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Journal articles on the topic 'Eclogite melting'

Author: Grafiati

Published: 9 March 2023

Last updated: 31 July 2025

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1

Schorn, Simon, Anna Rogowitz, and Christoph A. Hauzenberger. "Partial melting of amphibole–clinozoisite eclogite at the pressure maximum (eclogite type locality, Eastern Alps, Austria)." European Journal of Mineralogy 35, no. 5 (2023): 715–35. http://dx.doi.org/10.5194/ejm-35-715-2023.

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Abstract. Pristine amphibole–clinozoisite eclogite from within the eclogite type locality (Hohl, Koralpe) of the Eastern Alps in Austria preserves centimetre-thick, concordant, laterally continuous leucocratic segregations of coarse-grained (up to ∼ 1 cm grain diameter) euhedral amphibole–clinozoisite–quartz and disseminated garnet–omphacite–rutile. The segregations locally show selvedges dominated by coarse-grained amphibole at the interface with their host eclogite. Retrogression is limited to thin films of texturally late plagioclase ± amphibole and minor symplectites of diopside–plagioclas

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2

Gorbachev, N. S., A. V. Kostyuk, Yu B. Shapovalov, P. N. Gorbachev, A. N. Nekrasov, and D. M. Soultanov. "Critical phenomena and granatization of water-containing eclogite at P = 3,7-4,0 GPa, T = 1000-1300 °C." Доклады Академии наук 489, no. 4 (2019): 393–98. http://dx.doi.org/10.31857/s0869-56524894393-398.

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The phase relationships have been experimentally studied at eclogitization of basalts and the melting of H2O‑containing eclogite in the basalt-H2O system at P = 3,7-4,0 GPa, T = 1000-1300 C. It is established that the phase relationships depend on temperature. The formation of a supercritical fluid-melt occurs at T = 1000 C, P = 3,7 GPa, conversion eclogite-granatite occurs at T = 1000-1100 C, P = 3,9 GPa, partial melting of eclogite with the formation of Na-alkali silicate melt and clinopyroxenite restite at 1150 C and 1300 C. The supercritical fluid-melt has a high reactivity, resulting in t

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3

Kuznetsov, Maksim V., and Valery M. Savatenkov. "Melting modeling of mixed peridotitic and mafic lithologies at shallow depths of the continental metasomatized lithospheric mantle: Implementation for the Early Cretaceous volcanic rocks of Eastern Mongolia." Vestnik of Saint Petersburg University. Earth Sciences 68, no. 3 (2023): 596–617. http://dx.doi.org/10.21638/spbu07.2023.309.

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The Eastern Mongolia volcanic area formed in the Late Mesozoic–Early Cenozoic within Central Asian Orogenic Belt. The main volcanic events of the area occurred in the Early Cretaceous when alkaline basaltic lavas erupted and formed the so-called cover volcanic complex. Geochemical and isotope features of the cover volcanic complex allowed researchers to identify the following mantle rocks as their source: metasomatized peridotites, eclogites, and pyroxenites. Thermodynamic modeling in alphaMELTS program was performed to determine whether the simultaneous melting of these rocks with subsequent

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4

Dokukina, K. A., M. V. Mints, and A. N. Konilov. "Melting of eclogite facies sedimentary rocks in the Belomorian Eclogite Province, Russia." Journal of Metamorphic Geology 35, no. 4 (2016): 435–51. http://dx.doi.org/10.1111/jmg.12239.

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5

Cao, Wentao, Jane A. Gilotti, and Hans-Joachim Massonne. "Partial melting of zoisite eclogite from the Sanddal area, North-East Greenland Caledonides." European Journal of Mineralogy 32, no. 4 (2020): 405–25. http://dx.doi.org/10.5194/ejm-32-405-2020.

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Abstract. Metamorphic textures and a pressure–temperature (P–T) path of zoisite eclogite are presented to better understand the metamorphic evolution of the North-East Greenland eclogite province and this particular type of eclogite. The eclogite contained the mineral assemblage garnet, omphacite, kyanite, phengite, quartz and rutile at peak pressure. Partial melting occurred via breakdown of hydrous phases, paragonite, phengite and zoisite, based on (1) polymineralic inclusions of albite and K-feldspar with cusps into host garnet, (2) small euhedral garnet with straight boundaries against pla

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6

ShuaiQi, LIU, and ZHANG GuiBin. "Isotope fractionation during partial melting of eclogite." Acta Petrologica Sinica 37, no. 1 (2021): 95–112. http://dx.doi.org/10.18654/1000-0569/2021.01.07.

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7

Chu, Xu, Jay J. Ague, Yury Y. Podladchikov, and Meng Tian. "Ultrafast eclogite formation via melting-induced overpressure." Earth and Planetary Science Letters 479 (December 2017): 1–17. http://dx.doi.org/10.1016/j.epsl.2017.09.007.

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8

Tang, Pan, and Shun Guo. "Corundum-bearing and spinel-bearing symplectites in ultrahigh-pressure eclogites record high-temperature overprint and partial melting during slab exhumation." European Journal of Mineralogy 35, no. 4 (2023): 569–88. http://dx.doi.org/10.5194/ejm-35-569-2023.

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Abstract. Corundum- and spinel-bearing symplectites after muscovite were found in ultrahigh-pressure (UHP) eclogites from the Dabie terrane, China. Three types of symplectites were recognized based on their mineral assemblages: (1) symplectitic intergrowths of corundum + plagioclase + biotite after phengite (CPB), (2) symplectitic intergrowths of spinel + plagioclase + biotite after phengite (SPB), and (3) symplectitic intergrowths of spinel + plagioclase after paragonite (SP). The microtextures and mineral assemblages of the symplectites, in combination with the results of thermodynamic model

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9

Spetsius, Zdzislaw, Ludmila Liskovaya, Alexander Ivanov, and Irina Bogush. "FEATURES OF GARNET AND CLINOPYROXENE IN DIAMONDIFEROUS ECLOGITES FROM THE UDACHNAYA KIMBERLITE PIPE, YAKUTIA: METASOMATOSIS EVIDENCE." Ores and metals, no. 4 (February 2, 2021): 45–53. http://dx.doi.org/10.47765/0869-5997-2020-10027.

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Mineralogy of diamondiferous eclogite xenolites showing metasomatosis evidence from the Udachnaya kimberlite pipe is discussed. The paper also reviews features of diamonds they contain, compositions of primary garnets and omphacites as well as alteration of structural and species compositions of original garnets and clinopyroxenes during metasomatosis. Based on pyrope structure update, two-phase garnet composition is suggested, which is mostly represented by complex pyrope associated with Ca-pyrope. In all samples, primary omphacite is replaced by another clinopyroxene variety depleted in Na2O

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10

Litvin, Yu A., A. V. Kuzyura, and E. B. Limanov. "The role of garnetization of olivine in olivine-diopside-jadeite system in the ultramafic-mafic evolution of the upper-mantle magmatism (experiment at 6 GPa)." Геохимия 64, no. 10 (2019): 1026–46. http://dx.doi.org/10.31857/s0016-752564101026-1046.

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Peritectic mechanisms, controlling fractional ultrabasic-basic evolution of the upper mantle magmatism and genesis of the peridotitepyroxeniteeclogite rock series, are substantiated in theory and experiment. Melting phase relations of a differentiated mantle material are studied with polythhermal section method in the multicomponent olivineclinopyroxene/omphacitecorundumcoesite system with boundary compositions duplicated these of peridotitic and eclogitic minerals. The peritectic reaction of orthopyroxene and melt with formation of clinopyroxene (the opthopyroxene clinopyroxenization reaction

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11

Sobolev, Alexander V., Albrecht W. Hofmann, Dmitry V. Kuzmin, et al. "The Amount of Recycled Crust in Sources of Mantle-Derived Melts." Science 316, no. 5823 (2007): 412–17. http://dx.doi.org/10.1126/science.1138113.

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Plate tectonic processes introduce basaltic crust (as eclogite) into the peridotitic mantle. The proportions of these two sources in mantle melts are poorly understood. Silica-rich melts formed from eclogite react with peridotite, converting it to olivine-free pyroxenite. Partial melts of this hybrid pyroxenite are higher in nickel and silicon but poorer in manganese, calcium, and magnesium than melts of peridotite. Olivine phenocrysts' compositions record these differences and were used to quantify the contributions of pyroxenite-derived melts in mid-ocean ridge basalts (10 to 30%), ocean isl

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12

Schorn, Simon, Michael I. H. Hartnady, Johann F. A. Diener, Chris Clark, and Chris Harris. "H2O-fluxed melting of eclogite during exhumation: an example from the eclogite type-locality, Eastern Alps (Austria)." Lithos 390-391 (June 2021): 106118. http://dx.doi.org/10.1016/j.lithos.2021.106118.

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13

Martin, Adam P., Alan F. Cooper, Richard C. Price, Philip R. Kyle, and John A. Gamble. "Chapter 5.2b Erebus Volcanic Province: petrology." Geological Society, London, Memoirs 55, no. 1 (2021): 447–89. http://dx.doi.org/10.1144/m55-2018-80.

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AbstractIgneous rocks of the Erebus Volcanic Province have been investigated for more than a century but many aspects of petrogenesis remain problematic. Current interpretations are assessed and summarized using a comprehensive dataset of previously published and new geochemical and geochronological data. Igneous rocks, ranging in age from 25 Ma to the present day, are mainly nepheline normative. Compositional variation is largely controlled by fractionation of olivine + clinopyroxene + magnetite/ilmenite + titanite ± kaersutite ± feldspar, with relatively undifferentiated melts being generate

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14

Spetsius, Zdislav V., and Lawrence A. Taylor. "Partial Melting in Mantle Eclogite Xenoliths: Connections with Diamond Paragenesis." International Geology Review 44, no. 11 (2002): 973–87. http://dx.doi.org/10.2747/0020-6814.44.11.973.

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15

Rapp, Robert P., Nobumichi Shimizu, and Marc D. Norman. "Growth of early continental crust by partial melting of eclogite." Nature 425, no. 6958 (2003): 605–9. http://dx.doi.org/10.1038/nature02031.

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16

Laurie, Angelique, and Gary Stevens. "Water-present eclogite melting to produce Earth's early felsic crust." Chemical Geology 314-317 (July 2012): 83–95. http://dx.doi.org/10.1016/j.chemgeo.2012.05.001.

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17

Skublov, Sergey G., Aleksey V. Berezin, Xian-Hua Li, et al. "Zircons from a Pegmatite Cutting Eclogite (Gridino, Belomorian Mobile Belt): U-Pb-O and Trace Element Constraints on Eclogite Metamorphism and Fluid Activity." Geosciences 10, no. 5 (2020): 197. http://dx.doi.org/10.3390/geosciences10050197.

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This report presents new data on U-Pb geochronology, oxygen isotopes, and trace element composition of zircon from a pegmatite vein crosscutting an eclogite boudin on Stolbikha Island, Gridino area, Belomorian mobile belt (BMB). The zircon grains occur as two distinct populations. The predominant population is pegmatitic and shows dark cathodoluminescence (CL); about a third of this population contains inherited cores. The second zircon population is typical of granulite and exhibits a well-defined sectorial (mosaic) zoning in CL. Both the inherited cores and sectorial in CL zircons appear to

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18

Borghini, Alessia, Silvio Ferrero, Patrick J. O'Brien, et al. "Halogen-bearing metasomatizing melt preserved in high-pressure (HP) eclogites of Pfaffenberg, Bohemian Massif." European Journal of Mineralogy 36, no. 2 (2024): 279–300. http://dx.doi.org/10.5194/ejm-36-279-2024.

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Abstract. Primary granitic melt inclusions are trapped in garnets of eclogites in the garnet peridotite body of Pfaffenberg, Granulitgebirge (Bohemian Massif, Germany). These polycrystalline inclusions, based on their nature and composition, can be called nanogranitoids and contain mainly phlogopite/biotite, kumdykolite, quartz/rare cristobalite, a phase with the main Raman peak at 412 cm−1, a phase with the main Raman peak at 430 cm−1, osumilite and plagioclase. The melt is hydrous, peraluminous and granitic and significantly enriched in large ion lithophile elements (LILE), Th, U, Li, B and

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19

Soldner, Jérémie, Chao Yuan, Karel Schulmann, et al. "Grenvillean evolution of the Beishan Orogen, NW China: Implications for development of an active Rodinian margin." GSA Bulletin 132, no. 7-8 (2019): 1657–80. http://dx.doi.org/10.1130/b35404.1.

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Abstract New geochemical and geochronological data are used to characterize the geodynamic setting of metasediments, felsic orthogneisses, and eclogite and amphibolite lenses forming the Beishan complex, NW China, at the southern part of the Central Asian Orogenic Belt. The metasediments correspond compositionally to immature greywackes receiving detritus from a heterogeneous source involving a magmatic arc and a Precambrian continental crust. Metagranitoids, represented by felsic orthogneisses, show both composition of greywacke-derived granitic melt with incompatible trace element patterns s

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20

Shatskiy, Anton, Altyna Bekhtenova, Anton V. Arefiev, and Konstantin D. Litasov. "Melt Composition and Phase Equilibria in the Eclogite-Carbonate System at 6 GPa and 900–1500 °C." Minerals 13, no. 1 (2023): 82. http://dx.doi.org/10.3390/min13010082.

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Melting phase relations in the eclogite-carbonate system were studied at 6 GPa and 900–1500 °C. Starting mixtures were prepared by blending natural bimineral eclogite group A (Ecl) with eutectic Na-Ca-Mg-Fe (N2) and K-Ca-Mg-Fe (K4) carbonate mixtures (systems Ecl-N2 and Ecl-K4). In the Ecl-N2 system, the subsolidus assemblage is represented by garnet, omphacite, eitelite, and a minor amount of Na2Ca4(CO3)5. In the Ecl-K4 system, the subsolidus assemblage includes garnet, clinopyroxene, K2Mg(CO3)2, and magnesite. The solidus of both systems is located at 950 °C and is controlled by the followin

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21

Dobrescu, Anca. "Pre-Variscan granitoids with adakitic signature at west Getic basement of the South Carpathians (Romania): constraints on genesis and timing based on whole-rock and zircon geochemistry." Geologica Acta 19 (April 14, 2021): 1–17. http://dx.doi.org/10.1344/geologicaacta2021.19.4.

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Research on two strata-like intrusions from Slatina-Timiş (STG) and Buchin (BG) at West Getic Domain of the South Carpathians (Semenic Mountains) identified granitoids with adakitic signature in a continental collision environment. Whole-rock geochemical composition with high Na2O, Al2O3 and Sr, depleted Y (18ppm) and HREE (Yb 1.8ppm) contents, high Sr/Y (40), (La/Yb)N (10) ratios and no Eu anomalies overlaps the High-Silica Adakites (HSA) main characteristics, though there are differences related to lower Mg#, heavy metal contents and slightly increased 87Sr/86Sr ratios. Comparison with HSA,

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22

Yaxley, G. M. "The Refractory Nature of Carbonate during Partial Melting of Eclogite: Evidence from High Pressure Experiments and Natural Carbonate-Bearing Eclogites." Mineralogical Magazine 58A, no. 2 (1994): 996–97. http://dx.doi.org/10.1180/minmag.1994.58a.2.253.

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23

Vanderhaeghe, Olivier, Oscar Laurent, Véronique Gardien, et al. "Flow of partially molten crust controlling construction, growth and collapse of the Variscan orogenic belt: the geologic record of the French Massif Central." BSGF - Earth Sciences Bulletin 191 (2020): 25. http://dx.doi.org/10.1051/bsgf/2020013.

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We present here a tectonic-geodynamic model for the generation and flow of partially molten rocks and for magmatism during the Variscan orogenic evolution from the Silurian to the late Carboniferous based on a synthesis of geological data from the French Massif Central. Eclogite facies metamorphism of mafic and ultramafic rocks records the subduction of the Gondwana hyperextended margin. Part of these eclogites are forming boudins-enclaves in felsic HP granulite facies migmatites partly retrogressed into amphibolite facies attesting for continental subduction followed by thermal relaxation and

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24

Zeng, Yunchuan, Mihai N. Ducea, Jifeng Xu, Jianlin Chen, and Yan-Hui Dong. "Negligible surface uplift following foundering of thickened central Tibetan lower crust." Geology 49, no. 1 (2020): 45–50. http://dx.doi.org/10.1130/g48142.1.

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Abstract This study used clinopyroxene (cpx) compositions and zircon Hf-O isotopes of Eocene adakitic rocks (EARs) from the Qiangtang block to resolve the mechanism(s) responsible for the formation of the central Tibetan Plateau. The two leading and opposing hypotheses for the origin of these rocks are (1) partially molten foundered lower crust, and (2) partial melting of continentally subducted upper crust. The consensus is that some crustal sources within the mantle have reached eclogite facies, while evidence remains insufficient. Reverse zonation for cpx in high Mg# andesitic samples shows

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25

Klemme, Stephan, Jonathan D. Blundy, and Bernard J. Wood. "Experimental constraints on major and trace element partitioning during partial melting of eclogite." Geochimica et Cosmochimica Acta 66, no. 17 (2002): 3109–23. http://dx.doi.org/10.1016/s0016-7037(02)00859-1.

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26

Cao, Yu-ting, Liang Liu, Dan-ling Chen, et al. "Partial melting during exhumation of Paleozoic retrograde eclogite in North Qaidam, western China." Journal of Asian Earth Sciences 148 (October 2017): 223–40. http://dx.doi.org/10.1016/j.jseaes.2017.09.009.

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27

Rapp, Robert Paul, E. Bruce Watson, and Calvin F. Miller. "Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalites." Precambrian Research 51, no. 1-4 (1991): 1–25. http://dx.doi.org/10.1016/0301-9268(91)90092-o.

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28

Zhang, Peng-Fei, Yan-Jie Tang, Yan Hu, et al. "Review of melting experiments on carbonated eclogite and peridotite: insights into mantle metasomatism." International Geology Review 54, no. 12 (2012): 1443–55. http://dx.doi.org/10.1080/00206814.2012.663645.

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29

Baziotis, I., and E. Mposkos. "GEOCHEMISTRY AND TECTONIC SETTING OF ECLOGITE PROTOLITHS FROM KECHROS COMPLEX IN EAST RHODOPE (N.E. GREECE)." Bulletin of the Geological Society of Greece 43, no. 5 (2017): 2522. http://dx.doi.org/10.12681/bgsg.11659.

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Eclogites and partially amphibolitized eclogites from the metamorphic Kechros complex in East Rhodope are studied in order to provide the geodynamic framework for the origin of their protoliths. Geochemical evidence from whole rock major and trace element concentrations shows two distinct protolith groups. The low-Fe-Ti eclogites (Charakoma locality) have low-TiO2 content (<0.67 wt%), negative Nb anomalies, positive Sr anomalies, small negative Zr and Hf anomalies and variable enrichments in LILE (e.g. Rb and Ba). The REE patterns are characterized by strong LREE enrichment (LaN/YbN=5.45-5.

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30

Benmammar, Anissa, Julien Berger, Antoine Triantafyllou, et al. "Pressure-temperature conditions and significance of Upper Devonian eclogite and amphibolite facies metamorphisms in southern French Massif central." BSGF - Earth Sciences Bulletin 191 (2020): 28. http://dx.doi.org/10.1051/bsgf/2020033.

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The southwestern French Massif central in western Rouergue displays an inverted metamorphic sequence with eclogite and amphibolite facies units forming the top of the nappe stack. They are often grouped into the leptyno-amphibolite complex included, in this area, at the base of the Upper Gneiss Unit. We sampled garnet micaschists and amphibolites to investigate their metamorphic history with isochemical phase diagrams, thermobarometry and U-Pb zircon dating. Our results demonstrate that two different tectono-metamorphic units can be distinguished. The Najac unit consists of biotite-poor phengi

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31

Leitch, A. M., and G. F. Davies. "Mantle plumes and flood basalts: Enhanced melting from plume ascent and an eclogite component." Journal of Geophysical Research: Solid Earth 106, B2 (2001): 2047–59. http://dx.doi.org/10.1029/2000jb900307.

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32

Liu, Qiang, ZhenMin Jin, and JunFeng Zhang. "An experimental study of dehydration melting of phengite-bearing eclogite at 1.5–3.0 GPa." Science Bulletin 54, no. 12 (2009): 2090–100. http://dx.doi.org/10.1007/s11434-009-0140-4.

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33

Litvin, Yuriy A., Anastasiya V. Kuzyura, and Anna V. Spivak. "The Peritectic Reaction of Olivine as the Mechanism of the Ultrabasic–Basic Evolution of the Diamond-Forming Silicate-Carbonate-(C-O-H) System: Experiments at 6.0 GPa." Minerals 13, no. 8 (2023): 1040. http://dx.doi.org/10.3390/min13081040.

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Melting phase relations of the diamond-forming olivine (Ol)–jadeite (Jd)–diopside (Di)–(Mg, Fe, Ca, Na)-carbonates (Carb)–(C-O-H-fluid) system are studied in experiments at 6.0 GPa in the polythermal Ol74Carb18.5(C-O-H)7.5-Omp74Carb18.5(C-O-H)7.5 section, where Ol = Fo80Fa20, Omp (omphacite) = Jd62Di38 and Carb = (MgCO3)25(FeCO3)25(CaCO3)25(Na2CO3)25. The peritectic reaction of olivine and jadeite-bearing melts with formation of garnet has been determined as a physico-chemical mechanism of the ultrabasic–basic evolution of the diamond-forming system. During the process, the CO2 component of th

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34

de Hoÿm de Marien, Luc, Pavel Pitra, Florence Cagnard, and Benjamin Le Bayon. "Prograde and retrograde P–T evolution of a Variscan high-temperature eclogite, French Massif Central, Haut-Allier." BSGF - Earth Sciences Bulletin 191 (2020): 14. http://dx.doi.org/10.1051/bsgf/2020016.

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The P–T evolution of a mafic eclogite sample from the Haut-Allier was studied in order to constrain the dynamic of the Variscan subduction in the eastern French Massif Central. Three successive metamorphic stages M1, M2 and M3, are characterized by assemblages comprising garnet1-omphacite-kyanite, garnet2-plagioclase, and amphibole-plagioclase, respectively, and define a clockwise P–T path. These events occurred at the conditions of eclogite (M1; ∼ 20 kbar, 650 °C to ∼ 22.5 kbar, 850 °C), high-pressure granulite (M2; 19.5 kbar and 875 °C) and high-temperature amphibolite facies (M3; < 9 kba

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35

Zhu, Di-Cheng, Qing Wang, Roberto F. Weinberg, et al. "Continental Crustal Growth Processes Recorded in the Gangdese Batholith, Southern Tibet." Annual Review of Earth and Planetary Sciences 51, no. 1 (2023): 155–88. http://dx.doi.org/10.1146/annurev-earth-032320-110452.

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The continental crust in the overriding plate of the India-Asia collision zone in southern Tibet is characterized by an overthickened layer of felsic composition with an underlying granulite-eclogite layer. A large data set indicates that this crust experienced magmatism from 245 to 10 Ma, as recorded by the Gangdese Batholith. Magmatism was punctuated by flare-ups at 185−170, 90−75, and 55−45 Ma caused by a combination of external and internal factors. The growth of this crust starts with a period dominated by fractional crystallization and the formation of voluminous (ultra)mafic arc cumulat

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36

Feng, Peng, Lu Wang, Michael Brown, Tim E. Johnson, Andrew Kylander-Clark, and Philip M. Piccoli. "Partial melting of ultrahigh-pressure eclogite by omphacite-breakdown facilitates exhumation of deeply-subducted crust." Earth and Planetary Science Letters 554 (January 2021): 116664. http://dx.doi.org/10.1016/j.epsl.2020.116664.

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37

Vrabec, M., J. C. M. de Hoog, and M. Janak. "Partial melting of zoisite eclogite and its significance for trace-element cycling in subduction zones." Geochimica et Cosmochimica Acta 70, no. 18 (2006): A676. http://dx.doi.org/10.1016/j.gca.2006.06.1264.

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38

MIYAZAKI, Takahiro, Daisuke NAKAMURA, Akihiro TAMURA, Martin SVOJTKA, Shoji ARAI, and Takao HIRAJIMA. "Evidence for partial melting of eclogite from the Moldanubian Zone of the Bohemian Massif, Czech Republic." Journal of Mineralogical and Petrological Sciences 111, no. 6 (2016): 405–19. http://dx.doi.org/10.2465/jmps.151029c.

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39

Zou, Zongqi, Zaicong Wang, Stephen Foley, et al. "Origin of low-MgO primitive intraplate alkaline basalts from partial melting of carbonate-bearing eclogite sources." Geochimica et Cosmochimica Acta 324 (May 2022): 240–61. http://dx.doi.org/10.1016/j.gca.2022.02.022.

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40

Chen, Dan-Ling, Liang Liu, Yong Sun, et al. "Felsic veins within UHP eclogite at xitieshan in North Qaidam, NW China: Partial melting during exhumation." Lithos 136-139 (April 2012): 187–200. http://dx.doi.org/10.1016/j.lithos.2011.11.006.

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41

Xiong, Xiao-Lin. "Trace element evidence for growth of early continental crust by melting of rutile-bearing hydrous eclogite." Geology 34, no. 11 (2006): 945. http://dx.doi.org/10.1130/g22711a.1.

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42

Butvina, V. G., O. G. Safonov, and Yu A. Litvin. "Experimental study of eclogite melting with participation of the H2O-CO2-KCl fluid at 5 GPa." Doklady Earth Sciences 427, no. 2 (2009): 956–60. http://dx.doi.org/10.1134/s1028334x09060154.

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43

Shkodzinskiy, V. S. "Происхождение магм и вулканических взрывов в океанических и субдукционных областях с учетом данных о горячей гетерогенной аккреции Земли". Bulletin of the North-East Science Center, № 1 (28 березня 2022): 40–48. http://dx.doi.org/10.34078/1814-0998-2022-1-40-48.

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The obtained numerous proofs of hot heterogeneous accretion of the Earth and the calculated quantitative models of magmas lead to a fundamentally new solution for the genetic problems of magmatic petrology. They indicate the formation of geospheres and the initial substance of magmas resulted from fractionation of the global magmatic ocean, which arose as a result of a huge impact heat release during mantle accretion. Due to the increase in temperature as accretion progressed, a reverse geothermal gradient first existed in the mantle, and on the early Earth there were no modern geodynamic cond

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44

Drummond, M. S., M. J. Defant, and P. K. Kepezhinskas. "Petrogenesis of slab-derived trondhjemite–tonalite–dacite/adakite magmas." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 87, no. 1-2 (1996): 205–15. http://dx.doi.org/10.1017/s0263593300006611.

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ABSTRACT:The prospect of partial melting of the subducted oceanic crust to produce arc magmatism has been debated for over 30 years. Debate has centred on the physical conditions of slab melting and the lack of a definitive, unambiguous geochemical signature and petrogenetic process. Experimental partial melting data for basalt over a wide range of pressures (1–32 kbar) and temperatures (700–1150°C) have shown that melt compositions are primarily trondhjemite–tonalite–dacite (TTD). High-Al (> 15% Al2O3 at the 70% SiO2 level) TTD melts are produced by high-pressure (≥ 5 kbar) partial melting

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GAO, X. Y., Y. F. ZHENG, and Y. X. CHEN. "Dehydration melting of ultrahigh-pressure eclogite in the Dabie orogen: evidence from multiphase solid inclusions in garnet." Journal of Metamorphic Geology 30, no. 2 (2011): 193–212. http://dx.doi.org/10.1111/j.1525-1314.2011.00962.x.

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Hammouda, Tahar. "High-pressure melting of carbonated eclogite and experimental constraints on carbon recycling and storage in the mantle." Earth and Planetary Science Letters 214, no. 1-2 (2003): 357–68. http://dx.doi.org/10.1016/s0012-821x(03)00361-3.

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Liu, Qiang, and Yao Wu. "Dehydration melting of UHP eclogite and paragneiss in the Dabie orogen: Evidence from laboratory experiment to natural observation." Chinese Science Bulletin 58, no. 35 (2013): 4390–96. http://dx.doi.org/10.1007/s11434-013-6075-9.

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Litasov, Konstantin D., Anton Shatskiy, and Eiji Ohtani. "Melting and subsolidus phase relations in peridotite and eclogite systems with reduced COH fluid at 3–16 GPa." Earth and Planetary Science Letters 391 (April 2014): 87–99. http://dx.doi.org/10.1016/j.epsl.2014.01.033.

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49

Dasgupta, Rajdeep, Marc M. Hirschmann, and Nikki Dellas. "The effect of bulk composition on the solidus of carbonated eclogite from partial melting experiments at 3 GPa." Contributions to Mineralogy and Petrology 149, no. 3 (2005): 288–305. http://dx.doi.org/10.1007/s00410-004-0649-0.

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Song, Shuguang, Yaoling Niu, Li Su, Chunjing Wei, and Lifei Zhang. "Adakitic (tonalitic-trondhjemitic) magmas resulting from eclogite decompression and dehydration melting during exhumation in response to continental collision." Geochimica et Cosmochimica Acta 130 (April 2014): 42–62. http://dx.doi.org/10.1016/j.gca.2014.01.008.

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