LEADER 00911nam0-22003131i-450- 001 990006807190403321 005 20001010 035 $a000680719 035 $aFED01000680719 035 $a(Aleph)000680719FED01 035 $a000680719 100 $a20001010d--------km-y0itay50------ba 101 0 $aita 105 $ay-------001yy 200 1 $a<>APPALTI pubblici in Europa$eguida pratica e normativa comunitaria e nazionale in tema di$eappalti publici di forniture ..$f(A cura di) Giancarlo Forti. 205 $a2. ed. 210 $aMilano$cPirola$d1994. 215 $aXVIII, 686 p.$d24 cm 225 1 $aAppalti$v 676 $a341.75 702 1$aForti,$bGiancarlo 801 0$aIT$bUNINA$gRICA$2UNIMARC 901 $aBK 912 $a990006807190403321 952 $aIII T 211$b25543$fFSPBC 959 $aFSPBC 996 $aAPPALTI pubblici in Europa$9633254 997 $aUNINA DB $aGEN01 LEADER 00895nam0-2200301---450- 001 990010082670403321 005 20160622123217.0 010 $a978-84-9097-082-9 035 $a001008267 035 $aFED01001008267 035 $a(Aleph)001008267FED01 035 $a001008267 100 $a20160622d2015----km-y0itay50------ba 101 0 $aspa 102 $aES 105 $ay-------001yy 200 1 $aPolíticas lingüísticas en democracias multilingües: es evitable el conflicto?$fJorge Cagiao y Conde y Juan Jiménez-Salcedo (coords.) 210 $aMadrid$cLos libros de la catarata$dc2015 215 $a300 p.$d21 cm 676 $a342$v20$zita 702 1$aCagiao y Conde,$bJorge 702 1$aJiménez-Salcedo,$bJuan 801 0$aIT$bUNINA$gRICA$2UNIMARC 901 $aBK 912 $a990010082670403321 952 $aXIV bis C 17$b92 cos$fDDCIC 959 $aDDCIC 997 $aUNINA LEADER 01061nam a22002651i 4500 001 991001509389707536 005 20030210150818.0 008 030121s1987 uika||||||||||||||||eng 020 $a0861876261 035 $ab1215717x-39ule_inst 035 $aARCHE-024697$9ExL 040 $aDip.to Filologia Ling. e Lett.$bita$cA.t.i. 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Pandora Sicilia s.r.l. 100 1 $aVentola, Eija$0450900 245 14$aThe structure of social interaction :$ba systemic approach to the semiotics of service encounters /$cEija Ventola 260 $aLondon :$bFrances Pinter,$c1987 300 $aXIX, 267 p. :$bill. ;$c24 cm 440 0$aOpen linguistics series 650 4$aLinguistica$xInterazione 650 4$aAnalisi del discorso 907 $a.b1215717x$b02-04-14$c01-04-03 912 $a991001509389707536 945 $aLE008 L.L.I.D B III 75$g1$i2008000460860$lle008$o-$pE0.00$q-$rl$s- $t0$u0$v0$w0$x0$y.i12487624$z01-04-03 996 $aStructure of social interaction$9147832 997 $aUNISALENTO 998 $ale008$b01-04-03$cm$da $e-$feng$guik$h4$i1 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