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TypeMineralsNameReferenceCommentsGrtCpxOpxOlSplIlmHblCrdStBtMuChlCldTlcPlFspKySilAndQtzCoeRuMlt
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TGrtCpxAi, 1994Ai Y. A revision of the garnet-clinopyroxene Fe[+2]-Mg exchange geothermometer // Contrib. Mineral. Petrol., 1994, v.115, p.467-473Lower crust and upper mantle11
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TGrtCpxEllis & Green, 1979Ellis D.J., Green D.H. An Experimental Study of the Effect of Ca Upon Garnet-Clinopyroxene Fe-Mg Exchange Equilibria // Contrib. Mineral. Petrol., 1979, v.71, p.13-22Better for T > 1200°C, uncertainty: ±40°11
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TGrtCpxKrogh, 1988Krogh E.J. The garnet-clinopyroxene Fe-Mg geothermometer - a reinterpretation of existing experimental data // Contrib. Mineral. Petrol., 1988, v.99(1), p.44-4811
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TGrtCpxRavna, 2000Ravna E.J.K. The garnet-clinopyroxene Fe[2+]-Mg geothermometer: an updated calibration // Journal of Metamorphic Geology, 2000, v.18(2), p.211-219Check "Use Fe[3+]" option11
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TGrtCpxMori & Green, 1978Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100°11
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TGrtCpxNakamura, 2006Nakamura D. A new formulation of garnet-clinopyroxene thermometer using large number of experimental data with graphite capsules. // 19th General Meeting of the International Mineralogical Association, Kobe, Japan (July. 2006). Program & Abstract, 2006, p.10211
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TGrtCpxNakamura, 2009Nakamura D. A new formulation of garnet-clinopyroxene geothermometer based on accumulation and statistical analysis of a large experimental data set // Journal of Metamorphic Geology, 2009, v.27(7), p.495-50811
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TGrtCpxNikitina & Ivanov, 1993Nikitina L.P., Ivanov M.V. Garnet-clinopyroxene geothermobarometer for mantle eclogites // Doklady Rossiyskoy Akademii Nauk, 1993, v.331(2), p.214-216 (in Russian))Component of Grt-Cpx geothermobarometer11
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TGrtCpxNikitina & Simakov, 1994-TNikitina L.P., Simakov S.K. Garnet-clinopyroxene thermobarometer and oxygen barometer for eclogites // V-th International EMPG Symposium (Abstracts), Terra Nova, 1994, v.6, p.34Component of Grt-Cpx geothermobarometer, garnet peridotites and eclogites11
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TGrtCpxPowell, 1985Powell R. Regression diagnostics and robust regress in geothermometer/geobarometer calibration: the garnet-clinopyroxene geothermometer revisited // Journal of Metamorphic Geology, 1985, v.3(3), p.231-243Preferable for T < 1200°C11
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TGrtCpxSengupta et al., 1989Sengupta P., Dasgupta S., Bhattacharya P.K., Hariya Y. Mixing behavior in quaternary garnet solid solution and an extended Ellis and Green garnet-clinopyroxene geothermometer // Contrib. Mineral. Petrol., 1989, v.103(2), p.223-227Granulites (with low contents of Na, Al and Fe+3 in Cpx), xFe(Grt)<0.6511
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TGrtCpxSudholz et al., 2022cSudholz Z.J., Green D.H., Yaxley G.M., Jaques A.L. Mantle geothermometry: experimental evaluation and recalibration of Fe-Mg geothermometers for garnet-clinopyroxene and garnet-orthopyroxene in peridotite, pyroxenite and eclogite systems // Contrib. Mineral. Petrol., 2022, v.177, a.77, DOI:10.1007/s00410-022-01944-3Multiple linear regression over dataset comprised of >300 peridotite, pyroxenite and eclogite experiments at P=10-70 kbar, T=850-1650°C11
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TCpx(Grt)Ashchepkov et al., 2008Ashchepkov I.V., Pokhilenko N.P., Vladykin N.V., Rotman A.Y., Afanasiev V.P., Logvinova A.M., Kostrovitsky S.I., Pokhilenko L.N., Karpenko M.A., Kuligin S.S., Malygina E.V., Stegnitsky Y.B., Alymova N.A., Khmelnikova O.S. Reconstruction of mantle sections beneath Yakutian kimberlite pipes using monomineral thermobarometry // In: Coltorty M. & Goire G.M. (eds) Metasomatism in Oceanic and Continental Lithospheric Mantle, Geological Society, London, Special Publications, 2008, v.293, p.335-352Correction of [Nimis & Taylor, 2000] Cpx geothermometer01
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TCpx(Grt)Ellis & Green, 1979sEllis D.J., Green D.H. An Experimental Study of the Effect of Ca Upon Garnet-Clinopyroxene Fe-Mg Exchange Equilibria // Contrib. Mineral. Petrol., 1979, v.71, p.13-22Modelled eclogitic Grt composition is used (Simakov, 2008)01
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TCpx(Grt)Nimis & Taylor, 2000-TNimis P., Taylor W.R. Single clinopyroxene thermobarometry for garnet peridotites. Part I. Calibration and testing of a Cr-in Cpx barometer and an enstatite-in-Cpx thermometer // Contrib. Mineral. Petrol., 2000, v.139(5), p.541-554Component of Cpx geothermobarometer for Grt peridotites01
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TGrtOpxCarswell & Harley, 1990Carswell D.A., Harley S.L. Mineral barometry and thermometry // In: Carswell D.A. (Ed.), Eclogite Facies Rocks, Blackie & Sous, Glasgow, 1990, p.83-110Garnet peridotites and eclogites11
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TGrtOpxGanguly, Cheng & Tirone, 1996Ganguly J., Cheng W., Tirone M. Thermodynamics of aluminosilicate garnet solid solution: new experimental data, an optimized model, and thermometric applications // Contrib. Mineral. Petrol., 1996, v.126(1-2), p.137-151, DOI:10.1007/s004100050240Mn-corrected version; small underestimation (ca. 2-3°) vs. GTPX-TEM.exe program of J. Ganguly is unclear11
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TGrtOpxHarley, 1984Harley S.L. An experimental study of the partitioning of Fe and Mg between garnet and orthopyroxene // Contrib. Mineral. Petrol., 1984, v.86, p.359-37311
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TGrtOpxLavrentieva & Perchuk, 1990Lavrentieva I.L., Perchuk L.L. Orthopyroxene-garnet geothermometer: experiment and theoretical processing of database // Doklady Akademii Nauk SSSR, 1990, v.310(1), p.179-182 (in Russian)11
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TGrtOpxMori & Green, 1978Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100°11
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TGrtOpxNikitina et al., 2010-TNikitina L.P., Goncharov A.G., Saltykova A.K., Babushkina M.S. Oxygen-reduction condition of continental lithosphere mantle under Baikal-Mongolian region // Geochemistry, 2010, №1, p..17-44 (in Russian)Component of Grt-Opx geothermobarometer for mafic and ultramafic rocks formed at 700°C < T < 1500°C and 4-5 < P,kbar < 55-60, uncertainty: ±10%11
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TGrtOpxNimis & Grutter, 2010Nimis P., Grutter H. Internally consistent geothermometers for garnet peridotites and pyroxenites // Contrib. Mineral. Petrol., 2010, v.159, p.411-427, DOI 10.1007/s00410-009-0455-9Based on natural samples (2Px thermometer [Taylor, 1998] and Grt-Opx barometer [Nickel & Green, 1985]), uncertainty: ±34°11
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TGrtOpxSudholz et al., 2022oSudholz Z.J., Green D.H., Yaxley G.M., Jaques A.L. Mantle geothermometry: experimental evaluation and recalibration of Fe-Mg geothermometers for garnet-clinopyroxene and garnet-orthopyroxene in peridotite, pyroxenite and eclogite systems // Contrib. Mineral. Petrol., 2022, v.177, a.77, DOI:10.1007/s00410-022-01944-3Multiple linear regression over dataset comprised of >300 peridotite, pyroxenite and eclogite experiments at P=10-70 kbar, T=850-1650°C11
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TGrt(OpxCpx)Boyd & Schairer, 1964aBoyd F.R., Schairer J.F. The system MgSiO3-CaMgSi2O6 // Journal of Petrology, 1964, v.5(2), p.275-309Mg-systems only, Cpx composition estimated from xFe(Grt) (Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136)100
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TGrt(OpxCpx)Boyd & Schairer, 1964bBoyd F.R., Schairer J.F. The system MgSiO3-CaMgSi2O6 // Journal of Petrology, 1964, v.5(2), p.275-309Mg-systems only, Cpx composition estimated from Ca/Mg(Grt) (Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136)100
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TGrt(OpxCpx)Davis & Boyd, 1966aDavis B.T.C., Boyd Jr F.R. The join Mg2Si2O6-CaMgSi2O6 at 30 kilobars pressure and its application to pyroxenes from kimberlites //Journal of Geophysical Research, 1966, v.71(14), p.3567-3576Mg-systems only, Cpx composition estimated from xFe(Grt) (Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136)100
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TGrt(OpxCpx)Davis & Boyd, 1966bDavis B.T.C., Boyd Jr F.R. The join Mg2Si2O6-CaMgSi2O6 at 30 kilobars pressure and its application to pyroxenes from kimberlites //Journal of Geophysical Research, 1966, v.71(14), p.3567-3576Mg-systems only, Cpx composition estimated from Ca/Mg(Grt) (Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136)100
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TGrt(OpxCpx)Lindsley & Dixon, 1976aLindsley D.H., Dixon S.S. Diopside-enstatite equilibria at 850°C-1400°C, 5-35 kb // American Journal of Sciences, 1976, v.276, p.1285-1301Mg-systems only, Cpx composition estimated from xFe(Grt) (Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136)100
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TGrt(OpxCpx)Lindsley & Dixon, 1976bLindsley D.H., Dixon S.S. Diopside-enstatite equilibria at 850°C-1400°C, 5-35 kb // American Journal of Sciences, 1976, v.276, p.1285-1301Mg-systems only, Cpx composition estimated from Ca/Mg(Grt) (Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136)100
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TGrt(OpxCpx)Simakov, 2012Simakov S.K. A new garnet thermometer for mantle peridotites and estimation of the diamond potential on its basis // Doklady Earth Sciences, 2012, v.445(2), p.1003-1005, DOI 10.1134/S1028334X12060189Garnet peridotites, Ca, Mg, Fe and Cr in Grt accounted, uncertainty is ±150°100
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TGrtOlCanil, 1999Canil D. The Ni in garnet geothermometer: calibration at natural abundances // Contrib. Mineral. Petrol., 1999, v.136(3), p.313-324Grt peridotites, based on Ni distribution (in ppm) between Grt and Ol11
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TGrtOlMori & Green, 1978Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100°11
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TGrtOlO'Neill & Wood, 1979O'Neill H.S.C., Wood B.J. An Experimental Study of Fe-Mg Partitioning Between Garnet and Olivine and Its Calibration as a Geothermometer // Contrib. Mineral. Petrol., 1979, v.70, p.59-70Lherzolites11
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TGrtOlSudholz et al., 2021Sudholz Z.J., Yaxley G.M., Jaques A.L., Chen J. Ni-in-garnet geothermometry in mantle rocks: a high pressure experimental recalibration between 1100 and 1325°C // Contrib. Mineral. Petrol., 2021, v.176, a.32, DOI:10.1007/s00410-021-01791-8For Grt peridotites, based on Ni-exchange between Grt and Ol; calibrated at 2.25-4.5 GPa and 1100-1325°C; uncertainties 55°C11
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TGrt(Ol)Sudholz et al., 2021aSudholz Z.J., Yaxley G.M., Jaques A.L., Chen J. Ni-in-garnet geothermometry in mantle rocks: a high pressure experimental recalibration between 1100 and 1325°C // Contrib. Mineral. Petrol., 2021, v.176, a.32, DOI:10.1007/s00410-021-01791-8For Grt peridotites, based on Ni-exchange between Grt and Ol; calibrated at 2.25-4.5 GPa and 1100-1325°C; uncertainties 55°C; 2900 ppm is taken as a default Ni content in Ol. You can change it using the button [Other] (placed under "Independent parameters")10
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TGrt(Ol)Canil, 1999aCanil D. The Ni in garnet geothermometer: calibration at natural abundances // Contrib. Mineral. Petrol., 1999, v.136(3), p.313-324Grt peridotites, modification of [Canil, 1999] geothermometer based on Ni distribution between Grt and Ol. 2900 ppm is taken as a default Ni content in Ol. You can change it using the button [Other] (placed under "Independent parameters")10
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TGrt(Ol)Creighton, 2009Creighton S. A semi-empirical manganese-in-garnet single crystal thermometer // 9th IKC Proceedings, Part I, Lithos, 2009, v.112S, p.177-182For Grt xenocrysts from garnet peridotites; accuracy ±150°; corrected publication typos10
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TGrt(Ol)Griffin et al., 1989Griffin W.L., Cousens D.R., Ryan C.G., Sie S.H., Suter G.F. Ni in chrome pyrope garnets: a new geothermometer // Contrib. Mineral. Petrol., 1989, v.103(2), p.199-202Grt peridotites, based on Ni solubility in the coexistent Chromium Ol and Grt, 3000 ppm used for Ni content in Ol10
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TGrt(Ol)Ryan, Griffin & Pearson, 1996aRyan C.G., Griffin W.L., Pearson N.J. Garnet geotherms: pressure-temperature data from Cr-pyrope garnet xenocrysts in volcanic rocks // Journal of Geophysical Research, 1996, v.101(B3), p.5611-5625Garnet peridotites, based on Ni distribution (in ppm) between Grt (enriched in Cr) and Ol10
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TGrt(Ol)Nimis, Zanetti & Franz, 2024Nimis P., Zanetti A. & Franz L. A revision of the Ni-in-garnet geothermometer with special regard to its pressure dependence // Lithos, 2024, v.468-469, a.107513 DOI:10.1016/j.lithos.2024.107513Pressure-dependent expression for Ni-in-garnet geothermometer11
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TGrt(Ol)Nimis, Zanetti & Franz, 2024aNimis P., Zanetti A. & Franz L. A revision of the Ni-in-garnet geothermometer with special regard to its pressure dependence // Lithos, 2024, v.468-469, a.107513 DOI:10.1016/j.lithos.2024.107513Pressure-dependent expression for Ni-in-garnet geothermometer; 2900 ppm is taken as a default Ni content in Ol. You can change it using the button [Other] (placed under "Independent parameters")10
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TGrt(OpxCpxOl)Ashchepkov et al., 2008aAshchepkov I.V., Pokhilenko N.P., Vladykin N.V., Rotman A.Y., Afanasiev V.P., Logvinova A.M., Kostrovitsky S.I., Pokhilenko L.N., Karpenko M.A., Kuligin S.S., Malygina E.V., Stegnitsky Y.B., Alymova N.A., Khmelnikova O.S. Reconstruction of mantle sections beneath Yakutian kimberlite pipes using monomineral thermobarometry // In: Coltorty M. & Goire G.M. (eds) Metasomatism in Oceanic and Continental Lithospheric Mantle, Geological Society, London, Special Publications, 2008, v.293, p.335-352Ordinary peridotites, based on correlation between Grt composition and temperatures estimated using Opx(GrtCpxOl) geothermometer T_BKN [Brey & Kohler, 1990] NB! Unclear errors detected!1000
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TOpxCpxBertrand & Mercier, 1985Bertrand P., Mercier J.-C.C. The mutual solubility of coexisting ortho- and clinopyroxene: toward an absolute geothermometer for the natural system? // E. Plan. Sc. Lett., 1985, v.76(1-2), p.109-12211
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TOpxCpxMori & Green, 1978Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100°11
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TOpxCpxNikitina at al., 2010aNikitina L.P., Goncharov A.G., Saltykova A.K., Babushkina M.S. Oxidation-reduction condition of continental lithosphere mantle under Baikal-Mongolian region // Geochemistry, 2010(1), p.17-44 (in Russian)11
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TOpxCpxSimakov, 2000aSimakov S.K. The clinopyroxene thermometry of mantle peridotites: implication for diamond evaluation potential // Doklady Earth Sciences, 2000, v.375(8), p.1266-1268Peridotites11
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TOpxCpxSimakov, 2008aSimakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136Peridotites11
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TOpxCpxTaylor, 1998Taylor W.R. An experimental test of some geothermometer and geobarometer formulations for upper mantle peridotites with application to the thermobarometry of fertile lherzolite and garnet websterite // Neues Jahrbuch fur Mineralogie. Abhandlungen, 1998, v.172(2-3), p.381-408Upper mantle peridotites and lherzolites, P=10-35 kbar, T=1050-1260°C11
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TOpxCpxWells, 1977Wells P.A. Pyroxene Thermometry in Simple and Complex Systems // Contrib. Mineral. Petrol., 1977, v.62, p.129-13911
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TOpxCpxWood & Banno, 1973Wood B. J., Banno S. Garnet-orthopyroxene and orthopyroxene-clinopyroxene relationships in simple and complex systems // Contrib. Mineral. Petrol., 1973, v.42, p.109-12411
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TOpxCpxPutirka, 2008Putirka K. Thermometers and Barometers for Volcanic Systems // In: Putirka K., Tepley F. (Eds.), Minerals, Inclusions and Volcanic Processes. Reviews in Mineralogy and Geochemistry, Mineralogical Soc. Am., 2008, v. 69(1), p. 61-120. DOI:10.2138/rmg.2008.69.3Global regression (eq. 36); perform best for mafic systems with xMg(Cpx)>0.7511
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TOpxCpxPutirka, 2008aPutirka K. Thermometers and Barometers for Volcanic Systems // In: Putirka K., Tepley F. (Eds.), Minerals, Inclusions and Volcanic Processes. Reviews in Mineralogy and Geochemistry, Mineralogical Soc. Am., 2008, v. 69(1), p. 61-120. DOI:10.2138/rmg.2008.69.3Regression for data with xMg(Cpx)<0.75 (eq. 37)11
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TOpxCpxSlavinsky, 1983Slavinsky V.V. Two-pyroxene thermometry // Mineralogical Journal, 1983, v.5(6), p. 29-38 (in Russian).Full PT-dependent expression (iterative solution)11
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TOpxCpxSlavinsky, 1983aSlavinsky V.V. Two-pyroxene thermometry // Mineralogical Journal, 1983, v.5(6), p. 29-38 (in Russian).Simplified expression not dependent on PT11
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TOpxCpxFonarev, Graphchikov, 1991aFonarev V.I., Graphchikov A.A. Two-pyroxene thermometry: a critical evaluation. In: "Progress in metamorphic and magmatic petrology. A memorial volume in honor of D.S.Korzhinskiy" Edt. L.L. Perchuk. Cambridge University Press, Cambridge, 1991, p. 65-92Based on experimental data which include low-temperature runs and Fe-rich compositions. High-T expression for T=900-1250°C, P<20 kbar. Option "Check constraints" is strongly recommended11
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TOpxCpxFonarev, Graphchikov, 1991bFonarev V.I., Graphchikov A.A. Two-pyroxene thermometry: a critical evaluation. In: "Progress in metamorphic and magmatic petrology. A memorial volume in honor of D.S.Korzhinskiy" Edt. L.L. Perchuk. Cambridge University Press, Cambridge, 1991, p. 65-92Based on experimental data which include low-temperature runs and Fe-rich compositions. Low-T expression for T=600-900°C, P<20 kbar. Option "Check constraints" is strongly recommended11
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TOpxCpxFonarev, Graphchikov, 1991cFonarev V.I., Graphchikov A.A. Two-pyroxene thermometry: a critical evaluation. In: "Progress in metamorphic and magmatic petrology. A memorial volume in honor of D.S.Korzhinskiy" Edt. L.L. Perchuk. Cambridge University Press, Cambridge, 1991, p. 65-92Based on experimental data which include low-temperature runs and Fe-rich compositions. Expression for Mn-rich Opx compositions and T=600-900°C, P<20 kbar. Option "Check constraints" is strongly recommended11
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TCpx(Opx)Boyd & Schairer, 1964Boyd F.R., Schairer J.F. The system MgSiO3-CaMgSi2O6 // Journal of Petrology, 1964, v.5(2), p.275-309Mg-systems only10
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TCpx(Opx)Davis & Boyd, 1966Davis B.T.C., Boyd Jr F.R. The join Mg2Si2O6-CaMgSi2O6 at 30 kilobars pressure and its application to pyroxenes from kimberlites //Journal of Geophysical Research, 1966, v.71(14), p.3567-3576Mg-systems only10
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TCpx(Opx)Lindsley & Dixon, 1976Lindsley D.H., Dixon S.S. Diopside-enstatite equilibria at 850°C-1400°C, 5-35 kb // American Journal of Sciences, 1976, v.276, p.1285-1301Mg-systems only10
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TCpx(Opx)Simakov, 2000bSimakov S.K. The clinopyroxene thermometry of mantle peridotites: implication for diamond evaluation potential // Doklady Earth Sciences, 2000, v.375(8), p.1266-1268Modelled Opx composition10
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TCpx(Opx)Simakov, 2008bSimakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136Estimated (modelled) Opx composion10
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TCpx(GrtOpx)Mercier, 1980bMercier J. Single-pyroxene thermobarometry // Tectonophysics, 1980, v.70, p.1-37Grt peridotites010
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TOpx(GrtCpx)Mercier, 1980bMercier J. Single-pyroxene thermobarometry // Tectonophysics, 1980, v.70, p.1-37Grt peridotites001
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TCpxPutirka, 2008bPutirka K. Thermometers and Barometers for Volcanic Systems // In: Putirka K., Tepley F. (Eds.), Minerals, Inclusions and Volcanic Processes. Reviews in Mineralogy and Geochemistry, Mineralogical Soc. Am., 2008, v. 69(1), p. 61-120. DOI:10.2138/rmg.2008.69.3Eq. 32d similar to Nimis & Taylor (2000) thermometer for Grt peridotites, based on expanded data set and claimed to be more precise1
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TCpxMltPutirka, 2008cPutirka K. Thermometers and Barometers for Volcanic Systems // In: Putirka K., Tepley F. (Eds.), Minerals, Inclusions and Volcanic Processes. Reviews in Mineralogy and Geochemistry, Mineralogical Soc. Am., 2008, v. 69(1), p. 61-120. DOI:10.2138/rmg.2008.69.3Eq. 33 for mafic to intermediate melts P<70 kbar; can be used with Putirka, 2008d (Cpx saturation curve); specify H2O by Totals of oxides (H2O,wt%=100-Sum of oxides,wt%) or via "H2O, wt.%" parameter in the "Other" window; only actual melt compositions to be used11
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TCpxMltWang et al., 2021aWang X., Hou T., Wang M., Zhang C., Zhang Z., Pan R., Marxer F., Zhang H. A new clinopyroxene thermobarometer for mafic to intermediate magmatic systems // European Journal of Mineralogy, 2021, v. 33(5), p. 621-637. DOI:10.5194/ejm-33-621-2021For mafic to intermediate melts (SiO2<60 wt%), empirical calibration based on simple polynomial expressions; Cpx: Al(M)>0, Jd>0; P=0.001-12 kbar, T>800°C; actual or fictive melt compositions are used for H2O=100-Sum of oxides, wt.%11
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TCpxMltWang et al., 2021cWang X., Hou T., Wang M., Zhang C., Zhang Z., Pan R., Marxer F., Zhang H. A new clinopyroxene thermobarometer for mafic to intermediate magmatic systems // European Journal of Mineralogy, 2021, v. 33(5), p. 621-637. DOI:10.5194/ejm-33-621-2021For mafic to intermediate melts (SiO2<60 wt%), Putirka (2008) model combined with empirical calibration based on simple polynomial expressions (eq. 32dH); Cpx: Al(M)>0, Jd>0; P=0.001-12 kbar, T>800°C; actual or fictive melt compositions are used for H2O=100-Sum of oxides, wt.%11
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TCpx(Mlt)Wang et al., 2021Wang X., Hou T., Wang M., Zhang C., Zhang Z., Pan R., Marxer F., Zhang H. A new clinopyroxene thermobarometer for mafic to intermediate magmatic systems // European Journal of Mineralogy, 2021, v. 33(5), p. 621-637. DOI:10.5194/ejm-33-621-2021For mafic to intermediate melts (SiO2<60 wt%), empirical calibration based on simple polynomial expressions; Cpx: Al(M)>0, Jd>0; P=0.001-12 kbar, T>800°C; set assumed wt.% H2O in melt (common for all samples) in the "Other" window10
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TCpx(Mlt)Wang et al., 2021bWang X., Hou T., Wang M., Zhang C., Zhang Z., Pan R., Marxer F., Zhang H. A new clinopyroxene thermobarometer for mafic to intermediate magmatic systems // European Journal of Mineralogy, 2021, v. 33(5), p. 621-637. DOI:10.5194/ejm-33-621-2021For mafic to intermediate melts (SiO2<60 wt%), Putirka (2008) model combined with empirical calibration based on simple polynomial expressions (eq. 32dH); Cpx: Al(M)>0, Jd>0; P=0.001-12 kbar, T>800°C; set assumed wt.% H2O in melt (common for all samples) in the "Other" window10
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TMlt(Cpx)Putirka, 2008dPutirka K. Thermometers and Barometers for Volcanic Systems // In: Putirka K., Tepley F. (Eds.), Minerals, Inclusions and Volcanic Processes. Reviews in Mineralogy and Geochemistry, Mineralogical Soc. Am., 2008, v. 69(1), p. 61-120. DOI:10.2138/rmg.2008.69.3Eq. 34 shows Cpx saturation curve of the mafic to intermediate melt; specify H2O by Totals of oxides (H2O,wt%=100-Sum of oxides,wt%) or via "H2O, wt.%" parameter in the "Other" window; only actual melt compositions to be used01
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TCpxOlDe Hoog, Gall & Cornell, 2010De Hoog J.C.M., Gall L., Cornell D.H. Trace-element geochemistry of mantle olivine and application to mantle petrogenesis and geothermobarometry // Chemical Geology, 2010, V.270(1-4), p.196-215, DOI:10.1016/j.chemgeo.2009.11.017Distribution of Ca between Ol and Cpx, compare also with Ol-Cpx barometer Kohler & Brey, 1990-P11
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TCpxOlHervig & Smith, 1982Hervig R.L., Smith J.V. Temperature-dependent distribution of Cr between olivine and pyroxenes in lherzolite xenoliths // Contrib. Mineral. Petrol., 1982, v.81(3), p.184-189, DOI: 10.1007/BF0037129511
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TCpxOlMori & Green, 1978Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100°11
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TCpxOlNikitina & Ivanov, 1992Nikitina L.P., Ivanov M.V. Geological thermobarometry based on mineral-forming reactions with solid solutions // St.-Petersburg, "Nedra". 1992, 192 p. (in Russian)11
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TCpxOlLoucks, 1996Loucks R.R. A precise olivine-augite Mg-Fe-exchange geothermometer // Contrib. Mineral. Petrol. 1996, v.125(2-3), p.140-150. DOI:10.1007/s004100050211Based on Fe-Mg distribution (experimental); extrusive and intrusive rocks with <2wt% H2O in the melt; P<10 kbar, T = 800-1250°C11
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TOpx(GrtCpxOl)Brey & Kohler, 1990cBrey G.P. & Kohler T. Geothermobarometry in Four-phase Lherzolites II. New Thermobarometers, and Practical Assessment of Existing Thermobarometers // Journal of Petrology, 1990, v.31(6), p.1353-1378Peridotites and lherzolites, based on Ca content in Opx (known as "BKN"); see also its corrected version [Nimis & Grutter, 2010a]0010
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TOpx(GrtCpxOl)Nimis & Grutter, 2010aNimis P., Grutter H. Internally consistent geothermometers for garnet peridotites and pyroxenites // Contrib. Mineral. Petrol., 2010, v.159, p.411-427, DOI 10.1007/s00410-009-0455-9Peridotites and lherzolites, based on Ca content in Opx, correction of thermometer [Brey & Kohler, 1990c]0010
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TOpxCpx(Ol)Kohler & Brey, 1990-TKohler T.P., Brey G.P. Calcium exchange between olivine and clinopyroxene calibrated as a geothermobarometer for natural peridotites from 2 to 60 kb with applications // Geochim. Cosmochim. Acta, 199O, v.54, p.2375-2388Component of Opx-Cpx-Ol geothermobarometer for peridotites110
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TOpxOlMori & Green, 1978Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100°10
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TOpxOlPodvin, 1988Podvin P. Ni-Mg partitioning between synthetic olivines and orthopyroxenes: Application to geothermometry // American Mineralogist, 1988, v.73, p.274-280Based on Ni/Mg distribution10
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TOpxOlSplMacGregor, 2015aMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 3: Al111
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TCpxOlSplMacGregor, 2015bMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 4: Al111
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TOpxOlSplMacGregor, 2015cMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 5: Cr111
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TCpxOlSplMacGregor, 2015dMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 6: Cr111
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TOlSplMacGregor, 2015eMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 9: Fe-Mg11
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TCpxSplMacGregor, 2015fMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 10: Fe-Mg11
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TOpxSplMacGregor, 2015gMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 11: Fe-Mg11
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TCpxOlMacGregor, 2015hMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 12: Fe-Mg11
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TCpxOpxMacGregor, 2015iMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 13: Fe-Mg11
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TCpxOpxMacGregor, 2015jMacGregor I.D. Empirical geothermometers and geothermobarometers for spinel peridotite phase assemblages // International Geology Review, 2015, v.57(15), p.1940-1974, DOI:10.1080/00206814.2015.1045307, DOI:10.1080/00206814.2015.1129752Reaction 14: Ca-Mg; erroneous Kd (missing brackets) used in regression?11
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TOpxOlSplWitt-Eickschen & Seck, 1991Witt-Eickschen G., Seck H.A. Solubility of Ca and Al in orthopyroxene from spinel peridotite: an improved version of an empirical geothermometer // Contrib. Mineral. Petrol., 1991, v.106(4), p.431-439, DOI:10.1007/BF00321986Al in Opx, calibrated using the [Brey & Kohler 1990c] Ca in Opx "BKN" thermometer (NB! BKN is derived for Grt peridotites!); original version; see also the corrected version [Witt-Eickschen & Seck, 1991a]111
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TOpxSpl(Ol)Witt-Eickschen & Seck, 1991aWitt-Eickschen G., Seck H.A. Solubility of Ca and Al in orthopyroxene from spinel peridotite: an improved version of an empirical geothermometer // Contrib. Mineral. Petrol., 1991, v.106(4), p.431-439, DOI:10.1007/BF00321986Al in Opx, calibrated using the [Brey & Kohler 1990c] Ca in Opx "BKN" thermometer (NB! BKN is derived for Grt peridotites!); original version; see also the corrected version [Witt-Eickschen & Seck, 1991a]; version with manually set xMg in olivine; default Fo=90 used, you can change this value using the button [Other] (placed under "Independent parameters")101
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TOpxOlSplWitt-Eickschen & Seck, 1991bWitt-Eickschen G., Seck H.A. Solubility of Ca and Al in orthopyroxene from spinel peridotite: an improved version of an empirical geothermometer // Contrib. Mineral. Petrol., 1991, v.106(4), p.431-439, DOI:10.1007/BF00321986Al in Opx, calibrated using the [Brey & Kohler 1990c] Ca in Opx "BKN" thermometer (NB! BKN is derived for Grt peridotites!), so the same correction is applied as in [Nimis & Grutter, 2010a] (DOI:10.1007/s00410-009-0455-9)111
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TOpxSpl(Ol)Witt-Eickschen & Seck, 1991cWitt-Eickschen G., Seck H.A. Solubility of Ca and Al in orthopyroxene from spinel peridotite: an improved version of an empirical geothermometer // Contrib. Mineral. Petrol., 1991, v.106(4), p.431-439, DOI:10.1007/BF00321986Al in Opx, calibrated using the [Brey & Kohler 1990c] Ca in Opx "BKN" thermometer (NB! BKN is derived for Grt peridotites!), so the same correction is applied as in [Nimis & Grutter, 2010a] (DOI:10.1007/s00410-009-0455-9); version with manually set xMg in olivine; default Fo=90 used, you can change this value using the button [Other] (placed under "Independent parameters")101
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TOlDe Hoog, Gall & Cornell, 2010 AlDe Hoog J.C.M., Gall L., Cornell D.H. Trace-element geochemistry of mantle olivine and application to mantle petrogenesis and geothermobarometry // Chemical Geology, 2010, V.270(1-4), p.196-215, DOI:10.1016/j.chemgeo.2009.11.017Non-zero contents of Al, Cr[+3] is absent or Cr[+2] is expected; Al(ppm) is calculated from its formula coefficient1
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TOlDe Hoog, Gall & Cornell, 2010 AlCrDe Hoog J.C.M., Gall L., Cornell D.H. Trace-element geochemistry of mantle olivine and application to mantle petrogenesis and geothermobarometry // Chemical Geology, 2010, V.270(1-4), p.196-215, DOI:10.1016/j.chemgeo.2009.11.017Non-zero contents of Al and Cr[+3], no Cr[+2]; Al and Cr (in ppm) are calculated from their formula coefficients1
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TOlDe Hoog, Gall & Cornell, 2010 CaDe Hoog J.C.M., Gall L., Cornell D.H. Trace-element geochemistry of mantle olivine and application to mantle petrogenesis and geothermobarometry // Chemical Geology, 2010, V.270(1-4), p.196-215, DOI:10.1016/j.chemgeo.2009.11.017Non-zero contents of Ca; Ca(ppm) is calculated from its formula coefficient1
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TOlDe Hoog, Gall & Cornell, 2010 CrDe Hoog J.C.M., Gall L., Cornell D.H. Trace-element geochemistry of mantle olivine and application to mantle petrogenesis and geothermobarometry // Chemical Geology, 2010, V.270(1-4), p.196-215, DOI:10.1016/j.chemgeo.2009.11.017Non-zero contents of Cr (Cr[+2] is not expected), presence of Al is not critical (Al-version is preferred); Cr and Al (in ppm) are calculated from their formula coefficients1