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XII.—Petrology and Petrogenesis of some Garnetiferous Peridotites*

Published online by Cambridge University Press:  17 January 2013

M. J. O'Hara M.A., Ph.D. ,
E. L. P. Mercy Ph.D., D.I.C., F.G.S.  and
F. H. Stewart
M. J. O'Hara M.A., Ph.D.
Affiliation:
Grant Institute of Geology, University of Edinburgh
E. L. P. Mercy Ph.D., D.I.C., F.G.S.
Affiliation:
Grant Institute of Geology, University of Edinburgh
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Synopsis

Garnetiferous peridotite masses which occur among gneisses in the Tafjord district of Norway are cold intrusions emplaced as crystalline rocks late in the metamorphic history of the region. No relationship other than similarity of mineral facies can be established between the peridotites and the eclogite bodies in the surrounding gneiss. Chemical analyses of twelve olivines, fourteen orthopyroxenes, nine chrome diopsides, nine garnets, three amphiboles and two rocks are presented, representing material from the Tafjord and Almklovdalen districts of Norway, a garnetiferous peridotite mass near Bellinzona, Switzerland, and the garnet-peridotite inclusions in the kimberlite pipes of South Africa. Optical and X-ray data for the analyzed and some unanalyzed assemblages are also presented. The mineral assemblages of these rocks are compared with each other, and with data from the peridotites of layered tholeiitic intrusions, alpine-type peridotites and the peridotite nodules in basalts. The garnet-peridotites of Norway, Switzerland and South Africa are believed to be little altered fragments of the mantle, whereas the peridotite nodules in basalts and the alpine-type peridotites are believed to be of igneous origin. Examination of the distribution of cations between the coexisting phases suggests that there are too many variables to permit a reliable interpretation of the results.

The orthopyroxenes from the garnetiferous peridotites are not rich in A1203, contrary to expectations based upon recent experimental work.

Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 65 , Issue 12 , 1963 , pp. 251 - 314
Copyright
Copyright © Royal Society of Edinburgh 1963

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References

XL. References to Literature

Backlund, H. G., 1936. “Zur genetischen Deutung des Eklogits”, Geol. Rdsch., 27, 47–61.Google Scholar
Balsillie, D., 1927. “Contemporaneous Volcanic Activity in East Fife”, Geol. Mag., 64, 481–494.CrossRefGoogle Scholar
Barth, T. F. W., 1951. “The Feldspar Geologic Thermometers”, Neues Jb. Min. Geol. Paläont., 82, 143–154.Google Scholar
Birch, F., 1952. “Elasticity and Constitution of the Earth's Interior”, J. Geophys. Res., 57, 227–286.Google Scholar
Bloxam, T. W., and Allen, J. B. 1960. “Glaucophane Schist, Eclogite, and Associated Rocks from Knocknormal in the Girvan-Ballantrae Complex, South Ayrshire”, Trans. Roy. Soc. Edin., 64, 1–27.CrossRefGoogle Scholar
Bobrievich, A. P., Bondarenko, M. N., Gnevtjshev, M. A., Krasov, L. M., Smirnov, G. I. and Yurkevich, R. K., 1959. Almaznye Mestorozhdeniya Yakutii, 1–525. Ed. Sobolev, V. S.. Gosgeoltekhizdat, Moscow.Google Scholar
Bobrievich, A. P., Smirnov, G. I., and Sobolev, V. S., 1959. “An Eclogite Xenolith with Diamonds”, C.R. Acad. Sci. U.R.S.S., 126, 637–640 (Miner. Abstr., 15, 288).Google Scholar
Bovenkerk, H. P., Bundy, F. P., Hall, H. T., Strong, H. M., and Wentorf, R. H., 1959. “Preparation of Diamond”, Nature, Lond., 184, 1094–1098.CrossRefGoogle Scholar
Bowen, N. L., and Schairer, J. F., 1935. “The System FeO-MgO-SiO2”, Amer. J. Sci., 229, 151–217.Google Scholar
Bowen, N. L., and Tuttle, O. F., 1949. “The System MgO-SiO-2H2O”, Bull. Geol. Soc. Amer., 60, 439–460.CrossRefGoogle Scholar
Boyd, F. R., and England, J. L., 1959. “Pyrope”, Yearb. Carneg. Instn., 58, 83–87.Google Scholar
Boyd, F. R., and England, J. L., 1960. “Minerals of the Mantle”, Yearb. Carneg. Instn., 59, 47–52.Google Scholar
Boyd, F. R., and England, J. L., 1961. “Melting of Silicates at High Pressures”, Yearb. Carneg. Instn., 60, 113–114.Google Scholar
Brown, G. M., 1956. “The Layered Ultrabasic Rocks of Rhum, Inner Hebrides”, Phil. Trans. B, 240, 1–53.Google Scholar
Brown, G. M., 1957. “Pyroxenes from the Early and Middle Stages of Fractionation of the Skaergaard Intrusion, East Greenland”, Miner. Mag., 31, 511–543.Google Scholar
Bullard, E. C., and Griggs, D. T., 1961. “The Nature of the Mohorovičić Discontinuity”, Geophys. J., 6, 118–123.CrossRefGoogle Scholar
Cameron, E. N., and Emerson, M. E., 1959. “The Origin of Certain Chromite Deposits of the Eastern Part of the Bushveld Complex”, Econ. Geol., 54, 1151–1213.CrossRefGoogle Scholar
Camsell, C., 1911. “A New Diamond Locality in the Tulameen District, British Columbia”, Econ. Geol., 6, 604–611.CrossRefGoogle Scholar
Camsell, C., 1912. “Note on the Occurrence of Diamonds at Tulameen and Scottie Creek, near Ashcroft, British Columbia”, Summ. Rep. Geol. Surv. Can., 1911, 123–124.Google Scholar
Chevenoy, M., 1957. “Sur l'origine des éclogites de Sauviat (Creuse)”, C.R. Acad. Sci., Paris, 241, 426–428.Google Scholar
Chinner, G. A., Boyd, F. R., and England, J. L., 1960. “Physical Properties of Garnet Solid Solutions”, Yearb. Carneg. Instn., 59, 76–78.Google Scholar
Clark, S. P., 1960. “Kyanite-sillimanite Equilibrium”, Yearb. Carneg. Instn., 59, 52–55.Google Scholar
Colony, R. J., 1923. “An Unusual Quartz-diamond Intergrowth”, Amer. J. Sci., 205, 400–402.CrossRefGoogle Scholar
Correns, C. W., 1931. “Uber Diamanten mit Quartzeinlagerungen”, Z. Krist., 80, 37–44.Google Scholar
Dal Vesco, E., 1953. “Genesi e metamorfosi delle rocce basiche e ultrabasiche nell'ambiente mesozonale dell'orogene Pennidico (Cantone Ticino)”, Schweiz. Min. Petrogr. Mitt., 33, 173–480.Google Scholar
David, T. W. E., 1906. “An Occurrence of Diamonds in Matrix at Oakey Creek, near Inverell, New South Wales”, Rep. Brit. Ass., 76, 562–563.Google Scholar
Davidson, C. F., 1943. “The Archæan Rocks of the Rodil District, South Harris, Outer Hebrides”, Trans. Roy. Soc. Edin., 61, 71–112.CrossRefGoogle Scholar
Davidson, C. F., 1957. “The Diamond Fields of Yakutia”, Miner. Mag., 97, 329–337.Google Scholar
Davidson, C. F., 1962. Personal communication.CrossRefGoogle Scholar
Dawson, J. B., 1962. “Basutoland Kimberlites”, Bull. Geol. Soc. Amer., 73, 545–560.Google Scholar
Draper, D., 1924. “Additional Evidence Concerning the High Level Diamond-bearing Breccias of Diamantina, Brazil”, Trans. Geol. Soc. S. Afr., 26, 7–12.Google Scholar
Eppler, W. F., 1961. “Inclusions in Diamond”, J. Gemm., 8, 1–13.CrossRefGoogle Scholar
Ernst, T. G., 1935. “Olivinknollen der Basalte als bruchstücke alter Olivinfelse”, Nachr. Ges. Wiss. Göttingen, 4, 147–154.Google Scholar
Ernst, T. G., 1936 a. “Der Melilith-basalt des Westberges bei Hofgeismar, nördlich von Kassel, ein Assimilations-produkt ultrabasischer gesteine”, Chem. d. Erde, 10, 4, 631–666.Google Scholar
Ernst, T. G., 1936 b. “Tiefeneinschlüsse der Basalte”, Geol. Rdsch., 27, 73–74.CrossRefGoogle Scholar
Eskola, P., 1921. “On the Eclogites of Norway”, Skr. VidenskSelsk., Christ., 8, 1–118.Google Scholar
Field, D. S. M., 1949. “The Question of Diamonds in Canada”, J. Gemm., 2, 103–111.CrossRefGoogle Scholar
Flett, J. S., and Hill, R. N., 1946. “Geology of the Lizard and Meneage”, Mem. Geol. Surv. U.K. (2nd Ed.).Google Scholar
Frechen, J., 1948. “Die genese der olivinausscheidungen vom Dreiser Weiher (Eifel) und Finkenberg (Siebengebirge)”, Neues Jb. Min. Geol. Palaont., 79A, 317–406.Google Scholar
Ghose, S., 1962. “The Nature of Mg2+−Fe2+ Distribution in Some Ferromagnesian Silicate Minerals”, Amer. Min., 47, 388–394.Google Scholar
Gisolf, W. F., 1923. “On the Occurrence of Diamond as an Accessory Mineral in Olivine and Anorthite-bearing Bombs, Occurring in Basaltic Lava Ejected by the Volcano Gunung-Ruang”, Proc. Acad. Sci., Amst., 26, 510–512.Google Scholar
Green, D. H., 1961. “Ultramafic Breccias from the Musa Valley, Eastern Papua”, Geol. Mag., 98, 1–26.CrossRefGoogle Scholar
Groves, A. W., 1935. “The Charnockite Series of Uganda, British East Africa”, Quart. J. Geol. Soc. Lond., 91, 150–207.Google Scholar
Grubenmann, U., 1908. “Der granatolivinfels der Gordunotals, und seine Begleitgesteine”, Vjschr. Naturf. Ges. Zurich, 53, 129–156.Google Scholar
Gubelin, E., 1952. “Inclusions in Diamond”, J. Gemm., 3, 175–187.Google Scholar
Hess, H. H., 1938. “A Primary Peridotite Magma”, Amer. J. Sci., 235, 321–344.CrossRefGoogle Scholar
Hess, H. H., 1949. “Chemical Composition and Optical Properties of Common Clinopyroxenes”, Amer. Min., 36, 621–666.Google Scholar
Hess, H. H., 1952. “Orthopyroxenes of the Bushveld type, etc.”, Amer. J. Sci., Bowen Vol., 173–188.Google Scholar
Hess, H. H., 1955. “Serpentines, Orogeny and Epeirogeny”, Spec. Pap. Geol. Soc. Amer., 62, 391–408.Google Scholar
Hess, H. H., 1960. “The Stillwater Igneous Complex, Montana”, Mem. Geol. Soc. Amer., 80.Google Scholar
Hess, H. H., and Phillips, A. H., 1936. “Metamorphic Differentiation at Contacts Between Serpentinite and Siliceous Country Rocks”, Amer. Min., 21, 333–362.Google Scholar
Holmes, A., 1936. “A Contribution to the Petrology of Kimberlite and its Inclusions”, Trans. Geol. Soc. S. Afr., 39, 379–428.Google Scholar
Holmes, A., 1950. “Petrogenesis of Katungite and its Associates”, Amer. Min., 35, 772–792.Google Scholar
Howie, R. A., 1955. “The Geochemistry of the Charnockite Series of Madras, India”, Trans. Roy. Soc. Edin., 62, 725–768.Google Scholar
Howie, R. A., and Subramaniam, A. P., 1957. “The Paragenesis of Garnet in Charnockite, Enderbite and Related Granulites”, Miner. Mag., 31, 565–587.Google Scholar
Hytönen, K., and Schairer, J. F., 1961. “The Plane Enstatite-anorthite-diopside and its Relation to Basalts”, Yearb. Carneg. Instn., 60, 125–141.Google Scholar
Jackson, E. D., 1960. “X-ray Determinative Curve for Natural Olivine of Composition Fo80−90”, Prof. Pap. U.S. Geol. Surv., 400-B, 432–434.Google Scholar
Jackson, E. D., 1961. “Primary Textures and Mineral Associations in the Ultramafic Zone of the Stillwater Complex, Montana”, Prof. Pap. U.S. Geol. Surv., 358.Google Scholar
Ježek, B., 1927. “K nálezu diamantů v Čechách”, Horn. Věstn., 28, 433–437, 461–466.Google Scholar
Johnston, R. A. A., 1915. “A List of Canadian Mineral Occurrences”, Mem. Geol. Surv. Can., 74, 86.Google Scholar
Joplin, G. A., 1959. “On the Origin and Occurrence of Basic Bodies Associated with Discordant Bathyliths”, Geol. Mag., 96, 361–373.CrossRefGoogle Scholar
Kokta, J., and Němec, K., 1936. “Granát ultrabasickýck hornin od Černína”, Přír., 17, 176–180.Google Scholar
Kretz, R., 1961 a. “Coexisting Pyroxenes”, Geol. Mag., 98, 344–345.CrossRefGoogle Scholar
Kretz, R., 1961 b. “Some Applications of Thermodynamics to Coexisting Minerals of Variable Composition. Examples: Orthopyroxene-clinopyroxene and Orthopyroxene-garnet”, J. Geol., 69, 361–387.CrossRefGoogle Scholar
Kuno, H., 1959. “Discussion of Paper by Lovering (Letter to the Editor)”, J. Geophys. Res., 64, 1071–1072.Google Scholar
Kuno, H., 1960. “High Alumina Basalt”, J. Petrol., 1, 121–145.Google Scholar
Lacroix, A., 1894. “Etude minéralogique de la lherzolite des Pyrénées et ses phénomènes de contact”, Nouv. Arch. Mus. Hist. Nat. Paris, 6, 209–308.Google Scholar
Lacroix, A., 1900. “Les loches basiques accompagnant les lherzolites et les ophites des pyrénées”, 8th Int. Geol. Congr. Report, Paris, 806–838.Google Scholar
Lappin, M. A., 1960. “On the Occurrence of Kyanite in the Eclogites of the Selje and Aheim Districts, Nordfjord”, Norsk Geol. Tidsskr., 40, 289–296.Google Scholar
Lappin, M. A., 1962. Unpublished Ph.D. Thesis. University of Durham.Google Scholar
Lipschutz, M. E., and Anders, E., 1961. “The Record in the Meteorites—IV. Origin of Diamonds in Iron Meteorites”, Geochim. et Cosmoch. Acta., 24, 83–105.CrossRefGoogle Scholar
Lovering, J. F., 1959. “Letter to the Editor”, J. Geophys. Res., 64, 1073.Google Scholar
Macdonald, G. J. F., 1959. “Chondrites and the Chemical Composition of the Earth”, Researches in Geochemistry, 476–494. Ed. Abelson, . Wiley, New York.Google Scholar
Macgregor, A. M., 1951. “Some Milestones in the Pre-Cambrian of Southern Rhodesia”, Proc. Geol. Soc. S.Afr., 54, xxvii–lxxi.Google Scholar
Matthes, S., 1951. “Die kontaktmetamorphe Überprägung basischer kristalliner Schiefer im Kontakthof des Steinwald-Granits nördlich von Erbendorf in der bayrischen Oberpfalz”, Neues Jb. Miner. Geol. Paläont., 82, 1–82.Google Scholar
Mersh, S., 1952. “Further Study of the Majgawan Diamond Mine, Panna State, Central India”, Quart. J. Geol. Soc. India, 24, 125–132.Google Scholar
Mikheenko, V. I., and Nenashev, N. I., 1961. “Absolutnei vozrast obrazovaniya i otnositelenyi rozrast vnedreniya kimberlitov Yakutii”, Trans. 9th Sess. Comm. Geol. Age, Moscow, 146–164.Google Scholar
Miser, H. D., and Ross, C. S., 1922. “Diamond-bearing Peridotite in Pike Country, Arkansas”, Ecom. Geol., 17, 662–674.Google Scholar
Mueller, R. F., 1960. “Compositional Characteristics of Equilibrium Relations in Mineral Assemblages of a Metamorphosed Iron Formation”, Amer. J. Sci., 258, 449–497.CrossRefGoogle Scholar
Mueller, R. F., 1962. “Analysis of Relations Among Mg, Fe and Mn in Certain Metamorphic Minerals”, Geochim. et Cosmoch. Acta, 25, 267–296.CrossRefGoogle Scholar
Muir, I. D., and Tilley, C. E., 1958. “The Composition of Coexisting Pyroxenes in Metamorphic Assemblages”, Geol. Mag., 95, 403–409.Google Scholar
Muret, G., 1960. “Partie S.E. de la culmination du Romsdal, Chaîne calédonienne Norvège”, 21st Int. Geol. Congr. Report, Copenhagen, Section 19, 28–32.Google Scholar
Nockolds, S. R., 1940. “The Garabal Hill-Glen Fyne Igneous Complex”, Quart. J. Geol. Soc. Lond., 96, 451–510.CrossRefGoogle Scholar
O'Hara, M. J., 1960. “A Garnet-hornblende-pyroxene Rock from Glenelg, Inverness-shire”, Geol. Mag., 97, 145–156.Google Scholar
O'Hara, M. J., 1961. “Zoned Ultrabasic and Basic Gneiss Masses in the Early Lewisian Metamorphic Complex at Scourie, Sutherland”, J. Petrol, 2, 248–276.Google Scholar
O'Hara, M. J., 1963. “Distribution of Iron Between Coexisting Olivines and Calcium-poor Pyroxenes in Peridotites, Gabbros and Other Magnesium Environments”, Amer. J. Sci., 261, 32–46.Google Scholar
Orlov, Yu.L., 1959. “Syngenetic and Epigenetic Inclusions in the Crystals of Diamonds”, Trans. Min. Mus. Acad. Sci. U.S.S.R., 10, 103–120.Google Scholar
Pittman, E. F., 1901. The Mineral Resources of New South Wales, Geol. Surv. N.S.W. Sydney, 385–397.Google Scholar
Ramberg, H., 1952. The Origin of Metamorphic and Metasomatic Rocks. Univ. Chicago Press, Chicago.Google Scholar
Ramberg, H., and De Vore, G., 1951. “The Distribution of Fe and Mg in Coexisting Olivines and Pyroxenes”, J. Geol., 59, 193–210.Google Scholar
Ringwood, A. E., 1959. “Constitution of the Mantle—a Revision”, Geochim. et Cosmoch. Acta, 16, 192–193.Google Scholar
Ringwood, A. E., 1961. “Silicon in the Metal Phase of Enstatite Chondrites and Some Geochemical Implications”, Geochim. et Cosmoch. Acta, 25, 1–13.Google Scholar
Robertson, E. C., Birch, F., and Macdonald, G. J. F., 1957. “Experimental Determination of Jadeite Stability Relations to 25,000 bars”, Amer. J. Sci., 255, 115–137.CrossRefGoogle Scholar
Ross, C. S., Foster, M. D., and Myers, A. T., 1954. “Origin of Dunites and of Olivine-rich Inclusions in Basaltic Rocks”, Amer. Min., 39, 693–737.Google Scholar
Rothstein, A. T. V., 1958. “Pyroxenes from the Dawros Peridotite and Some Comments on their Nature”, Geol. Mag., 95, 456–462.Google Scholar
Ruckmick, J. C., and Noble, J. A., 1959. “Origin of the Ultramafic Complex at Union Bay, South Eastern Alaska”, Bull. Geol. Soc. Amer., 70, 981–1018.Google Scholar
Segnit, E. R., 1953. “Some Data on Synthetic Aluminous and Other Pyroxenes”, Miner. Mag., 30, 218–226.Google Scholar
Schairer, J. F., and Boyd, F. R., 1957. “Pyroxenes—the Join MgSiO3−CaMgSi2O6”, Yearb. Carneg. Instn., 56, 223–225.Google Scholar
Shand, S. J., 1934. “The Heavy Minerals of Kimberlite”, Trans. Geol. Soc. S. Afr., 37, 57–68.Google Scholar
Smirnov, G. I., 1959. “Mineralogy of the Siberian Kimberlites”, Int. Geol. Rev., 1, 21–39.Google Scholar
Sobolev, V. S., 1960. “Role of High Pressure in Metamorphism”, 21st Int. Geol. Congr. Report, Copenhagen, Section 14, 72–82.Google Scholar
Sørensen, H., 1954. “The Border Relations of the Dunite At Siorarssuit, Sukkertoppen District, West Greenland”, Medd. Grenland, 135, 1–49.Google Scholar
Taubeneck, W. H., 1957. “Magnesian Hornfelses in the Aureole of the Bald Mountain Bathylith, Elkhorn Mountains, N.E. Oregon”, Bull. Geol. Soc. Amer., 68, 1803.Google Scholar
Thayer, T. P., 1946. “Preliminary Chemical Correlation of Chromite with the Containing Rocks”, Econ. Geol., 41, 202–217.Google Scholar
Thayer, T. P., 1960. “Some Critical Differences between Alpine-type and Stratiform Peridotite-gabbro Complexes”, 21st Int. Geol. Congr. Report, Copenhagen, Section 13, 247–259.Google Scholar
Tilley, C. E., 1938. “Aluminous Pyroxenes in Metamorphosed Limestones”, Geol. Mag., 75, 81–86.Google Scholar
Tilley, C. E., 1947. “The Dunite Mylonites of St. Paul's Rocks (Atlantic)”, Amer. J. Sci., 245, 483–491.CrossRefGoogle Scholar
Turner, F. J., and Verhoogen, J., 1960. Igneous and Metamorphic Petrology, 2nd Ed.McGraw Hill, New York.Google Scholar
Udovchina, N. G., 1959. “K voprosy ob eklogitisatsii uletraosnovneich porod v yuzhnoj chasti khreeta marunkeu”, Voprosy Magmatizma Orala, 32, 5–18.Google Scholar
Verhoogen, J., 1940. “Les pipes de Kimberlite du Katanga”, Ann. Serv. Mines Katanga, 9, 1–49.Google Scholar
Wager, L. R., 1958. “Beneath the Earth's Crust”, Adv. Sci., 15, 31–45.Google Scholar
Wager, L. R., Brown, G. M., and Wadsworth, W. J., 1960. “Types of Igneous Cumulates”, J. Petrol., 1, 73–85.Google Scholar
Wagner, P. A., 1914. The Diamond Fields of Southern Africa, 347 pp. Transvaal Leader, Johannesburg.Google Scholar
Wagner, P. A., 1928. “The Evidence of the Kimberlite Pipes on the Constitution of the Outer Part of the Earth”, S. Afr. J. Sci., 25, 127–148.Google Scholar
Wickman, F. E., 1956. “The Cycle of Carbon and the Stable Carbon Isotopes”, Geochim. et Cosmoch. Acta, 9, 136–153.Google Scholar
Williams, A. F., 1932. The Genesis of the Diamond, 2 Vols. Benn, London.Google Scholar
Wilshire, H. G., and Binns, R. A., 1961. “Basic and Ultrabasic Xenoliths from Volcanic Rocks of New South Wales”, J. Petrol, 2, 185–208.CrossRefGoogle Scholar
Wilson, N. W., 1948. “The World's Diamond Deposits”, Miner. Mag., 79, 329–341.Google Scholar
Wilson, N. W., 1960. “The Diamond Deposits of Yakutia”, Miner. Mag., 103, 205–213.Google Scholar
Winchell, H., 1947. “Honolulu Series, Oahu, Hawaii”, Bull. Geol. Soc. Amer., 58, 1–48.Google Scholar
Winkler, H. G. F., and von Platen, H., 1960. “Experimentelle Gesteinsmetamorphose—III. Anatektische Ultrametamorphose kalkhaltiger Tone”, Geochim. et Cosmoch. Acta, 18, 294–316.Google Scholar
Winkler, H. G. F., and von Platen, H., 1961. “Experimentelle Gesteinsmetamorphose—IV. Bildung anatektischer Schmelzen aus metamorphisierten Grauwacken”, Geochim. et Cosmoch. Acta, 24, 48–69.Google Scholar
Worst, B. G., 1958. “The Differentiation and Structure of the Great Dyke of Southern Rhodesia”, Trans. Geol. Soc. S. Afr., 61, 283–354.Google Scholar
Yoder, H. S., 1955. “Role of Water in Metamorphism”, Spec. Pap. Geol. Soc. Amer., 62, 505–524.Google Scholar
Yoder, H. S., and Tilley, C. E., 1959. “Eclogites”, Yearb. Carneg. Instn., 58, 89–94.Google Scholar
Yoder, H. S., and Tilley, C. E., 1961. “Derivation of Magma Types from a Primary Magma”, Yearb. Carneg. Instn., 60, 106–113.Google Scholar
Yoder, H. S., and Tilley, C. E. 1962. “Origin of Basalt Magmas: An Experimental Study of Natural and Synthetic Rock Systems”, J. Petrol., 3, 342–532.Google Scholar