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    Atlas Geografico Del Peru" stamped in gold on the spine. Images may be reproduced or transmitted, but not for commercial use.

    Atlas is bound in half leather brown marbled paper covered boards with "Paz Soldan. Digital images and descriptive data © 2000 by Cartography Associates.

    Paris, Libreria de Augusto Durand, Calle de Gres-Sorbonne, 7. Paz Soldan published a large six sheet Mapa del Peru in 1864 (see The Map Collector).

    (Paris, Libreria de Augusto Durand, 1865)Atlas geografico del Peru, publicado a expensas del Gobierno Peruano, siendo Presidente el Libertador Gran Mariscal Ramon Castilla, por Mariano Felipe Paz Soldan ... Nine of the Department maps in our copy are hand colored, with the rest uncolored (normally the Department maps are uncolored).

    Puedes seguir de cerca la programación de Azteca América en Twitter; y si deseas saber qué ocurre cada minuto, esta cadena maneja un perfil (Azteca Noticias) enfocado en noticias y últimos acontecimientos.

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    U–Th–Pb ion microprobe analysis of inherited/detrital zircon cores from the dacite reveals five principal age groups, 2·8–2·5 Ga, 2·1–1·9 Ga, 1·1–0·9 Ga, 650–550 Ma and 350–320 Ma, indicating a Gondwana domain provenance.Initially the rock was thought to have originated from a country rock contaminated andesitic magma (e.g. Current modelling, however, indicates that it represents an erupted anatectic magma generated by partial melting of a pelitic/quartzo-feldspathic high-grade gneiss complex (Zeck, 1968, 1970, 1992; Munksgaard, 1984; Zeck , 1999); the Al-rich enclaves represent the complementary syngenetic restite material trapped within the anatectic dacitic melt.The present paper reports the use of ion microprobe U–Pb zircon dating to test the model of anatectic magma production, and to infer the anatectic source rock complex and the timing of the magmatic evolution from anatexis to eruption.The inheritance age patterns of both dacite and restitic enclave, and zircon ages from the basement below the Cerro del Hoyazo, suggest that the anatectic source complex was probably a high-grade amphibolite facies equivalent of either the Palaeozoic schist complex of the basal nappe section or, more likely, its Permo-Triassic cover section.Cerro del Hoyazo cordierite dacite is a classic S-type magmatic rock, well known for its abundant, extremely Al-rich rock inclusions.

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