Читать книгу Magma Redox Geochemistry - Группа авторов - Страница 34

REFERENCES

Оглавление

1 Allende Prieto, C., Lambert, D. L., & Asplund, M. (2002). A reappraisal of the solar photospheric C/O ratio. Astrophysical Journal Letters, 573, L137–L140. https://doi.org/10.1086/342095

2 Andrault, D., Muñoz, M., Pesce, G., Cerantola, V., Chumakov, A., Kantor, I., et al. (2018). Large oxygen excess in the primitive mantle could be the source of the Great Oxygenation Event. Geochemical Perspectives Letters, 6, 5–10. doi: 10.7185/geochemlet.1801

3 Armstrong, K., Frost, D. J., McCammon, C. A., Rubie, D. C, & Boffa Ballaran, T. (2019). Deep magma ocean formation set the oxidation state of Earth's mantle. Science, 365, 6456, 903–906. doi: 10.1126/science.aax8376

4 Aulbach S., & Stagno V. (2016). Evidence for a reducing Archean ambient mantle and its effects on the carbon cycle. Geology, 44, 9, 751–754. https://doi.org/10.1130/G38070.1

5 Aulbach, S., & Viljoen, K. S. (2015) Eclogite xenoliths from the Lace kimberlite, Kaapvaal craton: From convecting mantle source to palaeo‐ocean floor and back. Earth and Planetary Science Letters, 431, 274–286. https://doi.org/10.1016/j.epsl.2015.08.039

6 Aulbach, S., Woodland, A. B., Vasilyev, P., Galvez, M. E., & Viljoen, K. S. (2017). Effects of low‐pressure igneous processes and subduction on Fe3+/∑Fe and redox state of mantle eclogites from Lace (Kaapvaal craton). Earth and Planetary Science Letters, 474, 283–295. https://doi.org/10.1016/j.epsl.2017.06.030

7 Aulbach, S., Woodland, A. B., Stern, R. A., Vasilyev, P., Heaman, L. M. & Viljoen, K. S. (2019). Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust. Scientific Reports 9.

8 Ballhaus, C., Frost, B. R. (1994), The generation of oxidised CO2‐bearing basaltic melts from reduced CH4‐bearing upper mantle sources. Geochimica et Cosmochimica Acta, 58, 4431–4440. https://doi.org/10.1016/0016‐7037(94)90222‐4

9 Berry, A. J., Stewart, G. A., O’Neill, H. S., Mallmann, G. F., & Mosselmans, J. F. (2018). A re‐assessment of the oxidation state of iron in MORB glasses. Earth and Planetary Science Letters, 483, 114–123. https://doi.org/10.1016/j.epsl.2017.11.032

10 Bickle, M. J., Nisbet, E. G., & Martin, A. (1994). Archaean greenstone belts are not oceanic crust? Journal of Geology, 102, 121–138.

11 Bouvier, A., & Wadhwa, M. (2010) The age of the Solar System redefined by the oldest Pb–Pb age of a meteoritic inclusion. Nature Geoscience, 3, 637–641. https://doi.org/10.1038/ngeo941

12 Brenker, F. E., Vollmer, C., Vincze, S., Vekemans, B., Szymanski, A., Janssens, K., et al. (2007). Carbonates from lower part of transition zone or even the lower mantle. Earth and Planetary Science Letters, 260, 1–9. https://doi.org/10.1016/j.epsl.2007.02.038

13 Brett, R., & Sato, M. (1984). Intrinsic oxygen fugacity measurements on 7 chondrites, a pallasite and a tektite and the redox state of the meteorite parent bodies. Geochimica et Cosmochimica Acta, 48, 111–120. https://doi.org/10.1016/0016‐7037(84)90353‐3

14 Brune, S., Williams, S. E., & Müller, R. D. (2017). Potential links between continental rifting, CO2 degassing and climate change through time. Nature Geoscience, 10, 941–946. doi: http://doi.org/10.1038/s41561‐017‐0003‐6

15 Canil, D. (1997). Vanadium partitioning and the oxidation state of Archaean komatiite magmas. Nature, 389, 842–845, doi:10.1038 /39860

16 Canil, D., & Scarfe, C. M. (1990). Phase relations in peridotite+CO2 Systems to 12 GPa: Implications for the origin of kimberlite and carbonate stability in the Earth’s upper mantle. Journal of Geophysical Research, 95(B10), 15805–15816. doi:10.1029/JB095iB10p15805

17 Cawood, P. A., & Hawkesworth, C. J. (2019). Continental crustal volume, thickness and area, and their geodynamic implications. Gondwana Research, 66, 116–125. https://doi.org/10.1016/j.gr.2018.11.001

18 Cline, C. J., Faul, U. H., David, E. C., Berry, A. J., & Jackson, I. S. (2018). Redox‐influenced seismic properties of upper‐mantle olivine. Nature, 555, 355–358. https://doi.org/10.1038/nature25764

19 Cottrell E., & Kelley, K. A. (2013). Redox heterogeneity in mid‐ocean ridge basalts as a function of mantle source. Science, 340, 1314–1317. doi: 10.1126/science.1233299

20 Delano, J. W. (2001). Redox history of the Earth’s interior since similar to 3900 Ma: Implications for prebiotic molecules. Origins of Life and Evolution of the Biosphere, 31, 311–341. doi:10.1023/A:1011895600380.

21 Duncan, M. S., & Dasgupta, R. (2017). Rise of Earth's atmospheric oxygen controlled by efficient subduction of organic carbon. Nature Geoscience, 10, 387–392. https://doi.org/10.1038/ngeo2939

22 Eguchi, J., & Dasgupta, R. (2018). Redox state of the convective mantle from CO2‐trace element systematics of oceanic basalts. Geochemical Perspectives Letters, 8, 17–21. doi: 10.7185/geochemlet.1823

23 Endl, M., Robertson, P., Cochran, W. D., MacQueen, P. J., Brugamyer, E. J., Caldwell, C., et al. (2012). Revisiting ρ1 CANCRI e: A new mass determination of the transiting super‐earth. The Astrophysical Journal, 759, 1.

24 Fischer‐Gödde, M., & Kleine, T. (2017) Ruthenium isotopic evidence for an inner Solar System origin of the late veneer. Nature, 541, 525–527. https://doi.org/10.1038/nature21045

25 Fitoussi, C., & Bourdon, B. (2012). Silicon isotope evidence against an enstatite chondrite Earth. Science, 335, 1477–1480. doi: 10.1126/science.1219509

26 Foley, S. F. (2011). A Reappraisal of Redox Melting in the Earth’s Mantle as a Function of Tectonic Setting and Time. Journal of Petrology, 52(7–8), 1363–1391. doi:https://doi.org/10.1093/petrology/egq061

27 Foley, B. J., & Rizo, H. (2017). Long‐term preservation of early formed mantle heterogeneity by mobile lid convection: Importance of grainsize evolution. Earth and Planetary Science Letters, 475, 94–105. https://doi.org/10.1016/j.epsl.2017.07.031

28 Frost, D. J., Liebske, C., Langenhorst, F., & McCammon, C. A. (2004). Experimental evidence for the existence of iron‐rich metal in the Earth’s lower mantle. Nature, 428, 409–412. https://doi.org/10.1038/nature02413

29 Frost, D. J., & McCammon, C. A. (2008). The redox state of the Earth’s mantle. Annual Review of Earth and Planetary Science 36, 389–420. https://doi.org/10.1146/annurev.earth.36.031207.124322

30 Fu, R. R., Young, E. D., Greenwood, R. C., Elkins‐Tanton, L. T. (2017). Silicate melting and volatile loss during differentiation in planetesimals. In: Elkins‐Tanton, L. T., Weiss, B. P. (Eds.), Planetesimals: Early Differentiation and Consequences for Planets. Cambridge: Cambridge University Press, pp. 115–135.

31 Fuentes, J. J., Crowley, J. W., Dasgupta, R., & Mitrovica, J. X. (2019). The influence of plate tectonic style on melt production and CO2 outgassing flux at mid‐ocean ridges. Earth and Planetary Science Letters, 511, 154–163. doi: https://doi.org/10.1016/j.epsl.2019.01.020

32 Gaillard, F., Scaillet, B., & Arndt, N. T. (2011). Atmospheric oxygenation caused by a change in volcanic degassing pressure. Nature, 478, 229–232. doi:10.1038/nature10460

33 Georg, R. B., Halliday, A. N., Schauble, E. A., Reynolds, B. C. (2007). Silicon in the Earth’s core. Nature, 447, 1102–1106. https://doi.org/10.1038/nature05927

34 Girard, J., Amulele, G., Farla, R., Mohiuddin, A., & Karato, S. (2016). Shear deformation of bridgmanite and magnesiowüstite aggregates at lower mantle conditions. Science, 351, 144–147. doi: 10.1126/science.aad3113

35 Gillon, M., Demory, B.‐O., Benneke, B., Valencia, D., Deming, D., Seager, S., et al. (2012). Improved precision on the radius of the nearby super‐Earth 55 Cnc e. Astronomy & Astrophysics, 539, A28. https://doi.org/10.1051/0004‐6361/201118309

36 Green, D. H. (2015). Experimental petrology of peridotites, including effects of water and carbon on melting in the Earth’s upper mantle. Physics and Chemistry of Minerals, 42, 95–122. https://doi.org/10.1007/s00269‐014‐0729‐2

37 Grossman, L. (1972). Condensation in the primitive solar nebula. Geochimica et Cosmochimica Acta, 36, 597–619. https://doi.org/10.1016/0016‐7037(72)90078‐6

38 Grossman, L., Beckett, J. R., Fedkin, A. V., Simon, S. B., & Ciesla, F. J. (2008). Redox conditions in the Solar Nebula: Observational, experimental, and theoretical constraints. Reviews in Mineralogy and Geochemistry, 68 (1), 93–140. https://doi.org/10.2138/rmg.2008.68.7

39 Grossman, L., Fedkin, A. V., Simon, S. B. (2012). Formation of the first oxidized iron in the Solar System. Meteoritics and Planetary Science, 47, 2160–2169. https://doi.org/10.1111/j.1945‐5100.2012.01353.x

40 Gu, T., Li, M., McCammon, C., & Lee, K. K. (2016). Redox‐induced lower mantle density contrast and effect on mantle structure and primitive oxygen. Nature Geoscience, 9, 723–727. https://doi.org/10.1038/ngeo2772

41 Gudfinnsson, G. H., & Presnall, D. C. (2005). Continuous gradations among primary kimberlitic, carbonatitic, melilitic, basaltic, picritic, and komatiitic melts in equilibrium with garnet lherzolite at 3‐8 GPa. Journal of Petrology, 46, 1645–1659. https://doi.org/10.1093/petrology/egi029

42 Hammouda, T., & Laporte, D. (2000). Ultrafast mantle impregnation by carbonatite melts. Geology, 28, 283–285. https://doi.org/10.1130/0091‐7613(2000)28<283:UMIBCM>2.0.CO;2

43 Harte, B., Harris, J. W., Hutchison, M. T., Watt, G. R., & Wilding, M. C. (1999). Lower mantle mineral associations in diamonds from Sao Luiz, Brazil. Mantle petrology: Field observations and high‐pressure experimentation: A tribute to Francis R. (Joe) Boyd, 6, 125–153. 10.1180/minmag.1994.58A.1.201

44 Holland, H. D. (2002). Volcanic gases, black smokers, and the Great Oxidation Event. Geochimica et Cosmochimica Acta, 66, 3811–3826. doi:10.1016/S0016‐7037(02)00950‐X

45 Horan, M. F., Carlson, R. W., Walker, R. J., Jackson, M., Garçon, M., & Norman, M. (2018). Tracking Hadean processes in modern basalts with 142‐Neodymium. Earth and Planetary Science Letters, 484, 184–191. doi:doi.org/10.1016/j.epsl.2017.12.017

46 Hu, Q., Kim, D. Y., Yang, W., Yang, L., Meng, Y., Zhang, L., & Mao, H. K. (2016). FeO2 and FeOOH under deep lower‐mantle conditions and Earth’s oxygen–hydrogen cycles. Nature, 534, 241–244. https://doi.org/10.1038/nature18018

47 Jacob, D. E., Piazolo, S., Schreiber, A., & Trimby, P. (2016). Redox‐freezing and nucleation of diamond via magnetite formation in the Earth’s mantle. Nature Communications, 7, 11891. doi:10.1038/ncomms11891

48 Javoy, M. (1995). The integral enstatite chondrite model of the Earth. Geophysical Research Letters, 22, 2219–2222. https://doi.org/10.1029/95GL02015

49 Kaminsky, F. (2012). Mineralogy of the Lower Mantle: A Review of “Super‐Deep” Mineral Inclusions in Diamond. Earth‐Science Reviews, 110, 127–147. doi:10.1016/j.earscirev.2011.10.005

50 Kaminsky, F. V., Ryabchikov, I. D., McCammon, A. C., Longo, M., Abakumov, A. M., Turner, S., & Heidari, H. (2015). Oxidation potential in the Earth's lower mantle as recorded by ferropericlase inclusions in diamond. Earth and Planetary Science Letters, 417, 49–56. doi:10.1016/j.epsl.2015.02.029

51 Kasting, J. F., Eggler, D. H., & Raeburn, S. P. (1993). Mantle redox evolution and the oxidation state of the Archean atmosphere. Journal of Geology, 101, 245–257. doi:10.1086/648219

52 Kiseeva, E., Vasiukov, D. M., Wood, B. J., McCammon, C., Stachel, T., Bykov, M., et al. (2018). Oxidized iron in garnets from the mantle transition zone. Nature Geoscience, 11, 144–147. https://doi.org/10.1038/s41561‐017‐0055‐7

53 Lammer, H., Zerkle, A. L., Gebauer, S., Tosi, N., Noack, L., Scherf, M., et al. (2018). Origin and evolution of the atmospheres of early Venus, Earth and Mars. The Astronomy and Astrophysics Review, 26, 2. https://doi.org/10.1007/s00159‐018‐0108‐y

54 Lécuyer, C., & Ricard, Y. (1999). Long‐term fluxes and budget of ferric iron: Implications for the redox state of Earth mantle and atmosphere. Earth and Planetary Science Letters, 165, 197–211. https://doi.org/10.1016/S0012‐821X(98)00267‐2

55 Li, Z. X. A., & Lee, C. T. A. (2004). The constancy of upper mantle fO(2) through time inferred from V/Sc ratios in basalts. Earth and Planetary Science Letters, 228, 483–493. doi:10.1016/j.epsl.2004.10.006.

56 Liebske, C., & Khan, A. (2019). On the principal building blocks of Mars and Earth. Icarus, 322, 121–134. https://doi.org/10.1016/j.icarus.2019.01.014

57 Liu, J., Dorfman, S. M., Zhu, F. J., Li, J., Wang, Y., Zhang, D., et al. (2018). Valence and spin states of iron are invisible in Earth’s lower mantle. Nature Communications, 9, 1284. https://doi.org/10.1038/s41467‐018‐03671‐5

58 Lyons, T. W., Reinhard, C. T., & Planavsky, N. J. (2014). The rise of oxygen in Earth’s early ocean and atmosphere. Nature, 506, 307–315. https://doi.org/10.1038/nature13068

59 Luth, R. W., & Stachel, T. (2014). The buffering capacity of lithospheric mantle: implications for diamond formation. Contributions to Mineralogy and Petrology, 168, 1–12. https://doi.org/10.1007/s00410‐014‐1083‐6

60 Madhusudhan, N. (2012). C/O ratio as a dimension for characterizing exoplanetary atmospheres. Astrophysics Journal, 758, 36. doi:10.1088/0004‐637X/758/1/36.

61 Martin, R. S., Mather, T. A., & Pyle D. M. (2007). Volcanic emissions and the early Earth atmosphere. Geochimica et Cosmochimica Acta, 71, 3673–3685. https://doi.org/10.1016/j.gca.2007.04.035

62 McCammon, C. A. (2005). The paradox of mantle redox. Science, 308, 807–808. 10.1126/science.1110532

63 McKenzie, D. (1989). Some remarks on the movement of small melt fractions in the mantle. Earth and Planetary Science Letters, 95(1–2), 5372. https://doi.org/10.1016/0012‐821X(89)90167‐2

64 Moussallam, Y., Oppenheimer, C., & Scaillet, B. (2019). On the relationship between oxidation state and temperature of volcanic gas emissions. Earth and Planetary Science Letters, 520, 260–267. https://doi.org/10.1016/j.epsl.2019.05.036

65 Nicklas R. W., Puchtel I. S., & Ash, R. D. (2018). Redox state of the Archean mantle: Evidence from V partitioning in 3.5–2.4 Ga komatiites. Geochimica et Cosmochimica Acta, 222, 447–466. https://doi.org/10.1016/j.gca.2017.11.002

66 Nicklas, R. W., Puchtel, I. S., Ash, R. D., Piccoli, P. M., Hanski, E., Nisbet, E. G., et al. (2019). Secular mantle oxidation across the Archean‐Proterozoic boundary: Evidence from V partitioning in komatiites and picrites. Geochimica et Cosmochimica Acta, 250, 49–75. doi:https://doi.org/10.1016/j.gca.2019.01.037

67 O’Neill, H. St.C. (1991). The origin of the Moon and the early history of the Earth ‐a chemical model. Part 2: The Earth. Geochimica et Cosmochimica Acta, 55, 1159–1172. https://doi.org/10.1016/0016‐7037(91)90169‐6

68 Pahlevan, K., Schaefer, L., & Hirschmann, M. M. (2019). Hydrogen isotopic evidence for early oxidation of silicate Earth. Earth and Planetary Science Letters, 115770. https://doi.org/10.1016/j.epsl.2019.115770

69 Pearson, D. G., Brenker, F. E., Nestola, F., McNeill, J., Nasdala, L., Hutchison, M. T., et al. (2014). Hydrous mantle transition zone indicated by ringwoodite included within diamond. Nature, 507, 221–224. doi:10.1038/nature13080.

70 Righter, K., Sutton, S. R., Danielson, L., Pando, K., & Newville, M. (2016). Redox variations in the inner solar system with new constraints from vanadium XANES in spinels. American Mineralogist, 101 (9), 1928–1942. doi: https://doi.org/10.2138/am‐2016‐5638

71 Rizo, H., Walker, R. J., Carlson, R. W., Horan, M. F., Mukhopadhyay, S., Manthos, V., et al. (2016). Preservation of Earth‐forming events in the tungsten isotopic composition of modern flood basalts. Science, 352, 809–812. 10.1126/science.aad8563

72 Rohrbach, A., Ballhaus, C., Ulmer, P., Golla‐Schindler, U., & Schönbohm, D. (2011). Experimental evidence for a reduced metal‐saturated upper mantle. Journal of Petrology, 52, 717–731. https://doi.org/10.1093/petrology/egq101

73 Rohrbach, A., & Schmidt, M. W. (2011). Redox freezing and melting in the Earth’s deep mantle resulting from carbon‐iron redox coupling. Nature, 472, 209–212. https://doi.org/10.1038/nature09899

74 Rollinson, H., Adetunji, J., Lenaz, D., & Szilas, K. (2017). Archaean chromitites show constant Fe3 +/∑Fe in Earth's asthenospheric mantle since 3.8 Ga. Lithos, 282–283, 316––325. https://doi.org/10.1016/j.lithos.2017.03.020

75 Rubie, D. C., Jacobson, S. A., Morbidelli, A., O’Brien, D. P., Young, E. D., de Vries, J., et al. (2015). Accretion and differentiation of the terrestrial planets with implications for the compositions of early‐formed Solar System bodies and accretion of water. Icarus, 248, 89–108. https://doi.org/10.1016/j.icarus.2014.10.015

76 Scaillet, B., & Gaillard, F. (2011). Redox state of early magmas. Nature, 480, 48–49. https://doi.org/10.1038/480048a

77 Schaefer, L., & Fegley, B. Jr. (2017). Redox states of initial atmospheres outgassed on rocky planets and planetesimals. Astrophysical Journal Letters, 843, 120. https://doi.org/10.3847/1538‐4357/aa784f

78 Smart, K. A., Tappe, S., Stern, R. A., Webb, S. J., & Ashwal, L. D. (2016). Early Archaean tectonics and mantle redox recorded in Witwatersrand diamonds. Nature Geoscience, 9, 255–259. doi: 10.1038/NGEO2628

79 Smith, E. M., Shirey, S. B., Nestola, F., Bullock, E. S., Wang, J. H., Richardson, S. H., & Wang, W. Y. (2016). Large gem diamonds from metallic liquid in Earth’s deep mantle. Science, 354, 1403–1405. doi: 10.1126/science.aal1303

80 Stachel, T., Brey, G. P., & Harris, J. W. (2005). Inclusions in sublithospheric diamonds: glimpses of deep Earth. Elements, 1, 73–78. https://doi.org/10.2113/gselements.1.2.73

81 Stagno, V. (2019). Carbon, carbonates and carbonatitic melts in the Earth’s interior. Journal of the Geological Society, London, 176, 375–387. doi:https://doi.org/10.1144/jgs2018‐095

82 Stagno, V., & Frost, D. J. (2010). Carbon speciation in the asthenosphere: Experimental measurements of the redox conditions at which carbonate‐bearing melts coexist with graphite or diamond in peridotite assemblages. Earth and Planetary Science Letters, 30, 72–84. doi:10.1016/j.epsl.2010.09.038.

83 Stagno, V., Tange, Y., Miyajima, N., McCammon, C. A., Irifune, T., & Frost, D. J. (2011). The stability of magnesite in the transition zone and the lower mantle as function of oxygen fugacity. Geophysical Research Letters, 38, L19309. https://doi.org/10.1029/2011GL049560

84 Stagno V., Ojwang, D. O., McCammon, C. A., & Frost, D. J. (2013). The oxidation state of the mantle and the extraction of carbon from Earth’s interior. Nature, 493, 84–88. https://doi.org/10.1038/nature11679

85 Stagno V., Frost, D. J., McCammon, C. A., Mohseni, H., & Fei, Y. (2015). The oxygen fugacity at which graphite or diamond forms from carbonate‐bearing melts in eclogitic rocks. Contributions to Mineralogy and Petrology, 169, 16. https://doi.org/10.1007/s00410‐015‐1111‐1

86 Stagno, V., Cerantola, V., Aulbach, S., Lobanov, S., McCammon, C., & Merlini, M. (2019). Carbon‐bearing phases throughout Earth’s interior: Evolution through space and time. In: Orcutt, B., Daniel, I., & Dasgupta, R. (Eds.), Deep Carbon: Past to Present. Cambridge: Cambridge University Press. pp. 66–88.

87 Tappe, S., Smart, K. A, Torsvik, T. H., Massuyeau, M., & de Wit, M. C. J. (2018) Geodynamics of kimberlites on a cooling Earth: Clues to plate tectonic evolution and deep volatile cycles. Earth and Planetary Science Letters, 484, 1–14. doi:10.1016/j.epsl.2017.12.013

88 Taylor, W. R., & Green, D. H. (1988). Measurement of reduced peridotite‐C‐O‐H solidus and implications for redox melting of the mantle. Nature, 332, 349–352. https://doi.org/10.1038/332349a0

89 Thomson, A. R., Walter, M. J., Kohn, S. C., & Brooker, R. A. (2016). Slab melting as a barrier to deep carbon subduction. Nature, 529, 76–79. https://doi.org/10.1038/nature16174

90 Trail, D., Watson, E. B., & Tailby, N. D. (2011). The oxidation state of Hadean magmas and implications for early Earth’s atmosphere. Nature, 480, 79–82. https://doi.org/10.1038/nature10655

91 Tschauner, O., Huang, S., Greenberg, E., Prakapenka, V. B., Ma, C., Rossman, G. R., et al. (2018). Ice‐VII inclusions in diamonds: Evidence for aqueous fluid in Earth’s deep mantle. Science, 356, 1136–1139. 10.1126/science.aao3030

92 Wade, J., & Wood, B. J. (2005). Core formation and the oxidation state of the Earth. Earth and Planetary Science Letters, 236, 78–95. https://doi.org/10.1016/j.epsl.2005.05.017

93 Walter, M., Bulanova, G., Armstrong, L., Keshav, S., Blundy, J. D., Gudfinnsson, G., et al. (2008). Primary carbonatite melt from deeply subducted oceanic crust. Nature, 454, 622–625. https://doi.org/10.1038/nature07132

94 Wang, Z., & Becker, H. A. (2013). Ratios of S, Se and Te in the silicate Earth require a volatile‐rich late veneer. Nature, 499, 328–331. https://doi.org/10.1038/nature12285

95 Wark, D. J., & Lovering, F. (1977). Marker events in the early evolution of the solar system: evidence from rims on Ca‐Al‐rich inclusion in carbonaceous chondrites. Proceedings of the Lunar Planetary Science Conference, 8th, 95–112.

96 Williams, S. N, Schaefer, S. J., Marta Lucia Calvache, V., & Lopez, D. (1992). Global carbon dioxide emission to the atmosphere by volcanoes. Geochimica et Cosmochimica Acta, 56(4), 1765–1770. doi:https://doi.org/10.1016/0016‐7037(92)90243‐C.

97 Wirth, R., Dobrzhineskaya, L., Harte, B., Schreiber, A., & Green, H. W. (2014). High‐Fe (Mg, Fe)O inclusion in diamond apparently from the lowermost mantle. Earth and Planetary Science Letters, 404, 365–375. https://doi.org/10.1016/j.epsl.2014.08.010

98 Wood, B. J., Walter, M. J., & Wade, J. H. (2006). Accretion of the Earth and segregation of its core. Nature, 441, 825–833. https://doi.org/10.1038/nature04763

99 Wyllie, P. J., & Huang, W. L. (1975). Influence of mantle CO2 in the generation of carbonatites and kimberlites. Nature, 257, 297–299. https://doi.org/10.1038/257297a0

100 Yang, X., Gaillard, F., & Scaillet, B. (2014). A relatively reduced Hadean continental crust and implications for the early atmosphere and crustal rheology. Earth and Planetary Science Letters, 393, 210–219. https://doi.org/10.1016/j.epsl.2014.02.056

Magma Redox Geochemistry

Подняться наверх