Evidence for liquid immiscibility in the upper mantle
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A range of carbonate globules in BVC xenoliths occur both as trapped inclusions within mantle minerals and in pockets between mineral grains, and are interpreted to have been deposited by primary mantle fluids.
“a range of carbonate globules in BVC xenoliths occur both as trapped inclusions within mantle minerals and in pockets between mineral grains, and are interpreted to have been deposited by primary mantle fluids (Amundsen 1987).”
From Comprehensive imaging and Raman spectroscopy of carbonate globules from Martian meteorite ALH 84001 and a terrestrial analogue from Svalbard (2007) · cites this paper as Amundsen 1987
The BVC eruptive centers have a range of different carbonate deposits, including magnesite globules similar to those found in ALH 84001.
“The BVC eruptive centers have a range of different carbonate deposits (Amundsen 1987), including magnesite globules similar to those found in ALH 84001.”
From Comprehensive imaging and Raman spectroscopy of carbonate globules from Martian meteorite ALH 84001 and a terrestrial analogue from Svalbard (2007) · cites this paper as Amundsen 1987
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Coltorti, M., Bonadiman, C., Hinton, R., Siena, F., & Upton, B. (1999) · doi:10.1093/petroj/40.1.133 · Cited by 477
“silicate–carbonatite (Amundsen, 1987) or silicate– Three main stages of volcanic activity have been recarbonatite–sulphide (Kogarko et al.”
BackgroundIonov, D., Dupuy, C., O'Reilly, S., Kopylova, M., & Genshaft, Y. S. (1993) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(93)90139-z · Cited by 380 · see citing works
Ionov, D., Bodinier, J., Mukasa, S., & Zanetti, A. (2002) · doi:10.1093/petrology/43.12.2219 · Cited by 366
Tappe, S., Foley, S., Jenner, G., Heaman, L., Kjarsgaard, B., Romer, R., Stracke, A., Joyce, N., & Hoefs, J. (2006) · Journal of Petrology · doi:10.1093/petrology/egl008 · Cited by 359 · see citing works
“Although immiscible silicate–carbonate liquids have been reported from natural mantle-derived xenoliths (Amundsen, 1987; Kogarko et al., 1995; Chalot-Prat & Arnold, 1999; van Achterbergh et al., 2004), they have been experimentally produced predominantly at crustal pressures.”
BackgroundCarbonate Melts and Carbonatites
Jones, A. P., Genge, M., & Carmody, L. (2013) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2013.75.10 · Cited by 334 · see citing works
“Immiscible melt fractions of CO 2 -saturated silicate melts (Freestone and Hamilton 1980; Amundsen 1987; Kjarsgaard and Hamilton 1988, 1989; Brooker and Hamilton 1990; Kjarsgaard and Peterson 1991; Church and Jones 1995; Lee and Wyllie 1997; Dawson 1998; Halama et al. 2005; Brooker and Kjarsgaard…”
BackgroundBrooker, R., & Kjarsgaard, B. (2011) · doi:10.1093/petrology/egq081 · Cited by 254
Silicate-melt inclusions in magmatic rocks: applications to petrology
Frezzotti, M. (2001) · doi:10.1016/s0024-4937(00)00048-7 · Cited by 245
Fluid inclusions in mantle xenoliths
Andersen, T., & Neumann, E. (2001) · doi:10.1016/s0024-4937(00)00049-9 · Cited by 225
Fluid inclusion evidence for immiscibility in magmatic differentiation
Roedder, E. (1992) · doi:10.1016/0016-7037(92)90113-w · Cited by 222
Worldwide occurrence of silica-rich melts in sub-continental and sub-oceanic mantle minerals
Schiano, P., & Clocchiatti, R. (1994) · Nature · doi:10.1038/368621a0 · Cited by 212
Residence of trace elements in metasomatized spinel lherzolite xenoliths: a proton-microprobe study
O'Reilly, S., Griffin, W. L., & Ryan, C. (1991) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00687203 · Cited by 199 · see citing works
Temporal evolution of mantle sources during continental rifting: The volcanism of Djibouti (Afar)
Deniel, C., Vidal, P., Coulon, C., Vellutini, P., & Piguet, P. (1994) · Journal of Geophysical Research Atmospheres · doi:10.1029/93jb02576 · Cited by 178 · see citing works
McInnes, B., & Cameron, E. M. (1994) · doi:10.1016/0012-821x(94)90055-8 · Cited by 177
Lee, W.-J., & Wyllie, P. (1998) · doi:10.1093/petroj/39.3.495 · Cited by 155
Melilitites: partial melts of the thermal boundary layer?
Wilson, M., Rosenbaum, J., & Dunworth, E. (1995) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00307280 · Cited by 142 · see citing works
Lee, W.-J., & Wyllie, P. (1997) · doi:10.1007/s004100050261 · Cited by 133
“Evidence for the existence of carbonate-rich liquids in the mantle includes silicate and carbonate immiscible liquid textures in mantle xenoliths (Amundsen 1987; Ionov et al. 1993; Pyle and Haggerty 1994; Kogarko et al. 1995).”
BackgroundKogarko, L., Henderson, C. M., & Pacheco, H. (1995) · doi:10.1007/bf02688242 · Cited by 120
Steele, A., Fries, M. D., Amundsen, H. E. F., Mysen, B. O., Fogel, M. L., Schweizer, M., & Boctor, N. Z. (2007) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2007.tb00590.x · Cited by 117 · see citing works
“used to infer a multiple depositional origin for the carbonate globules (Saxton et al. 1998). Conversely, the BVC globule samples are known to have formed from a single event during the time of the eruption of Sverrefjell volcano about 1 Myr ago. BVC carbonate chemistry (Fig. 3) varies as widely as in ALH 84001, thus…”
BackgroundMethodInfluentialSelf-citationCO2, carbonate-rich melts, and brines in the mantle
Frezzotti, M., & Touret, J. (2014) · Geoscience Frontiers · doi:10.1016/j.gsf.2014.03.014 · Cited by 114 · see citing works
“The same possibly has been described for carbonate aggregates in mantle xenoliths from Spitsbergen interpreted as being the result of mantle immiscibility processes between carbonate-rich and silicate-rich melts (Amundsen, 1987), though this still to be unanimously accepted by the scientific community.”
BackgroundXie, Y.-L., Li, Y., Hou, Z., Cooke, D., Danyushevsky, L., Dominy, S., & Yin, S.-P. (2015) · doi:10.1016/j.oregeorev.2014.10.027 · Cited by 106
“Introduction Carbonatite, a special type of magmatic rock sourced from the mantle (Le Bas, 1987; Gittins, 1989; Simonetti and Bell, 1994a, b, 1995; Somonetti et al et al, 1995, 1997, 1998; Bell et al, 1999 and the reference there in) provides important information on mantle heterogeneity, mantle metasomatism (Lev et a…”
BackgroundHaggerty, S. (1995) · doi:10.1016/0264-3707(95)00016-3 · Cited by 106
Lorand, J., Delpech, G., Grégoire, M., Moine, B., O'Reilly, S., & Cottin, J. (2004) · doi:10.1016/j.chemgeo.2004.04.012 · Cited by 102
Amundsen, H., Griffin, W., & O'Reilly, S. (1987) · doi:10.1016/0040-1951(87)90095-3 · Cited by 95
Self-citationLaumonier, M., Gaillard, F., & Sifré, D. (2015) · Chemical Geology · doi:10.1016/j.chemgeo.2014.09.019 · Cited by 93 · see citing works
“Hydrous fluids is related to the dehydration (+/- melting) of hydrous phases from the subducting slab (Amundsen, 1987; Baker et al., 1995; Schiano et al., 1995; Chazot et al., 1996; Wulff-Pedersen et al., 1996; Hirschmann et al., 1998; Hermann & Green, 2001; Scaillet & Prouteau, 2001; Klemme et al., 2002; Ishimaru et…”
BackgroundSchiano, P., & Bourdon, B. (1999) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(99)00074-6 · Cited by 85 · see citing works
Mantle Sulfides and their Role in Re–Os and Pb Isotope Geochronology
Harvey, J., Warren, J., & Shirey, S. (2016) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2016.81.10 · Cited by 83 · see citing works
“2; White 1966; Vakhrutshev and Prokoptsev 1972; MacRae 1979; Pasteris 1981; Amundsen 1987), garnet peridotite (e.g., Bishop et al. 1975; Meyer and Tsai 1979) and pyroxenite xenoliths (e.g., O’Reilly and Griffin 1987; Wilshire et al. 1988).”
BackgroundSchiano, P., Clocchiatti, R., & Joron, J. (1992) · doi:10.1016/0012-821x(92)90170-z · Cited by 79
The system CaO-MgO-SiO2-CO2 at 1 GPa, metasomatic wehrlites, and primary carbonatite magmas
Lee, W.-J., & Wyllie, P. (2000) · doi:10.1007/s004100050558 · Cited by 78
Lee, W.-J., & Wyllie, P. (1996) · doi:10.1093/petrology/37.5.1125 · Cited by 78
Carbonatite melt in oceanic upper mantle beneath the Kerguelen Archipelago
Moine, B., Grégoire, M., O'Reilly, S., Delpech, G., Sheppard, S., Lorand, J., Renac, C., Giret, A., & Cottin, J. (2004) · doi:10.1016/j.lithos.2003.12.019 · Cited by 76
Xu, Y.-G., Mercier, J., Menzies, M., Ross, J. V., Harte, B., Lin, C.-Y., & Shi, L.-B. (1996) · doi:10.1007/s004100050231 · Cited by 74
“Relatively high Ca concentrations in ol phenocrysts could be interpreted as reflecting the high content of CaO in parental melts andyor low pressure and rapid crystallization (Simkin and Smith 1970; Stormer 1973; Adams and Bishop 1986 ).”
BackgroundTreiman, A., Amundsen, H., Blake, D., & Bunch, T. (2002) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(02)00998-6 · Cited by 72 · see citing works
Self-citationHansteen, T., Andersen, T., Neumann, E., & Jelsma, H. (1991) · doi:10.1007/bf00310710 · Cited by 67
Bali, E., Szabó, C., Vaselli, O., & Török, K. (2002) · doi:10.1016/s0024-4937(01)00075-5 · Cited by 65
“Primary carbonates have been observed in upper mantle xenoliths or peridotite massifs (e.g. Amundsen, 1987; Ionov et al., 1993, 1996; Varela et al., 1998; Charlot-Prat and Arnold, 1999; Zanetti et al., 1999; Laurora et al., 2001).”
BackgroundQuantification of dissolved CO2 in silicate glasses using micro-Raman spectroscopy
Morizet, Y., Brooker, R., Iacono-Marziano, G., & Kjarsgaard, B. (2013) · American Mineralogist · doi:10.2138/am.2013.4516 · Cited by 64 · see citing works
“In addition, silicate glass is constantly being discovered in mantle xenoliths where it is sometime associated with carbonates (Amundsen 1987; Pyle and Haggerty 1994; Kogarko et al. 2001; Laurora et al. 2001; Hurai et al. 2007).”
BackgroundSkjelkvåle, B., Amundsen, H., O'Reilly, S., Griffin, W., & Gjelsvik, T. (1989) · Journal of Volcanology and Geothermal Research · doi:10.1016/0377-0273(89)90110-8 · Cited by 64 · see citing works
Self-citationGenesis and evolution of the lithospheric mantle beneath the Buffalo Head Terrane, Alberta (Canada)
Aulbach, S., Griffin, W., O'Reilly, S., & Mccandless, T. (2004) · Lithos · doi:10.1016/j.lithos.2004.04.020 · Cited by 62 · see citing works
“8) is similar to volatile-rich ultramafic liquids that occur in spinel lherzolites from Spitsbergen and are interpreted to have exsolved from a primitive volatile-rich magma due to liquid immiscibility (Amundsen, 1987).”
BackgroundEvolution of peralkaline calcite carbonatite magma in the Fen complex, southeast Norway
Andersen, T. (1988) · doi:10.1016/0024-4937(88)90019-9 · Cited by 59
Pyle, J., & Haggerty, S. (1994) · doi:10.1016/0016-7037(94)90174-0 · Cited by 58
Revision of the CaCO3–MgCO3 phase diagram at 3 and 6 GPa
Shatskiy, A., Podborodnikov, I., Arefiev, A., Minin, D. A., Chanyshev, A., & Litasov, K. (2018) · doi:10.2138/am-2018-6277 · Cited by 57
“…xenoliths (Amundsen 1987; Ionov et al. 1993, 1996; Kogarko et al. 1995) and as inclusions in kimberlitic diamonds (Meyer and McCallum 1986; Bulanova and Pavlova 1987; Phillips and Harris 1995; Wang et al. 1996; Sobolev et al. 1997; Stachel et al. 1998; Shatsky et al. 2008; Zedgenizov et…”
BackgroundMelts in the mantle modeled in the system CaO-MgO-SiO2-CO2 at 2.7 GPa
Lee, W.-J., Huang, W.-L., & Wyllie, P. (2000) · doi:10.1007/s004100050557 · Cited by 54
Wang, Z.-H., Ge, W., Yang, H.-T., Bi, J.-H., Ji, Z., Dong, Y.-C., & Xu, W.-L. (2017) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2016.09.021 · Cited by 50 · see citing works
Morishita, T., Arai, S., & Tamura, A. (2003) · doi:10.1016/s0024-4937(03)00046-x · Cited by 49
Frezzotti, M., Touret, J., & Neumann, E. (2002) · doi:10.1127/0935-1221/2002/0014-0891 · Cited by 49
Carbonates of the magnesite–siderite series from four carbonatite complexes
Buckley, H. A., & Woolley, A. (1990) · Mineralogical magazine · doi:10.1180/minmag.1990.054.376.06 · Cited by 48 · see citing works
“The discovery in spinel lherzolite xenoliths from Spitsbergen by Amundsen (1987) of evidence of three quenched liquids, of which one is carbonatitic and consists of co-existing dolomite and magnesite, is a further indication that dolomite-magnesite liquids are present at mantle depths.”
BackgroundInfluentialPowell, W., & O'Reilly, S. (2007) · Lithos · doi:10.1016/j.lithos.2006.06.010 · Cited by 45 · see citing works
Chalot-Prat, F., & Arnold, M. (1999) · doi:10.1016/s0024-4937(98)00067-x · Cited by 45
“.Fig. 13 . These later observations are not original inasmuch as pure calcite droplets or patches in veinlets of mantle xenoliths have already been reported . . by Amundsen 1987 , Ionov et al. 1993 , Pyle and . . Haggerty 1994 , Kogarko et al. 1995a and Xu et . al. 1996 . Juvenile sovite globules have also been”
BackgroundInfluentialDelpech, G., Grégoire, M., O'Reilly, S., Cottin, J., Moine, B., Michon, G., & Giret, A. (2004) · doi:10.1016/j.lithos.2003.12.018 · Cited by 44
“The characteristic features of carbonatitic metasomatism have been inferred from systematic studies of mantle xenoliths from many worldwide occurrences (Amundsen, 1987; Kogarko et al., 1995; Hauri et al., 1993, Ionov et al., 1993, Rudnick et al., 1993; Coltorti et al., 1999).”
BackgroundGriffin, W., Nikolic, N., O'Reilly, S., & Pearson, N. (2012) · Lithos · doi:10.1016/j.lithos.2012.03.003 · Cited by 43 · see citing works
High-temperature carbonate minerals in the Stillwater Complex, Montana, USA
Aird, H., & Boudreau, A. (2013) · Contributions to Mineralogy and Petrology · doi:10.1007/s00410-013-0913-2 · Cited by 40
“If a carbonatitic melt were the source for the Stillwater assemblages, excess apatite ought to be observed in association with the carbonates, as they are in carbonate assemblages in mantle xenoliths (Amundsen 1987; Yaxley et al. 1991; Hauri et al. 1993; Ionov et al. 1993, 1996; Kogarko et al. 1995; Ionov 1998; Blundy…”
BackgroundSolovova, I., Girnis, A., Kogarko, L., Kononkova, N., Stoppa, F., & Rosatelli, G. (2005) · doi:10.1016/j.lithos.2005.03.022 · Cited by 40
Choi, S., Suzuki, K., Mukasa, S., Lee, J., & Jung, H. (2010) · doi:10.1016/j.epsl.2010.06.013 · Cited by 39
“Previous work on these xenoliths mainly focused on the nature of metasomatism: processes, sources, and melt–fluid compositions (Amundsen, 1987; Ionov et al., 1993, 1996, 2002a,b).”
BackgroundChakhmouradian, A., & Zaitsev, A. (2004) · doi:10.1180/mss.10.08 · Cited by 32
CHeAr variations within a dunite nodule as a function of fluid inclusion morphology
Burnard, P., Stuart, F., & Turner, G. (1994) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(94)90148-1 · Cited by 28 · see citing works
Rare earth elements deposits in China: Spatio-temporal distribution and ore-forming processes
Xie, Y.-L., Xia, J., Cui, K., Qu, Y.-W., Liang, P., & Zhong, R. (2020) · Chinese Science Bulletin · doi:10.1360/tb-2020-0371 · Cited by 27
Shatskiy, A., Bekhtenova, A., Arefiev, A., Podborodnikov, I., Vinogradova, Y. G., Rezvukhin, D., & Litasov, K. (2022) · Gondwana Research · doi:10.1016/j.gr.2021.07.023 · Cited by 24 · see citing works
Hudon, P., Jung, I., & Baker, D. (2004) · doi:10.1029/2003jb002659 · Cited by 20
“However, immiscibility has been reported in more exotic rocks, such as impact glasses [Dence et al., 1974; Zolensky and Koeberl, 1991; Pratesi et al., 2002] and mantle xenoliths [ Amundsen, 1987; Pyle and Haggerty, 1994].”
BackgroundHong, J., Khan, T., Li, W.-Y., Khalil, Y. S., Narejo, A. A., Rashid, M. U., & Zeb, M. J. (2021) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2021.104547 · Cited by 18
Phonolitic melt production by carbonatite Mantle metasomatism: evidence from Eger Graben xenoliths
Loges, A., Schultze, D., Klügel, A., & Lucassen, F. (2019) · Contributions to Mineralogy and Petrology · doi:10.1007/s00410-019-1630-2 · Cited by 16
“1993) also contain an unusual glass phase, rich in SiO2, MgO and FeO, which Amundsen (1987) calls “ultramafic melt” and Ionov et al.”
BackgroundResultInfluentialHong, J., Ji, W., Yang, X.-Y., Khan, T., Wang, R., Li, W.-Y., & Zhang, H.-S. (2019) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2019.03.009 · Cited by 16 · see citing works
Safonov, O., & Butvina, V. (2013) · Petrology · doi:10.1134/s0869591113060076 · Cited by 16
Buikin, A., Solovova, I., Verchovsky, A., Kogarko, L., & Averin, A. A. (2014) · Geochemistry International · doi:10.1134/s0016702914100036 · Cited by 15
“The possibility that such inclusions can occur in the upper mantle was demonstrated in [19, 38, 39, 46, 47].”
BackgroundBurnard, P., Toplis, M., & Medynski, S. (2010) · doi:10.1016/j.gca.2009.11.031 · Cited by 15
Wilshire, H., & Mcguire, A. (1996) · doi:10.1007/s004100050162 · Cited by 15
“…and Green 1974; Padovani and Carter 1977); (4) to heating by proximity to intrusions in the xenolith source area (Stapleton 1991); (5) to general heating – related to rifting – of the source area (Jones et al. 1983a); (6) to heating by unspecified causes (Kuo and Essene 1986; Amundsen 1987a, b).”
BackgroundKogarko, L. (1997) · Mineralogical magazine · doi:10.1180/minmag.1997.061.407.07 · Cited by 14
“Recent studies of the geochemistry of mantle nodules and primary mantle carbonates have led to the conclusion that carbonatite magmas may be generated in the mantle (Amundsen, 1987; Pyle and Haggerty, 1994; Kogarko et al., 1995).”
BackgroundBucher-Nurminen, K. (1990) · Chemical Geology · doi:10.1016/0009-2541(90)90283-d · Cited by 14 · see citing works
Kibret, B., Ayele, A., & Keir, D. (2019) · Journal of African Earth Sciences · doi:10.1016/j.jafrearsci.2018.11.005 · Cited by 13
Zr/Hf IN CARBONATITES AND ALKALINE ROCKS: NEW DATA AND A RE-EVALUATION
de Andrade, F. R. D., Möller, P., & Dulski, P. (2008) · doi:10.5327/rbg.v32i3.991 · Cited by 13
Relationship between light rare earth deposits and mantle processes in Panxi rift, China
Niu, H.-C., Qiang, S., Chen, X.-M., & Zhang, H. (2003) · Science in China Series D Earth Sciences · doi:10.1360/03dz9026 · Cited by 13
Interfacial tension in immiscible mixtures of alkali halides.
Lockett, V. N., Rukavishnikova, I., Stepanov, V., & Tkachev, N. (2010) · Physical Chemistry, Chemical Physics - PCCP · doi:10.1039/b917694b · Cited by 12
Stern, J., McAdam, A., ten Kate, I., Bish, D., Blake, D., Morris, R., Bowden, R., Fogel, M., Glamoclija, M., Mahaffy, P., et al. (2013) · Icarus · doi:10.1016/j.icarus.2012.07.010 · Cited by 11 · see citing works
“alteration of these carbonates, may have also changed the isotopic signatures encoded during the original precipitation event (Amundsen, 1987; Treiman et al., 2002).”
BackgroundSelf-citationDuan, X.-Z., Sun, H., Yang, W., Su, B., Xiao, Y.-L., Hou, Z.-H., & Shi, H. (2014) · doi:10.1080/00206814.2013.873357 · Cited by 9
“…et al. 1998; Goodrich et al. 2001; Yaxley et al. 2004; Frezzotti et al. 2009; Ladenberger et al. 2009), magmatic immiscibility (Roedder 1984, 1992; Amundsen 1987; Schiano et al. 1994; Frezzotti et al. 2002; Hidas et al. 2010), recycling of subducted crustal material (Yang et al. 2001; Durance,…”
BackgroundSubmarine Alkalic Through Tholeiitic Shield-Stage Development of KīLauea Volcano, Hawai'i
Sisson, T., Lipman, P., & Naka, J. (2013) · doi:10.1029/gm128p0193 · Cited by 9
Varela, M. E., Clocchiatti, R., Massare, D., & Schiano, P. (1998) · doi:10.1007/bf01173765 · Cited by 8
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“Textural features like a globular shape of carbonate inclusions and curved menisci have been interpreted by several authors as an evidence for quenched liquids (Amundsen 1987; Brooker and Hamilton 1990; Pyle and Haggerty 1994; Kogarko et al. 1995).”
BackgroundHurai, V., Huraiová, M., Habler, G., Horschinegg, M., Milovský, R., Milovská, S., Hain, M., & Abart, R. (2022) · Mineralogy and Petrology · doi:10.1007/s00710-022-00783-1 · Cited by 6 · see citing works
“1 3 xenoliths, xenocrysts in alkali basalts, kimberlites, melilitites, lamprophyres, and extrusive carbonatites (Amundsen 1987; Schiano et al. 1994; Ionov et al. 1993, 1994, 1996; Seifert and Thomas 1995; Chalot-Prat and Arnold 1999; Moine et al. 2004; van Achterbergh et al. 2004; Rosatelli et al. 2007; Hurai et al. 2…”
BackgroundToscani, L., Salvioli-Mariani, E., Mattioli, M., Tellini, C., Boschetti, T., Iacumin, P., & Selmo, E. (2020) · doi:10.1016/j.lithos.2019.105288 · Cited by 6
Varela, M., Kurat, G., Clocchiatti, R., & Schiano, P. (1998) · doi:10.1111/j.1945-5100.1998.tb01711.x · Cited by 6
Wang, C., Ge, X., Fan, H.-Q., Yang, F., Hu, Q.-D., & Li, J.-G. (2022) · Journal of Materials Science & Technology · doi:10.1016/j.jmst.2022.10.026 · Cited by 5
Fluids and Melts in the Upper Mantle
Xia, L.-Q., Xia, Z.-C., & Xu, X.-Y. (1999) · doi:10.1111/j.1755-6724.1999.tb00841.x · Cited by 4
Kim, N., Choi, S., & Dale, C. (2016) · doi:10.1016/j.lithos.2015.11.033 · Cited by 3
Oppenheimer, J., Patel, K., Lindoo, A., Hillman, E., & Lev, E. (2021) · Geochemistry Geophysics Geosystems · doi:10.1029/2020gc009410 · Cited by 2
“In the upper mantle, flow of immiscible carbonate and silicate melts has been identified, for example, in samples of upper mantle eclogites (Pyle & Haggerty, 1994) and other xenoliths (Amundsen, 1987).”
BackgroundPierozzi, A., Faulkner, N., Szucs, A. M., Terribili, L., Maddin, M., Meloni, F., Devkota, K., Zubovic, K. P., Guyett, P. C., & Rodriguez-Blanco, J. D. (2025) · Carbon Capture Science & Technology · doi:10.1016/j.ccst.2025.100510 · Cited by 1 · see citing works
- Authors
- Amundsen, H. E. F.
- Corresponding author
- Amundsen, Hans E. F.
- Venue
- Nature
- Published
- 1987-06
- Volume
- 327
- Issue
- 6124
- Pages
- 692-695
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W2048417949
- Cited by
- 92
- References
- 7
- Citations by year
- 2025: 1 · 2024: 1 · 2023: 1 · 2022: 2 · 2021: 3 · 2020: 1 · 2019: 3 · 2018: 2 · 2017: 1 · 2016: 2 · 2015: 4 · 2014: 5 · 2013: 4 · 2012: 2
- FWCI
- 1.95
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Keywords
- liquid immiscibility, upper mantle, mantle xenoliths, metasomatism, apatite, phlogopite, mantle heterogeneity
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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