Startseite Special Collection: Olivine: Rates and styles of planetary cooling on Earth, Moon, Mars, and Vesta, using new models for oxygen fugacity, ferric-ferrous ratios, olivine-liquid Fe-Mg exchange, and mantle potential temperature
Artikel
Lizenziert
Nicht lizenziert Erfordert eine Authentifizierung

Special Collection: Olivine: Rates and styles of planetary cooling on Earth, Moon, Mars, and Vesta, using new models for oxygen fugacity, ferric-ferrous ratios, olivine-liquid Fe-Mg exchange, and mantle potential temperature

  • Keith Putirka EMAIL logo
Veröffentlicht/Copyright: 5. April 2016
Veröffentlichen auch Sie bei De Gruyter Brill
Informationen für Autor*innen
American Mineralogist
Aus der Zeitschrift American Mineralogist Band 101 Heft 4

Abstract

Mantle potential temperatures (Tp) provide insights into mantle circulation and tests of whether Earth is the only planet to exhibit thermally bi-modal volcanism—a distinctive signature of modern plate tectonics. Planets that have a stagnant lid, for example, should exhibit volcanism that is uni-modal with Tp, since mantle plumes would have a monopoly on the genesis of volcanism. But new studies of magmatic ferric-ferrous ratios (XFe2O3liq/XFeOliq) (Cottrell and Kelley 2011) and the olivine-liquid Fe-Mg exchange coefficient, KD(Fe-Mg)Ol-liq (or KD) (Matzen et al. 2011) indicate that re-evaluations of Tp are needed. New tests and calibrations are thus presented for oxygen fugacity (fO2), XFe2O3liq/XFeOliq, potential temperature (Tp), melt fraction (F), KD, and peridotite enthalpies of fusion (∆Hfus) and heat capacities (CP). The new models for XFe2O3liq/XFeOliq and fO2 reduce error by 25–30%, and residual error for all models appears random; this last observation supports the common, but mostly untested, assumption that equilibrium is the most probable of states obtained by experiment, and perhaps in nature as well. Aggregate 1s error on Tp is as high as ~±77 °C, and estimates of F, and mantle olivine composition, are the greatest sources of error. Pressure and ∆Hfus account for smaller, but systematic uncertainties (a constant ∆Hfus can under-predict Texcess = Tpplume−Tpambient; assumptions of 1 atm can under-predict Tp). However, assumptions about whether parental magmas are incremental, accumulated, or isobaric batch melts induces no additional systematic error.

The new models show that maximum Tp estimates on the oldest samples from Earth, Mars, Moon, and Vesta, decrease as planet size decreases. This may be expected since Tp should scale with accretion energy and reflect the Clausius-Clapeyron slope for the melting of silicates and Fe-Ni alloys. This outcome, however, occurs only if shergottites (from Mars) are 4.3 Ga (e.g., Bouvier et al. 2009; Werner et al. 2014), and the highest MgO komatiites from Earth’s Archean era (27–30% MgO; Green et al. 1975) are used to estimate Tp. With these assumptions, Earth and Mars exhibit monotonic cooling, and support for Stevenson’s (2003) idea that smaller planets cool at similar rates (~90–135 °C/Ga), but at lower absolute temperatures. Tp estimates for Mars and Earth are also important in two other ways: Mars exhibits non-linear cooling, with rates as high as 275–550 °C/Ga in its first 0.5 Ga, and Archean volcanism on Earth was thermally bi-modal. Several hundred Archean volcanic compositions are in equilibrium with Fo92–94 olivine, and yield Tp modes at 1940 and 1720 °C, possibly representing plume and ambient mantle, respectively. These estimates compare to modern Tp values of 1560–1670 °C at Mauna Loa (plume) and 1330–1450 °C at MORB (ambient). We conclude that plate tectonics was active in some manner in the Archean, and that assertions of an Archean “thermal catastrophe” are exaggerated. Our new models also show that the modern Hawaiian source, when compared at the same T, has a lower fO2 compared to MORB, which would discount a Hawaiian source rich in recycled pyroxenite.

Keywords: Potential temperature; Mars; Vesta; Moon; secular cooling; mantle plumes; Archean, tectonics
Special collection papers can be found online at http://www.minsocam.org/MSA/AmMin/special-collections.html

Acknowledgments

Special and sincere thanks are owed to Cin-Ty Lee, Claude Herzberg, and Mike Garcia. Each provided thorough and thoughtful reviews—among the most helpful received on any paper. I greatly appreciate Mike Garcia’s attention to detail, which saved the manuscript from being published with even more errors than it likely already has, and for making the paper a much better read than the original. Reviews by Lee and Herzberg were also invaluable, as they prompted serious re-evaluation of several key issues, including Lee’s concerns about reconstruction of mantle geotherms, and Claude’s recognition of possible bi-modal volcanism in the Archean. I also thank the National Science Foundation for their generous support. This work grew out of two broadly related projects funded by NSF, 1250322 and 1250323.

References Cited

Abbott, D., Burgess, L., Longhi, J., and Smith, W.H.F. (1994) An empirical thermal history of Earth’s upper mantle. Journal of Geophysical Research, 99, 13835–13850.10.1029/94JB00112Suche in Google Scholar

Agee, C.B., and Walker, D. (1993) Olivine flotation in mantle melt. Earth and Planetary Science Letters, 114, 315–324.10.1016/0012-821X(93)90033-6Suche in Google Scholar

Allan, J.F., and Carmichael, I.S.E. (1984) Lamprophyric lavas in the Colima graben, SW Mexico. Contributions to Mineralogy and Petrology, 88, 203–216.10.1007/BF00380166Suche in Google Scholar

Ariskin, A.A. (2007) Parental magmas of lunar troctolite: genetic problems and estimated original compositions. Geochemistry International, 45, 413–427.10.1134/S0016702907050011Suche in Google Scholar

Asimow, P.D., Hirschmann, M.M., and Stolper, E.M. (1997) An analysis of variations in isentropic melt productivity. Philosophical Transactions of the Royal Society, 355, 255–281.10.1017/CBO9780511600050.004Suche in Google Scholar

Baker, M.B., and Stolper, E.M. (1994) Determining the composition of high-pressure mantle melts using diamond aggregates. Geochimica et Cosmochimica Acta, 58, 2811–2827.10.1016/0016-7037(94)90116-3Suche in Google Scholar

Baker, M.B., Hirschmann, M.M., Ghiorso, M.S., and Stolper, E.M. (1995) Compositions of near-solidus peridotite melts from experiments and thermodynamic calculations. Nature, 375, 308–311.10.1038/375308a0Suche in Google Scholar

Baker, M.B., Alves, S., and Stolper, E.M. (1996) Petrography and petrology of the Hawaii scientific drilling project lavas: inferences from olivine phenocryst abundances and compositions. Journal of Geophysical Research, 101, 11715–11727.10.1029/96JB00180Suche in Google Scholar

Barr, J.A., and Grove, T.L. (2013) Experimental petrology of the Apollo 15 group A green glasses: Melting primordial lunar mantle and magma ocean cumulate assimilation. Geochimica et Cosmochimica Acta, 106, 216–230.10.1016/j.gca.2012.12.035Suche in Google Scholar

Beattie, P. (1993) Olivine-melt and orthopyroxene-melt equilibria. Contributions to Mineralogy and Petrology, 115, 103–111.10.1007/BF00712982Suche in Google Scholar

Bernstein, S., Kelemen, P.B., and Hanghøj, K. (2007) Consistent olivine Mg# in cratonic mantle reflects Archean mantle melting to the exhaustion of orthopyroxene. Geology, 35, 459–462.10.1130/G23336A.1Suche in Google Scholar

Berry, A.J., Danyushevsky, L.V., O’Neill, H.St.C., Newville, M., and Sutton, S.R. (2008) Oxidation state of iron in komatiitic melt inclusions indicates hot Archean mantle. Nature, 455, 960–963.10.1038/nature07377Suche in Google Scholar

Bezos, A., and Humler, E. (2005) The Fe3+/Fe ratios of MORB glasses and their implications for mantle melting. Geochimica et Cosmochimica Acta, 69, 711–725.10.1016/j.gca.2004.07.026Suche in Google Scholar

Bickle, M.J., Ford, C.E., and Nisbet, E.G. (1977) The petrogenesis of peridotitic komatiites: Evidence from high-pressure melting experiments. Earth and Planetary Science Letters, 37, 97–106.10.1016/0012-821X(77)90150-9Suche in Google Scholar

Blichert-Toft, J., Arndt, N.T., Wilson, A., and Coetzee, G. (2015) Hf and Nd isotopic systematics of early Archean komatiites from surface sampling and ICDP drilling in the Barberton Greenstone Belot, South Africa. American Mineralogist, 100, 2396–2411.10.2138/am-2015-5325Suche in Google Scholar

Bolton, D. (1980) The computation of equivalent potential temperature. Monthly Weather Review, 108, 1046–1053.10.1175/1520-0493(1980)108<1046:TCOEPT>2.0.CO;2Suche in Google Scholar

Botcharnikov, R.E., Koepke, J., Holtz, F., McCammon, C., and Wilke, M. (2005) The effect of water activity on the oxidation and structural state of Fe in a ferrobasaltic melt. Geochimica et Cosmochimica Acta, 69, 5071–5085.10.1016/j.gca.2005.04.023Suche in Google Scholar

Borisov, A.A. (2010) Ferric-ferrous ratio in liquid iron oxides: Analysis and applications to natural basaltic melts. Petrology, 18, 471–481.10.1134/S0869591110050024Suche in Google Scholar

Bouvier, A., Blichert-Toft, J., and Albarede, F. (2009) Martian meteorite chronology and the evolution of the interior of Mars. Earth and Planetary Science Letters, 280, 285–295.10.1016/j.epsl.2009.01.042Suche in Google Scholar

Bradley, R.S. (1962) Thermodynamic calculations on phase equilibria involving fused salts. Part II. Solid solutions and application to the olivines. American Journal of Science, 260, 550–554.10.2475/ajs.260.7.550Suche in Google Scholar

Brown, J.M., and Shankland, T.J. (1981) Thermodynamic parameters in the Earth as determined from seismic profiles. Geophysical Journal of the Royal Astronomical Society, 66, 579–596.10.1111/j.1365-246X.1981.tb04891.xSuche in Google Scholar

Bunge, H-P. (2005) Low plume excess temperature and a high core heat flux inferred form non-adiabatic geotherms in internally heated mantle circulation models. Physics of the Earth and Planetary Interiors, 153, 3–10.10.1016/j.pepi.2005.03.017Suche in Google Scholar

Canil, D., O’Neill, H.St.C., Pearson, D.G., Rudnick, R.L., McDonough, W.F., and Carswell, D.A. (1994) Ferric iron in peridotites and mantle oxidation states. Earth and Planetary Science Letters, 123, 205–220.10.1016/0012-821X(94)90268-2Suche in Google Scholar

Carmichael, I.S.E. (1991) The redox state of basic and silicic magmas: A reflection of their source regions? Contributions to Mineralogy and Petrology, 106, 129–141.10.1007/BF00306429Suche in Google Scholar

Carmichael, I.S.E., and Ghiorso, M.S. (1990) The effect of oxygen fugacity on the redox state of natural liquids and their crystallizing phases. Reviews in Mineralogy, 24, 191–212.10.1515/9781501508769-011Suche in Google Scholar

Carmichael, I.S.E., Lange, R.A., and Luhr, J.F. (1996) Minettes and related lavas in the Mascota Volcanic Field, Jalisco, Mexico. Contributions to Mineralogy and Petrology 124, 304–323.Suche in Google Scholar

Castellan, G.W. (1971) Physical Chemistry, 2nd ed. Addison-Wesley, Reading, Massachusetts. 866 p.Suche in Google Scholar

Cawthorn, R.G. (1975) Degrees of melting in mantle diapers and the origin of ultrabasic liquids. Earth and Planetary Science Letters, 27, 113–120.10.1016/0012-821X(75)90169-7Suche in Google Scholar

Consolmagno, G.J., and Schaefer, M.W. (1994) Worlds apart: A textbook in planetary sciences. Prentice Hall, Englewood Cliffs, New Jersey, 323 p.Suche in Google Scholar

Cottrell, E., and Kelley, K.A. (2011) The oxidation state of Fe in MORB glasses and the oxygen fugacity of the upper mantle. Earth and Planetary Science Letters, 305, 270–282.10.1016/j.epsl.2011.03.014Suche in Google Scholar

DaSilva, C.R.S., Wentzcovitch, R.M., Patel, A., Price, G.D., and Karato, S.I. (2000) The composition and geotherm of the lower mantle: Constraints from the elasticity of silicate perovskite. Physics of Earth and Planetary Materials, 188, 103–109.10.1016/S0031-9201(99)00133-8Suche in Google Scholar

Davies, G.F. (1988) Ocean bathymetry and mantle convection 1. Large-scale flow and hotspots. Journal of Geophysical Research, 93, 10467–10480.10.1029/JB093iB09p10467Suche in Google Scholar

Davies, G.F. (2009) Reconciling the geophysical and geochemical mantles: Plume flows, heterogeneities, and disequilibrium. Geochemistry, Geophysics, Geosystems, doi: 10.1029/2009GC002634.10.1029/2009GC002634Suche in Google Scholar

Delano, J.W. (1986) Pristine lunar glasses: Criteria, data and implications. Lunar and Planetary Science Conference Proceedings, 17, D201–213.10.1029/JB091iB04p0D201Suche in Google Scholar

Deschamps, F., and Trampert, J. (2004) Towards a lower mantle reference temperature and composition. Earth and Planetary Science Letters, 222, 161–175.10.1016/j.epsl.2004.02.024Suche in Google Scholar

Ding, S.D., and Dasgupta, R.D. (2015) Solidus of martian mantle constrained by new high pressure-temperature experiments at nominally anhydrous conditions. 46th Lunar and Planetary Science Conference, contribution no. 1832, 2079.Suche in Google Scholar

Eugster, H.P., and Wones, D.R. (1962) Stability relation of the ferruginous biotite, annite. Journal of Petrology, 3, 82–125.10.1093/petrology/3.1.82Suche in Google Scholar

Fegley, B. Jr. (2013) Practical chemical thermodynamics for geoscientists. Academic Press, New York.Suche in Google Scholar

Feldstein, S.N., and Lange, R.A. (1999) Pliocene potassic magmas from the Kings River region, Sierra Nevada, California: Evidence for melting of a subduction-modified mantle. Journal of Petrology, 40, 1301–1320.10.1093/petroj/40.8.1301Suche in Google Scholar

Filberto, J., and Dasgupta, R. (2011) Fe2+-Mg partitioning between olivine and basaltic melts: applications to genesis of olivine-phyric shergottites and conditions of melting in the martian interior. Earth and Planetary Science Letters, 304, 527–537.10.1016/j.epsl.2011.02.029Suche in Google Scholar

Filberto, J., and Dasgupta, R. (2015) Constraints on the depth and thermal vigor of melting in the martian mantle. Journal of Geophysical Research: Planets, DOI: 10.1002/2014JE004745.10.1002/2014JE004745Suche in Google Scholar

Filberto, J., Treiman, A.H., and Le, L. (2008) Crystallization experiments on a Gusev Adirondack basalt composition. Meteoritics and Planetary Science, 43, 1137–1146.10.1111/j.1945-5100.2008.tb01118.xSuche in Google Scholar

Fiquet, G., Auzende, A.L., Siebert, J., Corgne, A., Bureau, H., Ozawa, H., and Barbarino, G. (2010) Melting of peridotite to 140 GPa. Science, 329, 1516–1518.10.1126/science.1192448Suche in Google Scholar

Frost, D.J., and McCammon, C.A. (2008) The redox state of Earth’s mantle. Annual Reviews in Earth and Planetary Science, 36, 389–420.10.1146/annurev.earth.36.031207.124322Suche in Google Scholar

Gaillard, F., Scaillet, B., Pichavant, M., and Bény, J.-M. (2001) The effect of water and on the ferric-ferrous ratio of silicic melts. Chemical Geology, 174, 255–273.10.1016/S0009-2541(00)00319-3Suche in Google Scholar

Galton, F. (1886) Regression towards mediocrity in hereditary stature. The Journal of the Anthropological Institute of Great Britain and Ireland, 15, 246–263.10.2307/2841583Suche in Google Scholar

Ganguly, J. (2005) Adiabatic decompression and melting of mantle rocks: An irreversible thermodynamic analysis. Geophysical Research Letters, 32, L06312, doi: 10.1029/2005GL022363.10.1029/2005GL022363Suche in Google Scholar

Garcia, M.O., Hulsebosch, T.P., and Rhodes, J.M. (1995) Olivine-rich submarine basalts form the southwest Rift Zone of Mauna Loa Volcano: Implications for magmatic processes and geochemical evolution. In M.J. Rhodes and J.P. Lockwood, Eds., Mauna Loa Revealed. American Geophysical Union, Washington, D.C., 219–239.Suche in Google Scholar

Gee, L.L., and Sack, R.O. (1988) Experimental petrology of melilite nephelinites. Journal of Petrology 29, 1233–1255.10.1093/petrology/29.6.1233Suche in Google Scholar

Gillet, P., Richet, P., Guyot, F., and Fiquet, G. (1991) High-temperature thermodynamic properties of forsterite. Journal of Geophysical Research, 96, 11805–11816.10.1029/91JB00680Suche in Google Scholar

Goodrich, C.A., Treiman, A.H., Filberto, J., and Jercinovic, M.J. (2010) The Nakhla parent magma: old problems, new approaches. 41st Lunar and Planetary Science Conference, 1387.Suche in Google Scholar

Goodrich, C.A., Treiman, A.H., Filberto, J., Gross, J., and Jercinovic, M.J. (2013) The K2O-rich trapped melt in olivine in the Nakhla meteorite: Implications for petrogenesis of nakhlites and evolution of the martian mantle. Meteoritics and Planetary Science, 48, 2371–2405.10.1111/maps.12226Suche in Google Scholar

Greeley, R., Foing, B.H., McSween, H.Y., Neukum, G., Pinet, P., van Kan, M., Werner, S.C., Williams, D.A., and Zegers, T.E. (2005) Fluid lava flows in Gusev crater, Mars. Journal of Geophysical Research, 110, E05008, doi: 10.1029/2005JE002401.10.1029/2005JE002401Suche in Google Scholar

Green, D.H., Nicholls, I.A., Vilojen, M., and Vilojen, R. (1975) Experimental demonstration of the existence of peridotitic liquids in earliest Archean magmatism. Geology, 3, 11–14.10.1130/0091-7613(1975)3<11:EDOTEO>2.0.CO;2Suche in Google Scholar

Herd, C. (2006) Insights into the redox history of the NWA 1068/1110 martian basalt from mineral equilibria and vanadium oxybarometry. American Mineralogist, 91, 1616–1627.10.2138/am.2006.2104Suche in Google Scholar

Herzberg, C. (1995) Generation of plume magmas through time: An experimental perspective. Chemical Geology, 126, 1–16.10.1016/0009-2541(95)00099-4Suche in Google Scholar

Herzberg, C., and Asimow, P.D. (2008) Petrology of some oceanic island basalts: PRIMELT2.XLS software for primary magma calculation. Geochemistry, Geophysics, Geosystems, doi: 10.1029/2008GC002057.10.1029/2008GC002057Suche in Google Scholar

Herzberg, C., and Asimow, P.D. (2015) PRIMELT3 MEGA.XLSM software for primary magma calculation: Peridotite primary magma MgO contents from the liquidus to the solidus.10.1002/2014GC005631">10.1002/2014GC005631Suche in Google Scholar

Herzberg, C., and Gazel, E. (2009) Petrological evidence for secular cooling in mantle plumes. Nature, 458, 619–623.10.1038/nature07857Suche in Google Scholar

Herzberg, C., and O’Hara, M.J. (1998) Phase equilibrium constraints on the origin of basalts, picrites and komatiites. Earth-Science Reviews 44, 39–79.10.1016/S0012-8252(98)00021-XSuche in Google Scholar

Herzberg, C., and O’Hara, M.J. (2002) Plume-associated ultramafic magmas of Phanerozoic age. Journal of Petrology, 43, 1857–1883.10.1093/petrology/43.10.1857Suche in Google Scholar

Herzberg, C., and Rudnick, R. (2012) Formation of cratonic lithosphere: An integrated thermal and petrological model. Lithos, 149, 4–15.10.1016/j.lithos.2012.01.010Suche in Google Scholar

Herzberg, C., and Zhang, J. (1996) Melting experiments on anhydrous peridotite KLB-1; Composition of magmas in the upper mantle and transition zone. Journal of Geophysical Research, 101, 8271–8295.10.1029/96JB00170Suche in Google Scholar

Herzberg, C., Condie, K., and Korenaga, J. (2010) Thermal history of the Earth and its petrological expression. Earth and Planetary Science Letters, 292, 79–88.10.1016/j.epsl.2010.01.022Suche in Google Scholar

Hess, H. (1962) History of the ocean basins. In A.F. Buddington, A.E. Engle, H.L. James, and B.F. Leonard, Eds., Petrologic Studies: A Volume in Honor A.F. Buddington. The Society, p. 599–620.10.1130/Petrologic.1962.599Suche in Google Scholar

Hewitt, D.A. (1978) A redetermination of the fayalite-magnetite-quartz equilibrium between 650 and 850 °C. American Journal of Science, 278, 715–724.10.2475/ajs.278.5.715Suche in Google Scholar

Hirose, K., and Kawamura, K. (1994) A new experimental approach for incremental batch melting of peridotite at 1.5 GPa. Geophysical Research Letters, 19, 2139–2142.10.1029/94GL01792Suche in Google Scholar

Hirose, K., and Kushiro, I. (1998) The effect of melt segregation on polybaric mantle melting: estimation from the incremental melting experiments. Physics of Earth and Planetary Interiors, 107, 111–118.10.1016/S0031-9201(97)00129-5Suche in Google Scholar

Hirschmann, M.M. (2000) Mantle solidus: Experimental constraints and the effects of peridotite composition. Geochemistry, Geophysics, Geosystems, 1, 2000GC000070.10.1029/2000GC000070Suche in Google Scholar

Hirschmann, M.M., Asimow, P.D., Ghiorso, M.S., and Stolper, E.M. (1999) Calculation of peridotite partial melting from thermodynamic models of minerals and melts III. Controls on isobaric melt production and the effect of water on melt production. Journal of Petrology, 40, 831–851.10.1093/petroj/40.5.831Suche in Google Scholar

Hirschmann, M.M., Ghiorso, M.S., Davis, F.A., Gordon, S.M., Mukherjee, S., Grove, T.L., Krawczynski, M., Medard, E., and Till, C.B. (2008). Library of experimental phase relations (LEPR): A database and web portal for experimental magmatic phase equilibria data. Geochemistry, Geophysics, Geosystems 9, Q03011, doi: 10.1029/2007GC001894.10.1029/2007GC001894Suche in Google Scholar

Hole, M.J. (2015) The generation of continental flood basalts by decompression melting of internally heated mantle. Geology, 43, 311–314.10.1130/G36442.1Suche in Google Scholar

Holland, T.J.B., and Powell, R. (1998) An internally consistent thermodynamic data set for phases of petrological interest. Journal of Metamorphic Geology, 16, 309–343.10.1111/j.1525-1314.1998.00140.xSuche in Google Scholar

Jayasuriya, K., O’Neill, H. St., Berry, A.J., and Campbell, S.J. (2004) A Mössbauer study of the oxidation state of Fe in silicate melts. American Mineralogist, 89, 1597–1609.10.2138/am-2004-11-1203Suche in Google Scholar

Katsura, T., Yoneda, A., Yamazaki, D., Yoshino, T., and Ito, E. (2010) Adiabatic temperature profile in the mantle. Physics of the Earth and Planetary Interiors, 183, 212–218.10.1016/j.pepi.2010.07.001Suche in Google Scholar

Katz, R.F., Spiegelman, M., and Langmuir, C.H. (2003) A new parameterization of hydrous mantle melting. Geochemistry, Geophysics, Geosystems, 4, doi: 10.1029/2002GC000433.10.1029/2002GC000433Suche in Google Scholar

Keiding, J.K., Trumbull, R.B., Veksler, I.V., and Jerram, D.A. (2011) On the significance of ultra-magnesian olivines in basaltic rocks. Geology, 39, 1095–1098.10.1130/G32214.1Suche in Google Scholar

Kelley, K.A., and Cottrell, E. (2012) The influence of magmatic differentiation on the oxidation state of Fe in a basaltic arc magma. Earth and Planetary Science Letters, 329–330, 109–121.10.1016/j.epsl.2012.02.010Suche in Google Scholar

Kilinc, A., Carmichael, I.S.E., Rivers, M.L., and Sack, R.O. (1983) The ferric-ferrous ratio of natural silicate liquids equilibrated in air. Contributions to Mineralogy and Petrology, 83, 136–140.10.1007/BF00373086Suche in Google Scholar

Kojitani, H., and Akaogi, M. (1997) Melting enthalpies of mantle peridotite: Calorimetric determinations in the system CaO-MgO-Al2O3-SiO2 and application to magma generation. Earth and Planetary Science Letters, 153, 209–222.10.1016/S0012-821X(97)00186-6Suche in Google Scholar

Korenaga, J. (2005) Firm mantle plumes and the nature of the core-mantle boundary region. Earth and Planetary Science Letters, 232, 29–37.10.1016/j.epsl.2005.01.016Suche in Google Scholar

Korenaga, J. (2008) Urey ratio and the structure and evolution of Earth’s mantle. Reviews in Geophysics, 46, 1–32, article no. 2007RG000241.10.1029/2007RG000241Suche in Google Scholar

Kress, V.C., and Carmichael, I.S.E. (1988) Stoichiometry of the iron oxidation reaction in silicate melts. American Mineralogist, 73, 1267–1274.Suche in Google Scholar

Kress, V.C., and Carmichael, I.S.E. (1991) The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity, and pressure on their redox states. Contributions to Mineralogy and Petrology, 108, 82–92.10.1007/BF00307328Suche in Google Scholar

Lange, R.L., and Carmichael, I.S.E. (1990) Thermodynamic properties of silicate liquids with emphasis on density, thermal expansion and compressibility. Reviews in Mineralogy 24, 25–64.10.1515/9781501508769-006Suche in Google Scholar

Lange, R.A., Carmichael, I.S.E., and Renne, P.R. (1993) Potassic volcanism near Mono basin, California: Evidence for high water and oxygen fugacities inherited from subduction. Geology, 21, 949–952.10.1130/0091-7613(1993)021<0949:PVNMBC>2.3.CO;2Suche in Google Scholar

Lee, C-T., and Chin, E.J. (2014) Calculating melting temperatures and pressure of peridotite protoliths: Implications for the origin of cratonic mantle. Earth and Planetary Science Letters, 403, 273–286.10.1016/j.epsl.2014.06.048Suche in Google Scholar

Lee, C-T., Luffi, P., Plank, T., Dalton, H., and Leeman, W.P. (2009) Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets, using new thermobarometers for mafic magmas. Earth and Planetary Science Letters, 279, 20–33.10.1016/j.epsl.2008.12.020Suche in Google Scholar

Longhi, J., and Pan, V. (1989) The parent magmas of the SNC meteorites. Proceedings of the 19th Lunar and Planetary Science Conference, 451–464.Suche in Google Scholar

Luhr, J.F., Allan, J.F., Carmichael, I.S.E., Nelson, S.A., and Hasenaka, T. (1989) Primitive calc-alkaline and alkaline rock types from the western Mexican Volcanic Belt. Journal of Geophysical Research, 94, 4515–4530.10.1029/JB094iB04p04515Suche in Google Scholar

Mandler, B.E., and Elkins-Tanton, L.T. (2013) The origin of eucrites, diogenites, and olivine diogenites: Magma ocean crystallization and shallow magma chamber processes on Vesta. Meteoritics and Planetary Science, 48, 2333–2349.10.1111/maps.12135Suche in Google Scholar

Mattern, E., Matas, J., Ricard, Y., and Bass, J. (2005) Lower mantle composition and temperature from mineral physics and thermodynamic modeling. Geophysical Journal International, 160, 973–990.10.1111/j.1365-246X.2004.02549.xSuche in Google Scholar

Matzen, A.K., Baker, M.B., Beckett, J.R., and Stolper, E.M. (2011) Fe-Mg partitioning between olivine and high-magnesian melts and the nature of Hawaiian parental liquids. Journal of Petrology, doi: 10.1093/petrology/egq089.10.1093/petrology/egq089Suche in Google Scholar

McCallum, I.S., and Schwartz, J.M. (2001) Lunar Mg suite: Thermobarometry and petrogenesis of parental magmas. Journal of Geophysical Research, 106, 27969–27983.10.1029/2000JE001397Suche in Google Scholar

McKenzie, D.P. (1967) Some remarks on heat flow and gravity anomalies. Journal of Geophysical Research, 72, 6261–6273.10.1002/9781118782149.ch3Suche in Google Scholar

McKenzie, D.P., and Bickle, M.J. (1988) The volume and composition of melt generated by extension of the lithosphere. Journal of Petrology, 29, 625–679.10.1093/petrology/29.3.625Suche in Google Scholar

Miller, G.H., Stolper, E.M., and Ahrens, T.J. (1991) The equation of state of a molten komatiite: 2. Application to komatiite petrogenesis and the Hadean mantle. Journal of Geophysical Research, 96, 11849–11864.10.1029/91JB01203Suche in Google Scholar

Monders, A.G., Médard, E., and Grove, T.L. (2007) Phase equilibrium investigations of the Adirondak class basalts from the Gusev plains, Gusev crater, Mars. Meteoritics and Planetary Science, 42, 131–148.10.1111/j.1945-5100.2007.tb00222.xSuche in Google Scholar

Moore, G., Righter, K., and Carmichael, I.S.E. (1995) The effect of dissolved water on the oxidation state of iron in natural silicate liquids. Contributions to Mineralogy and Petrology, 120, 170–179.10.1007/BF00287114Suche in Google Scholar

Morgan, W.J. (1971) Convection plumes in the lower mantle. Nature, 230, 42–43.10.1038/230042a0Suche in Google Scholar

Musselwhite, D.S., Dalton, H.A., Kiefer, W.S., and Treiman, A.H. (2006) Experimental petrology of the basaltic shergottite Yamato-980459: Implications for the thermal structure of the martian mantle. Meteoritics and Planetary Science, 41, 1271–1290.10.1111/j.1945-5100.2006.tb00521.xSuche in Google Scholar

Myers, J., and Eugster, H.P. (1983) The system Fe-Si-O: Oxygen buffer calibrations to 1500 K. Contributions to Mineralogy and Petrology, 82, 75–90.10.1007/BF00371177Suche in Google Scholar

Mysen, B.O. (1991) Relations between structure, redox equilibria of iron, and properties of magmatic liquids. In L.L. Perchuk and I. Kushiro, Eds., Physical Chemistry of Magmas. Springer-Verlag, New York, 41–98.10.1007/978-1-4612-3128-8_2Suche in Google Scholar

Nakagawa, T., and Tackley, P.J. (2010) Influence of initial CMB temperature and other parameters on the thermal evolution of Earth’s core resulting from thermochemical and spherical mantle convection. Geochemistry, Geophysics, Geosystems, 11, DOI: 10.1029/2010GC003031.10.1029/2010GC003031Suche in Google Scholar

Nakagawa, T., and Tackley, P.J. (2012) Influence of magmatism on mantle cooling, surface heat flow and Urey ratio. Earth and Planetary Science Letters, 329–330, 1–10.10.1016/j.epsl.2012.02.011Suche in Google Scholar

Nakagawa, T., and Tackley, P.J. (2014) Influence of combined primordial layering and recycled MORB on the coupled thermal evolution of Earth’s mantle and core. Geochemistry, Geophysics, Geosystems, DOI: 10.1002/2013GC005128.10.1002/2013GC005128Suche in Google Scholar

Navrotsky, A., Ziegler, D., Oestrike, R., and Maniar, P. (1989) Calorimetry of silicate melts at 1773 K: Measurement of enthalpies of fusion and of mixing I the systems diopside-anorthite-albite and anorthite-forsterite. Contributions to Mineralogy and Petrology, 101, 122–130.10.1007/BF00387206Suche in Google Scholar

Nisbet, E.G., Cheadle, M.J., Arndt, N.T., and Bickle, M.J. (1993) Constraining the potential temperature of the Archean mantle; A review of the evidence from komatiites. Lithos, 30, 291–307.10.1016/0024-4937(93)90042-BSuche in Google Scholar

Nomura, R., Hirose, K., Usegui, K., Ohishi, Y., Tsuchiyama, A., Miyake, A., and Ueno, Y. (2014) Low core-mantle boundary temperature inferred from the solidus of pyrolite. Science, 343, 522–525.10.1126/science.1248186Suche in Google Scholar PubMed

O’Neill, C., and Debaille, V. (2014) The evolution of Hadean-Eoarchean geodynamics. Earth and Planetary Science Letters, 406, 49–58.10.1016/j.epsl.2014.08.034Suche in Google Scholar

O’Rourke, J.G., and Korenaga, J. (2012) Terrestrial planet evolution in the stagnant-lid regime: size effects and the formation of self-destabilizing crust. Icarus, 221, 1043–1060.10.1016/j.icarus.2012.10.015Suche in Google Scholar

Papuc, A.M., and Davies, G.F. (2008) The internal activity and thermal evolution of Earth-like planets. Icarus, 195, 447–458.10.1016/j.icarus.2007.12.016Suche in Google Scholar

Parman, S.W., Dann, J.C., Grove, T.L., and deWit, M.J. (1997) Emplacement conditions of komatiite magmas from the 3.49 Ga Komati Formation, Barberton Greenstone Belt, South Africa. Earth and Planetary Science Letters, 150, 303–323.10.1016/S0012-821X(97)00104-0Suche in Google Scholar

Pickering-Witter, J., and Johnston, A.D. (2000) The effects of variable bulk composition on the melting systematics of fertile peridotitic assemblages. Contributions to Mineralogy and Petrology, 140, 190–211.10.1007/s004100000183Suche in Google Scholar

Putirka, K.D. (2005). Mantle potential temperatures at Hawaii, Iceland, and the mid-ocean ridge system, as inferred from olivine phenocrysts: Evidence for thermally driven mantle plumes. Geochemistry, Geophysics, Geosystems, 6, doi: 10.1029/005GC000915.10.1029/2005GC000915Suche in Google Scholar

Putirka, K.D. (2008a) Thermometers and barometers for volcanic systems. Reviews in Mineralogy and Geochemistry 69, 61–120.10.1515/9781501508486-004Suche in Google Scholar

Putirka, K.D. (2008b) Excess temperatures at ocean islands: Implications for mantle layering and convection. Geology, 36, 283–286.10.1130/G24615A.1Suche in Google Scholar

Putirka, K.D., Perfit, M., Ryerson, F.J., and Jackson, M.G. (2007) Ambient and excess mantle temperatures, olivine thermometry, and active vs. passive upwelling. Chemical Geology, 241, 177–206.10.1016/j.chemgeo.2007.01.014Suche in Google Scholar

Putirka, K.D., Ryerson, F.J., Perfit, M., and Ridley, W.I. (2011) Mineralogy and composition of the oceanic mantle. Journal of Petrology, 52, 279–313.10.1093/petrology/egq080Suche in Google Scholar

Ramburg, H. (1971) Temperature changes associated with adiabatic decompression in geological processes. Nature, 234, 539–540.10.1038/234539a0Suche in Google Scholar

Rhodes, J.M., and Vollinger, M.J. (2004) Composition of basaltic lavas sampled by phase-2 of the Hawaii Scientific Drilling Project: Geochemical stratigraphy and magma types. Geochemistry, Geophysics, Geosystems, 5, doi: 10.1029/2002GC000434.10.1029/2002GC000434Suche in Google Scholar

Rhodes, J.M., and Vollinger, M.J. (2005) Ferric/ferrous ratios in 1984 Mauna Loa lavas: A contribution to understanding the oxidation state of Hawaiian magmas. Contributions to Mineralogy and Petrology, 149, 666–674.10.1007/s00410-005-0662-ySuche in Google Scholar

Richet, P., and Bottinga, Y. (1986) Thermochemical properties of silicate glasses and liquids: A review. Reviews in Geophysics, 24, 1–25.10.1029/RG024i001p00001Suche in Google Scholar

Richet, P., Leclerc, F., and Benoist, L. (1993) Melting of forsterite and spinel, with implications for the glass transition of Mg2SiO4 liquid. Geophysical Research Letters, 20, 1675–1678.10.1029/93GL01836Suche in Google Scholar

Righter, K., Yang, H., Costin, G., and Downs, R.T. (2008) Oxygen fugacity in the martian mantle controlled by carbon: new constraints from the Nakhlite MIL 03346. Meteoritics and Planetary Sciences, 43, 1709–1723.10.1111/j.1945-5100.2008.tb00638.xSuche in Google Scholar

Robie, R.A., and Hemingway, B.S. (1995) Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (108 Pascals) pressure and at higher temperatures. U.S. Geological Survey Bulletin 2131, U.S. Government Printing Office, Washington, D.C.Suche in Google Scholar

Robin-Popieul, C.C.M., Arndt, N.T., Chauvel, C., Byerly, G.R., Sobolev, A.V., and Wilson, A. (2012) A new model for Barberton Komatiites: Deep critical melting with high melt retention. Journal of Petrology, 53, 2191–2229.10.1093/petrology/egs042Suche in Google Scholar

Robinson, J.A.C., Wood, B.J., and Blundy, J.D. (1998) The beginning of melting of fertile and depleted peridotite at 1.5 GPa. Earth and Planetary Science Letters, 155, 97–111.10.1016/S0012-821X(97)00162-3Suche in Google Scholar

Roeder, P.L., and Emslie, R.F. (1970) Olivine-liquid equilibrium. Contributions to Mineralogy and Petrology, 29, 275–289.10.1007/BF00371276Suche in Google Scholar

Sack, R.O., Carmichael, I.S.E., Rivers, M., and Ghiorso, M.S. (1980) Ferric-ferrous equilibria in natural silicate liquids at 1 bar. Contributions to Mineralogy and Petrology, 75, 369–376.10.1007/BF00374720Suche in Google Scholar

Saunders, P.M. (1957) The thermodynamics of saturated air: A contribution to the classical theory. Quarterly Journal of the Royal Meteorological Society, 83, 342–350.10.1002/qj.49708335707Suche in Google Scholar

Schmidt, B.C., and Behrens, H. (2008) Water solubility in phonolite melts: Influence of melt composition and temperature. Chemical Geology, 256, 259–268.10.1016/j.chemgeo.2008.06.043Suche in Google Scholar

Schuessler, J.A., Botcharnikov, R.E., Behrens, H., Misiti, V., and Freda, C. (2008) Oxidation state of iron in hydrous phono-tephritic melts. American Mineralogist, 93, 1493–1504.10.2138/am.2008.2795Suche in Google Scholar

Schwab, R.O., and Küstner, D. (1981) Die Gleichgewichtsfugazitäten technologisch und petrologisch wichtiger Sauerstoffpuffer. Neues Jahrbuch für Mineralogie Abhandlungen, 140, 111–142.Suche in Google Scholar

Shirey, S.B., Kamber, B.S., Whitehouse, M.J., Mueller, P.A., and Basu, A.R. (2008) A review of the isotopic and trace element evidence for mantle and crustal processes in the Hadean and Archean: Implications for the onset of plate tectonic subduction. In K.C. Condie and V. Pease, Eds., When Did Plate Tectonics Begin on Planet Earth? GSA Special Paper 440, 1–29.10.1130/2008.2440(01)Suche in Google Scholar

Silver, P.G., and Behn, M.D. (2008) Intermittent plate tectonics. Science, 319, 85–88.10.1126/science.1148397Suche in Google Scholar

Sobolev, A.V., Hofmann, A.W., Kuzmin, D.V., Yaxley, G.M., Arndt, N.T., Chung, S.-L., Danyushevsky, L.V., Elliott, T., Frey, F.A., Garcia, M.O., Gurenko, A.A., Kamenetsky, V.S., Kerr, A.C., Krivolutskaya, N.A., Matvienkov, V.V., Nikogosian, I.K., Rocholl, A., Sigurdsson, I.A., Sushchevskaya, N.M., and Teklay, M. (2007) The amount of recycled crust in source of mantle-derived melts. Nature, 316, 412–417.Suche in Google Scholar

Stebbins, J.F., Carmichael, I.S.E., and Moret, L.K. (1984) Heat capacities and entropies of silicate liquids and glasses. Contributions to Mineralogy and Petrology, 86, 131–148.10.1007/BF00381840Suche in Google Scholar

Stevenson, D.J. (2003) Styles of mantle convection and their influence on planetary evolution. Comptes Rendus Geoscience, 335, 99–111.10.1016/S1631-0713(03)00009-9Suche in Google Scholar

Stolper, E. (1980) A phase diagram for mid-ocean ridge basalts: Preliminary results and implications for petrogenesis. Contributions to Mineralogy and Petrology, 74, 13–27.10.1007/BF00375485Suche in Google Scholar

Takahashi, E., Shimazaki, T., Tsuzaki, Y., and Yoshida, H. (1993) Melting study of a peridotite KLB-1 to 6.5 GPa, and the origin of basaltic magmas. Philosophical Transactions of the Royal Society of London, 342, 105–120.10.1098/rsta.1993.0008Suche in Google Scholar

Thieblot, L., Tequi, C., and Richet, P. (1999) High-temperature heat capacity of grossular (Ca3Al2Si3O12), enstatite (MgSiO3), and titanite (CaTiSiO5). American Mineralogist, 84, 848–855.10.2138/am-1999-5-618Suche in Google Scholar

Tirone, M. (2015) On the thermal gradient in the Earth’s deep interior. Solid Earth, 7, 2501–2525.10.5194/se-7-229-2016Suche in Google Scholar

Toplis, M.J. (2005) The thermodynamics of iron and magnesium partitioning between olivine and liquid: Criteria for assessing and predicting equilibrium in natural and experimental systems. Contributions to Mineralogy and Petrology, 149, 22–39.10.1007/s00410-004-0629-4Suche in Google Scholar

Treiman, A.H. (1986) The parental magmas of the nakhla achondrite meteorite: ultrabasic volcanism on the shergottite parent body. Geochimica et Cosmochimica Acta, 50, 1061–1070.10.1016/0016-7037(86)90388-1Suche in Google Scholar

Treiman, A.H. (1993) The parent magma of the Nakhla (SNC) meteorite, inferred from magmatic inclusions. Geochimica et Cosmochimica Acta, 57, 4753–4767.10.1016/0016-7037(93)90198-6Suche in Google Scholar

Treiman, A.H. (1997) The parent magmas of the cumulate eucrites: A mass balance approach. Meteoritics and Planetary Science, 32, 217–230.10.1111/j.1945-5100.1997.tb01261.xSuche in Google Scholar

Turcotte, D.L., and Oxburgh, E.R. (1972) Mantle convection and the new global tectonics. Annual Reviews in Fluid Mechanics, 4, 33–66.10.1146/annurev.fl.04.010172.000341Suche in Google Scholar

Wadhwa, M. (2008) Redox conditions on small bodies, the Moon and Mars. Reviews in Mineralogy and Geochemistry, 68, 493–510.10.1515/9781501508509-017Suche in Google Scholar

Wallace, P., and Carmichael, I.S.E. (1989) Minette lavas and associated leucitites from the western front of the Mexican Volcanic Belt: Petrology, chemistry and origin. Contributions to Mineralogy and Petrology, 103, 470–492.10.1007/BF01041754Suche in Google Scholar

Walter, M.J. (1998) Melting of garnet peridotite and the origin of komatiite and depleted lithosphere. Journal of Petrology, 39, 29–60.10.1093/petroj/39.1.29Suche in Google Scholar

Werner, S.C., Ody, A., and Poulet, F. (2014) The source crater of martian shergottite meteorites. Science, 343, 1343–1346.10.1126/science.1247282Suche in Google Scholar PubMed

Wilke, M., Behrens, H. Burkhard, D.J.M., and Rossano, S. (2002) The oxidation state of iron in silicic melt at 500 MPa water pressure. Chemical Geology, 189, 55–67.10.1016/S0009-2541(02)00042-6Suche in Google Scholar

Zerr, A., Diegeler, A., and Boehler, R. (1998) Solidus of Earth’s Deep Mantle. Science, 281, 243–246.10.1126/science.281.5374.243Suche in Google Scholar PubMed

Received: 2015-3-1
Accepted: 2015-11-27
Published Online: 2016-4-5
Published in Print: 2016-4-1

© 2016 by Walter de Gruyter Berlin/Boston

Artikel in diesem Heft

  1. Research Article
  2. Glass structure, melt structure, and dynamics: Some concepts for petrology
  3. Research Article
  4. The validity of plagioclase-melt geothermometry for degassing-driven magma crystallization
  5. Research Article
  6. Outlooks in Earth and Planetary Materials: Chemistry and Mineralogy of Earth’s Mantle: A petrological assessment of diamond as a recorder of the mantle nitrogen cycle
  7. Research Article
  8. Special Collection: Advances in Ultrahigh-Pressure Metamorphism: Contrasting P-T paths within the Barchi-Kol UHP terrain (Kokchetav Complex): Implications for subduction and exhumation of continental crust
  9. Research Article
  10. Special Collection: New Advances in Subduction Zone Magma Genesis: Experimental formation of pyroxenite veins by reactions between olivine and Si, Al, Ca, Na, and Cl-rich fluids at 800 °C and 800 MPa: Implications for fluid metasomatism in the mantle wedge
  11. Review
  12. Special Collection: Olivine: Rates and styles of planetary cooling on Earth, Moon, Mars, and Vesta, using new models for oxygen fugacity, ferric-ferrous ratios, olivine-liquid Fe-Mg exchange, and mantle potential temperature
  13. Research Article
  14. Special Collection: Rates and Depths of Magma Ascent on Earth: Amphibole thermometers and barometers for igneous systems and some implications for eruption mechanisms of felsic magmas at arc volcanoes
  15. Research Article
  16. Special Collection: Rates and Depths of Magma Ascent on Earth: Degassing of Hydrous Trachytic Campi Flegrei and Phonolitic Vesuvius Melts: Experimental Limitations and Chances to Study Homogeneous Bubble Nucleation
  17. Research Article
  18. Special Collection: Water in Nominally Hydrous and Anhydrous Minerals: Crystal/melt partitioning of water and other volatiles during the near-solidus melting of mantle peridotite: Comparisons with non-volatile incompatible elements and implications for the generation of intraplate magmatism
  19. Research Article
  20. Carbon mineral ecology: Predicting the undiscovered minerals of carbon
  21. Research Article
  22. Chromium, vanadium, and titanium valence systematics in Solar System pyroxene as a recorder of oxygen fugacity, planetary provenance, and processes
  23. Research Article
  24. Iron-titanium oxyhydroxides as water carriers in the Earth’s deep mantle
  25. Research Article
  26. Radiation damage in biotite mica by accelerated α-particles: A synchrotron microfocus X-ray diffraction and X-ray absorption spectroscopy study
  27. Research Article
  28. Models for the estimation of Fe3+/Fetot ratio in terrestrial and extraterrestrial alkali- and iron-rich silicate glasses using Raman spectroscopy
  29. Research Article
  30. An advanced rotational rheometer system for extremely fluid liquids up to 1273 K and applications to alkali carbonate melts
  31. Research Article
  32. Experimental temperature cycling as a powerful tool to enlarge melt pools and crystals at magma storage conditions
  33. Research Article
  34. Exploring the potential of Raman spectroscopy for crystallochemical analyses of complex hydrous silicates: II. Tourmalines
  35. Research Article
  36. Crystal structure of a new compound, CuZnCl(OH)3, isostructural with botallackite
  37. Research Article
  38. Elastic wave velocities in polycrystalline Mg3Al2Si3O12-pyrope garnet to 24 GPa and 1300 K
  39. Research Article
  40. Presentation of the Mineralogical Society of America Award for 2015 to Nicholas J. Tosca
  41. Research Article
  42. Acceptance of the Mineralogical Society of America Award for 2015
  43. Research Article
  44. Presentation of the 2015 Roebling Medal of the Mineralogical Society of America to Rodney C. Ewing
  45. Research Article
  46. Acceptance of the 2015 Roebling Medal of the Mineralogical Society of America
  47. Research Article
  48. Presentation of the Distinguished Public Service Award of the Mineralogical Society of America for 2015 to J. Alexander Speer
  49. Research Article
  50. Acceptance of the 2015 Mineralogical Society of America Distinguished Public Service Award
  51. Research Article
  52. Presentation of the Dana Medal of the Mineralogical Society of America for 2016 to Patrick Cordier
  53. Research Article
  54. Acceptance of the Dana Medal of the Mineralogical Society of America for 2016
  55. Book Review
  56. New Mineral Names*†
  57. Book Review
  58. Book Review
https://doi.org/10.2138/am-2016-5402
Schlagwörter für diesen Artikel
Potential temperature; Mars; Vesta; Moon; secular cooling; mantle plumes; Archean, tectonics

Artikel in diesem Heft

  1. Research Article
  2. Glass structure, melt structure, and dynamics: Some concepts for petrology
  3. Research Article
  4. The validity of plagioclase-melt geothermometry for degassing-driven magma crystallization
  5. Research Article
  6. Outlooks in Earth and Planetary Materials: Chemistry and Mineralogy of Earth’s Mantle: A petrological assessment of diamond as a recorder of the mantle nitrogen cycle
  7. Research Article
  8. Special Collection: Advances in Ultrahigh-Pressure Metamorphism: Contrasting P-T paths within the Barchi-Kol UHP terrain (Kokchetav Complex): Implications for subduction and exhumation of continental crust
  9. Research Article
  10. Special Collection: New Advances in Subduction Zone Magma Genesis: Experimental formation of pyroxenite veins by reactions between olivine and Si, Al, Ca, Na, and Cl-rich fluids at 800 °C and 800 MPa: Implications for fluid metasomatism in the mantle wedge
  11. Review
  12. Special Collection: Olivine: Rates and styles of planetary cooling on Earth, Moon, Mars, and Vesta, using new models for oxygen fugacity, ferric-ferrous ratios, olivine-liquid Fe-Mg exchange, and mantle potential temperature
  13. Research Article
  14. Special Collection: Rates and Depths of Magma Ascent on Earth: Amphibole thermometers and barometers for igneous systems and some implications for eruption mechanisms of felsic magmas at arc volcanoes
  15. Research Article
  16. Special Collection: Rates and Depths of Magma Ascent on Earth: Degassing of Hydrous Trachytic Campi Flegrei and Phonolitic Vesuvius Melts: Experimental Limitations and Chances to Study Homogeneous Bubble Nucleation
  17. Research Article
  18. Special Collection: Water in Nominally Hydrous and Anhydrous Minerals: Crystal/melt partitioning of water and other volatiles during the near-solidus melting of mantle peridotite: Comparisons with non-volatile incompatible elements and implications for the generation of intraplate magmatism
  19. Research Article
  20. Carbon mineral ecology: Predicting the undiscovered minerals of carbon
  21. Research Article
  22. Chromium, vanadium, and titanium valence systematics in Solar System pyroxene as a recorder of oxygen fugacity, planetary provenance, and processes
  23. Research Article
  24. Iron-titanium oxyhydroxides as water carriers in the Earth’s deep mantle
  25. Research Article
  26. Radiation damage in biotite mica by accelerated α-particles: A synchrotron microfocus X-ray diffraction and X-ray absorption spectroscopy study
  27. Research Article
  28. Models for the estimation of Fe3+/Fetot ratio in terrestrial and extraterrestrial alkali- and iron-rich silicate glasses using Raman spectroscopy
  29. Research Article
  30. An advanced rotational rheometer system for extremely fluid liquids up to 1273 K and applications to alkali carbonate melts
  31. Research Article
  32. Experimental temperature cycling as a powerful tool to enlarge melt pools and crystals at magma storage conditions
  33. Research Article
  34. Exploring the potential of Raman spectroscopy for crystallochemical analyses of complex hydrous silicates: II. Tourmalines
  35. Research Article
  36. Crystal structure of a new compound, CuZnCl(OH)3, isostructural with botallackite
  37. Research Article
  38. Elastic wave velocities in polycrystalline Mg3Al2Si3O12-pyrope garnet to 24 GPa and 1300 K
  39. Research Article
  40. Presentation of the Mineralogical Society of America Award for 2015 to Nicholas J. Tosca
  41. Research Article
  42. Acceptance of the Mineralogical Society of America Award for 2015
  43. Research Article
  44. Presentation of the 2015 Roebling Medal of the Mineralogical Society of America to Rodney C. Ewing
  45. Research Article
  46. Acceptance of the 2015 Roebling Medal of the Mineralogical Society of America
  47. Research Article
  48. Presentation of the Distinguished Public Service Award of the Mineralogical Society of America for 2015 to J. Alexander Speer
  49. Research Article
  50. Acceptance of the 2015 Mineralogical Society of America Distinguished Public Service Award
  51. Research Article
  52. Presentation of the Dana Medal of the Mineralogical Society of America for 2016 to Patrick Cordier
  53. Research Article
  54. Acceptance of the Dana Medal of the Mineralogical Society of America for 2016
  55. Book Review
  56. New Mineral Names*†
  57. Book Review
  58. Book Review
Jetzt anmelden und 20% sparen
Institutioneller Zugang
Wie funktioniert Authentifizierung?
Haben Sie eine Idee, wie wir unsere Website verbessern können?
Bitte schreiben Sie uns.
© 2025 De Gruyter Brill
Heruntergeladen am 23.9.2025 von https://www.degruyterbrill.com/document/doi/10.2138/am-2016-5402/html
Button zum nach oben scrollen