A | B | C | D | E | F | G | H | I | J | K | L | M | N | O | P | Q | R | S | T | U | V | W | X | Y | Z | AA | |
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1 | Type | Minerals | Name | Reference | Comments | Grt | Cpx | Opx | Ol | Spl | Ilm | Hbl | Crd | St | Bt | Mu | Chl | Cld | Tlc | Pl | Fsp | Ky | Sil | And | Qtz | Coe | Ru |
2 | T | GrtCpx | Ai, 1994 | Ai Y. A revision of the garnet-clinopyroxene Fe[+2]-Mg exchange geothermometer // Contrib. Mineral. Petrol., 1994, v.115, p.467-473 | Lower crust and upper mantle | 1 | 1 | ||||||||||||||||||||
3 | T | GrtCpx | Ellis & Green, 1979 | Ellis 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.13-22 | Better for T > 1200°C, uncertainty: ±40° | 1 | 1 | ||||||||||||||||||||
4 | T | GrtCpx | Krogh, 1988 | Krogh E.J. The garnet-clinopyroxene Fe-Mg geothermometer - a reinterpretation of existing experimental data // Contrib. Mineral. Petrol., 1988, v.99(1), p.44-48 | 1 | 1 | |||||||||||||||||||||
5 | T | GrtCpx | Ravna, 2000 | Ravna E.J.K. The garnet-clinopyroxene Fe[2+]-Mg geothermometer: an updated calibration // Journal of Metamorphic Geology, 2000, v.18(2), p.211-219 | Check "Use Fe[3+]" option | 1 | 1 | ||||||||||||||||||||
6 | T | GrtCpx | Mori & Green, 1978 | Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97 | Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100° | 1 | 1 | ||||||||||||||||||||
7 | T | GrtCpx | Nakamura, 2006 | Nakamura 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.102 | 1 | 1 | |||||||||||||||||||||
8 | T | GrtCpx | Nakamura, 2009 | Nakamura 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.495-508 | 1 | 1 | |||||||||||||||||||||
9 | T | GrtCpx | Nikitina & Ivanov, 1993 | Nikitina 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 geothermobarometer | 1 | 1 | ||||||||||||||||||||
10 | T | GrtCpx | Nikitina & Simakov, 1994-T | Nikitina 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.34 | Component of Grt-Cpx geothermobarometer, garnet peridotites and eclogites | 1 | 1 | ||||||||||||||||||||
11 | T | GrtCpx | Powell, 1985 | Powell R. Regression diagnostics and robust regress in geothermometer/geobarometer calibration: the garnet-clinopyroxene geothermometer revisited // Journal of Metamorphic Geology, 1985, v.3(3), p.231-243 | Preferable for T < 1200°C | 1 | 1 | ||||||||||||||||||||
12 | T | GrtCpx | Sengupta et al., 1989 | Sengupta 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.223-227 | Granulites (with low contents of Na, Al and Fe+3 in Cpx), xFe(Grt)<0.65 | 1 | 1 | ||||||||||||||||||||
13 | T | GrtCpx | Sudholz et al., 2022c | Sudholz 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/s00410-022-01944-3 | Multiple linear regression over dataset comprised of >300 peridotite, pyroxenite and eclogite experiments at P=10-70 kbar, T=850-1650°C | 1 | 1 | ||||||||||||||||||||
14 | T | Cpx(Grt) | Ashchepkov et al., 2008 | Ashchepkov 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.335-352 | Correction of [Nimis & Taylor, 2000] Cpx geothermometer | 0 | 1 | ||||||||||||||||||||
15 | T | Cpx(Grt) | Ellis & Green, 1979s | Ellis 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.13-22 | Modelled eclogitic Grt composition is used (Simakov, 2008) | 0 | 1 | ||||||||||||||||||||
16 | T | Cpx(Grt) | Nimis & Taylor, 2000-T | Nimis 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.541-554 | Component of Cpx geothermobarometer for Grt peridotites | 0 | 1 | ||||||||||||||||||||
17 | T | GrtOpx | Carswell & Harley, 1990 | Carswell D.A., Harley S.L. Mineral barometry and thermometry // In: Carswell D.A. (Ed.), Eclogite Facies Rocks, Blackie & Sous, Glasgow, 1990, p.83-110 | Garnet peridotites and eclogites | 1 | 1 | ||||||||||||||||||||
18 | T | GrtOpx | Ganguly, Cheng & Tirone, 1996 | Ganguly 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/s004100050240 | Mn-corrected version; small underestimation (ca. 2-3°) vs. GTPX-TEM.exe program of J. Ganguly is unclear | 1 | 1 | ||||||||||||||||||||
19 | T | GrtOpx | Harley, 1984 | Harley S.L. An experimental study of the partitioning of Fe and Mg between garnet and orthopyroxene // Contrib. Mineral. Petrol., 1984, v.86, p.359-373 | 1 | 1 | |||||||||||||||||||||
20 | T | GrtOpx | Lavrentieva & Perchuk, 1990 | Lavrentieva 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) | 1 | 1 | |||||||||||||||||||||
21 | T | GrtOpx | Mori & Green, 1978 | Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97 | Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100° | 1 | 1 | ||||||||||||||||||||
22 | T | GrtOpx | Nikitina et al., 2010-T | Nikitina 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% | 1 | 1 | ||||||||||||||||||||
23 | T | GrtOpx | Nimis & Grutter, 2010 | Nimis P., Grutter H. Internally consistent geothermometers for garnet peridotites and pyroxenites // Contrib. Mineral. Petrol., 2010, v.159, p.411-427, DOI 10.1007/s00410-009-0455-9 | Based on natural samples (2Px thermometer [Taylor, 1998] and Grt-Opx barometer [Nickel & Green, 1985]), uncertainty: ±34° | 1 | 1 | ||||||||||||||||||||
24 | T | GrtOpx | Sudholz et al., 2022o | Sudholz 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/s00410-022-01944-3 | Multiple linear regression over dataset comprised of >300 peridotite, pyroxenite and eclogite experiments at P=10-70 kbar, T=850-1650°C | 1 | 1 | ||||||||||||||||||||
25 | T | Grt(OpxCpx) | Boyd & Schairer, 1964a | Boyd F.R., Schairer J.F. The system MgSiO3-CaMgSi2O6 // Journal of Petrology, 1964, v.5(2), p.275-309 | Mg-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) | 1 | 0 | 0 | |||||||||||||||||||
26 | T | Grt(OpxCpx) | Boyd & Schairer, 1964b | Boyd F.R., Schairer J.F. The system MgSiO3-CaMgSi2O6 // Journal of Petrology, 1964, v.5(2), p.275-309 | Mg-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) | 1 | 0 | 0 | |||||||||||||||||||
27 | T | Grt(OpxCpx) | Davis & Boyd, 1966a | Davis 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.3567-3576 | Mg-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) | 1 | 0 | 0 | |||||||||||||||||||
28 | T | Grt(OpxCpx) | Davis & Boyd, 1966b | Davis 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.3567-3576 | Mg-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) | 1 | 0 | 0 | |||||||||||||||||||
29 | T | Grt(OpxCpx) | Lindsley & Dixon, 1976a | Lindsley D.H., Dixon S.S. Diopside-enstatite equilibria at 850°C-1400°C, 5-35 kb // American Journal of Sciences, 1976, v.276, p.1285-1301 | Mg-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) | 1 | 0 | 0 | |||||||||||||||||||
30 | T | Grt(OpxCpx) | Lindsley & Dixon, 1976b | Lindsley D.H., Dixon S.S. Diopside-enstatite equilibria at 850°C-1400°C, 5-35 kb // American Journal of Sciences, 1976, v.276, p.1285-1301 | Mg-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) | 1 | 0 | 0 | |||||||||||||||||||
31 | T | Grt(OpxCpx) | Simakov, 2012 | Simakov 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/S1028334X12060189 | Garnet peridotites, Ca, Mg, Fe and Cr in Grt accounted, uncertainty is ±150° | 1 | 0 | 0 | |||||||||||||||||||
32 | T | GrtOl | Canil, 1999 | Canil D. The Ni in garnet geothermometer: calibration at natural abundances // Contrib. Mineral. Petrol., 1999, v.136(3), p.313-324 | Grt peridotites, based on Ni distribution (in ppm) between Grt and Ol | 1 | 1 | ||||||||||||||||||||
33 | T | GrtOl | Mori & Green, 1978 | Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97 | Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100° | 1 | 1 | ||||||||||||||||||||
34 | T | GrtOl | O'Neill & Wood, 1979 | O'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.59-70 | Lherzolites | 1 | 1 | ||||||||||||||||||||
35 | T | GrtOl | Sudholz et al., 2021 | Sudholz 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/s00410-021-01791-8 | For Grt peridotites, based on Ni-exchange between Grt and Ol; calibrated at 2.25-4.5 GPa and 1100-1325°C; uncertainties 55°C | 1 | 1 | ||||||||||||||||||||
36 | T | Grt(Ol) | Sudholz et al., 2021a | Sudholz 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/s00410-021-01791-8 | For 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") | 1 | 0 | ||||||||||||||||||||
37 | T | Grt(Ol) | Canil, 1999a | Canil D. The Ni in garnet geothermometer: calibration at natural abundances // Contrib. Mineral. Petrol., 1999, v.136(3), p.313-324 | Grt 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") | 1 | 0 | ||||||||||||||||||||
38 | T | Grt(Ol) | Creighton, 2009 | Creighton S. A semi-empirical manganese-in-garnet single crystal thermometer // 9th IKC Proceedings, Part I, Lithos, 2009, v.112S, p.177-182 | For Grt xenocrysts from garnet peridotites; accuracy ±150°; corrected publication typos | 1 | 0 | ||||||||||||||||||||
39 | T | Grt(Ol) | Griffin et al., 1989 | Griffin 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.199-202 | Grt peridotites, based on Ni solubility in the coexistent Chromium Ol and Grt, 3000 ppm used for Ni content in Ol | 1 | 0 | ||||||||||||||||||||
40 | T | Grt(Ol) | Ryan, Griffin & Pearson, 1996a | Ryan 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.5611-5625 | Garnet peridotites, based on Ni distribution (in ppm) between Grt (enriched in Cr) and Ol | 1 | 0 | ||||||||||||||||||||
41 | T | Grt(Ol) | Nimis, Zanetti & Franz, 2024 | Nimis 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.2024.107513 | Pressure-dependent expression for Ni-in-garnet geothermometer | 1 | 1 | ||||||||||||||||||||
42 | T | Grt(Ol) | Nimis, Zanetti & Franz, 2024a | Nimis 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.2024.107513 | Pressure-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") | 1 | 0 | ||||||||||||||||||||
43 | T | Grt(OpxCpxOl) | Ashchepkov et al., 2008a | Ashchepkov 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.335-352 | Ordinary peridotites, based on correlation between Grt composition and temperatures estimated using Opx(GrtCpxOl) geothermometer T_BKN [Brey & Kohler, 1990] NB! Unclear errors detected! | 1 | 0 | 0 | 0 | ||||||||||||||||||
44 | T | OpxCpx | Bertrand & Mercier, 1985 | Bertrand 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.109-122 | 1 | 1 | |||||||||||||||||||||
45 | T | OpxCpx | Mori & Green, 1978 | Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97 | Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100° | 1 | 1 | ||||||||||||||||||||
46 | T | OpxCpx | Nikitina at al., 2010a | Nikitina 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) | 1 | 1 | |||||||||||||||||||||
47 | T | OpxCpx | Simakov, 2000a | Simakov S.K. The clinopyroxene thermometry of mantle peridotites: implication for diamond evaluation potential // Doklady Earth Sciences, 2000, v.375(8), p.1266-1268 | Peridotites | 1 | 1 | ||||||||||||||||||||
48 | T | OpxCpx | Simakov, 2008a | Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136 | Peridotites | 1 | 1 | ||||||||||||||||||||
49 | T | OpxCpx | Taylor, 1998 | Taylor 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.381-408 | Upper mantle peridotites and lherzolites, P=10-35 kbar, T=1050-1260°C | 1 | 1 | ||||||||||||||||||||
50 | T | OpxCpx | Wells, 1977 | Wells P.A. Pyroxene Thermometry in Simple and Complex Systems // Contrib. Mineral. Petrol., 1977, v.62, p.129-139 | 1 | 1 | |||||||||||||||||||||
51 | T | OpxCpx | Wood & Banno, 1973 | Wood B. J., Banno S. Garnet-orthopyroxene and orthopyroxene-clinopyroxene relationships in simple and complex systems // Contrib. Mineral. Petrol., 1973, v.42, p.109-124 | 1 | 1 | |||||||||||||||||||||
52 | T | OpxCpx | Putirka, 2008 | Putirka, 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, p. 61-120. | Global regression (eq. 36); perform best for mafic systems with xMg(Cpx)>0.75; uncheck "Use Fe[3+]" option | 1 | 1 | ||||||||||||||||||||
53 | T | OpxCpx | Putirka, 2008a | Putirka, 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, p. 61-120. | Regression for data with xMg(Cpx)<0.75 (eq. 37); uncheck "Use Fe[3+]" option | 1 | 1 | ||||||||||||||||||||
54 | T | Cpx(Opx) | Boyd & Schairer, 1964 | Boyd F.R., Schairer J.F. The system MgSiO3-CaMgSi2O6 // Journal of Petrology, 1964, v.5(2), p.275-309 | Mg-systems only | 1 | 0 | ||||||||||||||||||||
55 | T | Cpx(Opx) | Davis & Boyd, 1966 | Davis 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.3567-3576 | Mg-systems only | 1 | 0 | ||||||||||||||||||||
56 | T | Cpx(Opx) | Lindsley & Dixon, 1976 | Lindsley D.H., Dixon S.S. Diopside-enstatite equilibria at 850°C-1400°C, 5-35 kb // American Journal of Sciences, 1976, v.276, p.1285-1301 | Mg-systems only | 1 | 0 | ||||||||||||||||||||
57 | T | Cpx(Opx) | Simakov, 2000b | Simakov S.K. The clinopyroxene thermometry of mantle peridotites: implication for diamond evaluation potential // Doklady Earth Sciences, 2000, v.375(8), p.1266-1268 | Modelled Opx composition | 1 | 0 | ||||||||||||||||||||
58 | T | Cpx(Opx) | Simakov, 2008b | Simakov S.K. Garnet-clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites // Lithos, 2008, v.106, p.125-136 | Estimated (modelled) Opx composion | 1 | 0 | ||||||||||||||||||||
59 | T | Cpx(GrtOpx) | Mercier, 1980b | Mercier J. Single-pyroxene thermobarometry // Tectonophysics, 1980, v.70, p.1-37 | Grt peridotites | 0 | 1 | 0 | |||||||||||||||||||
60 | T | Opx(GrtCpx) | Mercier, 1980b | Mercier J. Single-pyroxene thermobarometry // Tectonophysics, 1980, v.70, p.1-37 | Grt peridotites | 0 | 0 | 1 | |||||||||||||||||||
61 | T | CpxOl | De Hoog, Gall & Cornell, 2010 | De 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.2009.11.017 | Distribution of Ca between Ol and Cpx, compare also with Ol-Cpx barometer Kohler & Brey, 1990-P | 1 | 1 | ||||||||||||||||||||
62 | T | CpxOl | Hervig & Smith, 1982 | Hervig 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/BF00371295 | 1 | 1 | |||||||||||||||||||||
63 | T | CpxOl | Mori & Green, 1978 | Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97 | Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100° | 1 | 1 | ||||||||||||||||||||
64 | T | CpxOl | Nikitina & Ivanov, 1992 | Nikitina L.P., Ivanov M.V. Geological thermobarometry based on mineral-forming reactions with solid solutions // St.-Petersburg, "Nedra". 1992, 192 p. (in Russian) | 1 | 1 | |||||||||||||||||||||
65 | T | CpxOl | Loucks, 1996 | Loucks R.R. A precise olivine-augite Mg-Fe-exchange geothermometer // Contrib. Mineral. Petrol. 1996, v.125(2-3), p.140-150. DOI:10.1007/s004100050211 | Based on Fe-Mg distribution (experimental); extrusive and intrusive rocks with <2wt% H2O in the melt; P<10 kbar, T = 800-1250°C | 1 | 1 | ||||||||||||||||||||
66 | T | Opx(GrtCpxOl) | Brey & Kohler, 1990c | Brey 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.1353-1378 | Peridotites and lherzolites, based on Ca content in Opx (known as "BKN"); see also its corrected version [Nimis & Grutter, 2010a] | 0 | 0 | 1 | 0 | ||||||||||||||||||
67 | T | Opx(GrtCpxOl) | Nimis & Grutter, 2010a | Nimis P., Grutter H. Internally consistent geothermometers for garnet peridotites and pyroxenites // Contrib. Mineral. Petrol., 2010, v.159, p.411-427, DOI 10.1007/s00410-009-0455-9 | Peridotites and lherzolites, based on Ca content in Opx, correction of thermometer [Brey & Kohler, 1990c] | 0 | 0 | 1 | 0 | ||||||||||||||||||
68 | T | OpxCpx(Ol) | Kohler & Brey, 1990-T | Kohler 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.2375-2388 | Component of Opx-Cpx-Ol geothermobarometer for peridotites | 1 | 1 | 0 | |||||||||||||||||||
69 | T | OpxOl | Mori & Green, 1978 | Mori T., Green D.H. Laboratory duplication of phase equilibria observed in natural garnet lherzolites // Journal Of Geology, 1978, v.86, p.83-97 | Garnet lherzolites, T=950-1500°C, P=30-40 kbars, uncertainty: ±100° | 1 | 0 | ||||||||||||||||||||
70 | T | OpxOl | Podvin, 1988 | Podvin P. Ni-Mg partitioning between synthetic olivines and orthopyroxenes: Application to geothermometry // American Mineralogist, 1988, v.73, p.274-280 | Based on Ni/Mg distribution | 1 | 0 | ||||||||||||||||||||
71 | T | OpxOlSpl | MacGregor, 2015a | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 3: Al | 1 | 1 | 1 | |||||||||||||||||||
72 | T | CpxOlSpl | MacGregor, 2015b | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 4: Al | 1 | 1 | 1 | |||||||||||||||||||
73 | T | OpxOlSpl | MacGregor, 2015c | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 5: Cr | 1 | 1 | 1 | |||||||||||||||||||
74 | T | CpxOlSpl | MacGregor, 2015d | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 6: Cr | 1 | 1 | 1 | |||||||||||||||||||
75 | T | OlSpl | MacGregor, 2015e | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 9: Fe-Mg | 1 | 1 | ||||||||||||||||||||
76 | T | CpxSpl | MacGregor, 2015f | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 10: Fe-Mg | 1 | 1 | ||||||||||||||||||||
77 | T | OpxSpl | MacGregor, 2015g | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 11: Fe-Mg | 1 | 1 | ||||||||||||||||||||
78 | T | CpxOl | MacGregor, 2015h | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 12: Fe-Mg | 1 | 1 | ||||||||||||||||||||
79 | T | CpxOpx | MacGregor, 2015i | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 13: Fe-Mg | 1 | 1 | ||||||||||||||||||||
80 | T | CpxOpx | MacGregor, 2015j | MacGregor 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:10.1080/00206814.2015.1129752 | Reaction 14: Ca-Mg; erroneous Kd (missing brackets) used in regression? | 1 | 1 | ||||||||||||||||||||
81 | T | OpxOlSpl | Witt-Eickschen & Seck, 1991 | Witt-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/BF00321986 | Al 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] | 1 | 1 | 1 | |||||||||||||||||||
82 | T | OpxSpl(Ol) | Witt-Eickschen & Seck, 1991a | Witt-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/BF00321986 | Al 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") | 1 | 0 | 1 | |||||||||||||||||||
83 | T | OpxOlSpl | Witt-Eickschen & Seck, 1991b | Witt-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/BF00321986 | Al 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) | 1 | 1 | 1 | |||||||||||||||||||
84 | T | OpxSpl(Ol) | Witt-Eickschen & Seck, 1991c | Witt-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/BF00321986 | Al 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") | 1 | 0 | 1 | |||||||||||||||||||
85 | T | Ol | De Hoog, Gall & Cornell, 2010 Al | De 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.2009.11.017 | Non-zero contents of Al, Cr[+3] is absent or Cr[+2] is expected; Al(ppm) is calculated from its formula coefficient | 1 | |||||||||||||||||||||
86 | T | Ol | De Hoog, Gall & Cornell, 2010 AlCr | De 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.2009.11.017 | Non-zero contents of Al and Cr[+3], no Cr[+2]; Al and Cr (in ppm) are calculated from their formula coefficients | 1 | |||||||||||||||||||||
87 | T | Ol | De Hoog, Gall & Cornell, 2010 Ca | De 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.2009.11.017 | Non-zero contents of Ca; Ca(ppm) is calculated from its formula coefficient | 1 | |||||||||||||||||||||
88 | T | Ol | De Hoog, Gall & Cornell, 2010 Cr | De 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.2009.11.017 | Non-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 coefficients | 1 | |||||||||||||||||||||
89 | T | Ol | Bussweiler et al., 2017 | Bussweiler Y., Brey G.P., Pearson D.G., Stachel T., Stern R.A., Hardman M.F., Kjarsgaard B.A., Jackson S.E. The aluminum-in-olivine thermometer for mantle peridotites - experimental versus empirical calibration and potential applications // Lithos, 2017, v.272-273, p.301-314, DOI:10.1016/j.lithos.2016.12.015 | Experimental calibration of the Al-in-Ol thermometer for Grt peridotites, harzburgites and lherzolites; accuracy ±20°C; Al(ppm) is calculated from wt% of Al2O3 | 1 | |||||||||||||||||||||
90 | T | OlIlm | Andersen & Lindsley, 1981 | Andersen D.J., Lindsley D.H. A valid Margules formulation for an asymmetric ternary solution - revision of the olivine-ilmenite thermometer, with applications // Geochim Cosmochim Acta, v.45, 1981, p.847-853 | 1 | 1 | |||||||||||||||||||||
91 | T | OlIlm | Taylor, Kamperman & Hamilton, 1998 | Taylor W.R., Kamperman M., Hamilton R. New thermobarometer and oxygen fugacity sensor calibrations for ilmenite- and chromian spinel-bearing peridotitic assemblages // Proc. VII Int. Kimb. Conf., Red. Roof. Design, Cape Town, South Africa, 1998, p.891-892 | Peridotites, P<=35 kbar, Fe[+3]/Fe[+2] - Moessbauer determination | 1 | 1 | ||||||||||||||||||||
92 | T | Ilm(Ol) | Andersen & Lindsley, 1981a | Andersen D.J., Lindsley D.H. A valid Margules formulation for an asymmetric ternary solution - revision of the olivine-ilmenite thermometer, with applications // Geochim Cosmochim Acta, v.45, 1981, p.847-853 | Default Fo=90 in olivine used, you can change this value using the button [Other] (placed under "Independent parameters") | 0 | 1 | ||||||||||||||||||||
93 | T | Ilm(Ol) | Ashchepkov et al., 2008 | Ashchepkov 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.335-352 | Based on Ol-Ilm geothermometer [Taylor, Kamperman & Hamilton, 1998] with different model Ol compositions (empirical correlations between Ol compositions and P-T parameter used); NB! This sensor may demonstrate less dP/dT than barometers for some compositions (so that intersection can not be found by iterative method); if constraints are checked then P<=35 kbar from [Taylor, Kamperman & Hamilton, 1998] will be applied | 0 | 1 | ||||||||||||||||||||
94 | T | OlSpl | Ballhaus, Berry & Green, 1991 | Ballhaus C., Berry R.F., Green D.H. High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle // Contrib. Mineral. Petrol., 1991, v.107, p.27-40 | Improved version of the geothermometer [O'Neill & Wall, 1987] | 1 | 1 | ||||||||||||||||||||
95 | T | OlSpl | Wan, Coogan, Canil, 2008 | Wan Zh., Coogan L.A., Canil D. Experimental calibration of aluminum partitioning between olivine and spinel as a geothermometer // American Mineralogist, 2008, V.93(7), p.1142-1147 | No pressure dependence (experiments at 1 bar and 1250-1450°C, Spl: xCr = 0.07-0.69, <0.1 Fe3+, <0.025Ti apfu); good analytical data required for Al2O3 (wt%) in Ol; | 1 | 1 | ||||||||||||||||||||
96 | T | OlSpl | Coogan, Saunders & Wilson, 2014 | Coogan L.A., Saunders A.D., Wilson R.N. Aluminum-in-olivine thermometry of primitive basalts: Evidence of an anomalously hot mantle source for large igneous provinces // Chemical Geology, 2014, v.368, p.1–10, DOI:10.1016/j.chemgeo.2014.01.004 | Newer version of Wan, Coogan & Canil (2008) for wider ranges of aSiO2, xCr (0-0.69) and Fe3+ (0-0.11 apfu) in Spl . No pressure dependence (experiments at 1 bar); good analytical data required for Al2O3 (wt%) in Ol | 1 | 1 | ||||||||||||||||||||
97 | T | OlSpl | Taylor, Kamperman & Hamilton, 1998 | Taylor W.R., Kamperman M., Hamilton R. New thermobarometer and oxygen fugacity sensor calibrations for ilmenite- and chromian spinel-bearing peridotitic assemblages // Proc. VII Int. Kimb. Conf., Red. Roof. Design, Cape Town, South Africa, 1998, p.891-892 | Peridotites, P<=35 kbar, Fe[+3]/Fe[+2] - Moessbauer determination | 1 | 1 | ||||||||||||||||||||
98 | T | OlSpl | Li et al., 1995 | Li J., Kornprobst J., Vielzeuf D., Fabries J. An improved experimental calibration of the olivine-spinel geothermometer // Chinese Journal of Geochemistry, 1995, v.14(1), p.68-77, DOI:10.1007/BF02840385 | Based on Fe-Mg distribution from low-P experiments | 1 | 1 | ||||||||||||||||||||
99 | T | OlSpl(Opx) | O'Neill & Wall, 1987 | O'Neill H.St.C., Wall V.J. The Olivine-Orthopyroxene-Spinel Oxygen Geobarometer, the Nickel Precipitation Curve, and the Oxygen Fugacity of the Earth's Upper Mantle // Journal of Petrology, 1987, v.28(), p.1169-1191 | 0 | 1 | 1 | ||||||||||||||||||||
100 | T | Spl(Ol) | Ballhaus, Berry & Green, 1991a | Ballhaus C., Berry R.F., Green D.H. High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle // Contrib. Mineral. Petrol., 1991, v.107, p.27-40 | Improved version of the geothermometer [O'Neill & Wall, 1987] | 0 | 1 |