Abstract
The almandine-bearing biotite-cordierite-labradorite dacite of the Cerro del Hoyazo is part of the Neogene volcanic range in SE Spain, extending roughly from Cabo de Gata to Cartagena.
About 1 vol. % of the lava consists of rock inclusions, measuring over 1 cm, made up of almandine-biotite-sillimanite gneiss, quartz-cordierite gneiss and spinel-cordierite rock. On the ground of their abundance, chemical composition, mineral content and structure, the first and the second type are interpreted as restite inclusions and the third type as recrystallized restite. These restites and the dacitic magma were derived syngenetically from a (semi-) pelitic rock sequence by means of anatexis: the (semi-)pelitic rocks separated into a granitoid melt and Al-rich restites. Euhedral almandine crystals found in the glass base of the dacite have a pre-magmatic origin, and may be compared directly to those in the restites.
Another type of inclusion is represented by basic igneous rocks of varying grain size, comprising mainly basaltoid rocks and quartz-rich gabbros. These inclusions commonly bear some restite fragments of the kind mentioned above, and therefore are interpreted as representing basic magma of deeper origin that has absorbed some anatectic material. In part, the composite basic melt thus formed crystallized under plutonic conditions and fragments of the resulting quartz-rich gabbro were incorporated in a later stage in the dacitic melt. Another portion of the composite basic magma was incorporated in the dacitic melt (probably shortly before the eruption of the dacitic magma) as magma blebs (Ø ≅1–20 cm) which subsequently crystallized in part, some of them showing a comparatively fine-grained border zone.
Two possible hypotheses are suggested for the time relation between the anatexis of the (semi-) pelitic complex and the appearance of the basic magma: (a) the anatexis was of a regional nature, and was in progress when the basic magma entered the stage (and assumedly triggered the eruption of the granitoid magma); (b) the regional anatexis took place considerably earlier and the basic magma intruded an essentially solid migmatite complex, which was then melted down (contact anatexis) and subsequently erupted.
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References
Bordet, P.: Courbes pour la détermination des feldspaths plagioclases haute température et basse température, dans la zone perpendicular à g' (010). Bull. Soc. Franç. Minéral. Crist. 86, 206–207 (1963).
Brown, G. M.: Melting relations of Tertiary granitic rocks in Skye and Rhum. Mineral. Mag. 33, 533–562 (1963).
Burri, C., Parga-Pondal, I.: Neue Beiträge zur Kenntnis des granat-führenden Cordieritandesites vom Hoyazo bei Nijar (Provinz Almería, Spanien). Schweiz. Mineral. Petrog. Mitt. 16, 226–262 (1936).
Dietrich, R. V., Mehnert, K. R.: Proposal for the nomenclature of migmatites and associated rocks. Report Int. Geol. Congr., 1960, Part 26, 56–67 (1961).
Glanchaud, L., Letolle, R.: La théorie des deux magmas fondamentaux dans le volcanisme intracontinental et l'évolution géochimique des lavas du Mont-Dore (France). Geol. Rundschau 55, 316–329 (1965).
Green, T. H., Ringwood, A. E.: Origin of the calc-alkaline igneous rock suite. Earth Plan. Sci. Lett. 1, 307–316 (1966).
—: Genesis of the calc-alkaline rocks. Contr. Mineral. and Petrol. 18, 105–162 (1968a).
—: Origin of garnet phenocrysts in calc-alkaline rocks. Contr. Mineral. and Petrol. 18, 163–174 (1968b).
Gribble, C. D.: The cordierite-bearing rocks of the Haddo House and Arnage Districts, Aberdeenshire. Contr. Mineral. and Petrol. 17, 315–330 (1968).
—, O'Hara, M. J.: Interaction of basic magma with pelitic materials. Nature 214, 1198–1201 (1967).
Hawkes, D. D.: Order of abundant crystal nucleation in a natural magma. Geol. Mag. 104, 473–486 (1967).
Holmes, A.: The origin of igneous rocks. Geol. Mag. 69, 543–558 (1932).
Kuno, H.: Differentiation of basalt magmas. In: Basalts (The Poldervaart treatise on rocks of basaltic composition, New York etc.: Interscience), vol. 2, p. 623–688 (1968).
Marinelli, G.: Genèse des magmas du volcanisme plioquaternaire des Apennins. Geol. Rundschau 57, 127–141 (1967).
Mehnert, K. R.: Der gegenwärtige Stand des Granitproblems. Fortschr. Mineral. 37, 117–206 (1959).
—: Petrographie und Abfolge der Granitisation im Schwarzwald, III. Neues Jahrb. Mineral., Abhandl. 98, 208–249 (1962).
—: Petrographie und Abfolge der Granitisation im Schwarzwald, IV. Neues Jahrb. Mineral., Abhandl. 99, 161–199 (1963).
Osann, A.: 5. Über den Cordierit führenden Andesit vom Hoyazo (Cabo de Gata). Z. Deut. Geol. Ges. 40, 694–708 (1888).
Piwinskii, A. J., Wyllie, P. J.: Experimental studies of igneous rock series: a zoned pluton in the Wallowa Batholith, Oregon, J. Geol. 76, 205–234 (1968).
Plas, L., van der, Tobi, A. C.: A chart for judging the reliability of point counting results. Am. J. Sci. 263, 87–90 (1965).
Poldervaart, E.: Chemistry of the earth's crust, in: Crust of the Earth (symposium). Geol. Soc. Am., Spec. Papers 66, 119–144 (1955).
Read, H. H., Farquhar, O. C.: The geology of the Arnage district (Aberdeenshire): a reinterpretation. Quart. J. Geol. Soc. London 107, 423–440 (1952).
Rittmann, A.: Nomenclature of volcanic rocks. Bull. Volcanol. 12, 75–102 (1952).
—: Die Bimodalität des Vulkanismus und die Herkunft der Magmen. Geol. Rundschau 57, 277–295 (1967).
Ronov, A. B., Khlebnikova, Z. V.: Chemical composition of the main genetic clay types. Geochemistry, 527–552 (1957).
Shaw, D. M.: Geochemistry of pelitic rocks. Part III: Major elements and general geochemistry. Bull. Geol. Soc. Am. 67, 919–934 (1956).
Streckeisen, A. L.: Classification and nomenclature of igneous rocks. Neues Jahrb. Mineral., Abhandl. 107, 104–214 (1967).
Thornton, C. P., Tuttle, O. F.: Chemistry of igneous rocks. I. Differentiation Index. Am. J. Sci. 258, 664–684 (1960).
Turner, F. J.: Metamorphic petrology. New York etc: McGraw-Hill, 1968.
Tuttle, O. F., Bowen, N. L.: Origin of granite in the light of experimental studies in the system NaAlSi3O8-KAlSi3O8-SiO2-H2O. Geol. Soc. Am. Mem. 74, (1958).
Wager, L. R., Bailey, E. B.: Basic magma chilled against acid magma. Nature 172, 68–70 (1953).
Walker, G. P. L.: Acid volcanic rocks in Iceland. Bull. Volcanol. 29, 375–402 (1966).
—, Skelhorn, R. R.: Some associations of acid and basic igneous rocks. Earth-Sci. Rev. 2, 93–109 (1966).
Wilcox, R. E.: Rhyolite-basalt complex on Gardiner River, Yellowstone Park, Wyoming. Bull. Geol. Soc. Am. 55, 1047–1080 (1944).
Winkler, H. G. F.: Die Genese der metamorphen Gesteine, second edition. Berlin-Heidelberg-New York: Springer, 1967.
Wyllie, P. J., Tuttle, O. F.: Hydrothermal melting of shales. Geol. Mag. 98, 56–66 (1961).
Zeck, H. P.: Anatectic origin and further petrogenesis of almandine-bearing biotite-cordierite-labradorite-dacite with many inclusions of restite and basaltoid material, Sherry del Hoyazo, SE Spain. Thesis, Amsterdam University (1968).
Zoubek, V.: Le métamorphism d'injection et le métamorphism de contact dans les environs de Pelhrimov. Sb. St. Geol. Ust. ČSR (Prague) 7, 366–413 (1927).
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Zeck, H.P. An erupted migmatite from Cerro del Hoyazo, SE Spain. Contr. Mineral. and Petrol. 26, 225–246 (1970). https://doi.org/10.1007/BF00373202
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DOI: https://doi.org/10.1007/BF00373202