703321 996 $aMetasomatism and the chemical transformation of rock$94203746 997 $aUNINA