By A. N. Sial, J. S. Bettencourt, C. P. De Campos, V. P. Ferreira
This quantity brings jointly a suite of papers that summarize present rules and up to date development within the learn of granite-related mineralization structures. they supply a mix of box, experimental and theoretical reviews. Papers are grouped based on the most granite-related ore structures: granite-pegmatite, skarn and greisen-veins, porphyry, orogenic gold, intrusion-related, epithermal and porphyry-related gold and base steel, iron oxide-copper-gold (IOCG), and exact case reviews. The reports supply a vast unfold by way of either area and time, highlighting granite-related ore deposits from Europe (Russia, Sweden, Croatia and Turkey) , the center East (Iran), Asia (Japan and China) and South the United States (Brazil and Argentina) and spanning rocks from Palaeoproterozoic to Miocene in age. The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on this planet, and one of many greatest publishers within the Earth sciences.The Society publishes quite a lot of top of the range peer-reviewed titles for teachers and execs operating within the geosciences, and enjoys an enviable foreign attractiveness for the standard of its work.The many parts within which we submit in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reviews and geochemistry-Remote sensing-History of geology-Regional geology courses
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Additional resources for Granite-Related Ore Deposits - Special Publication 350
585 Ma. Nevertheless, U –Pb ages from zircon overgrowths and zircon crystals from neosomes of migmatized G1 bodies, as well as U –Pb ages from monazite and some Pb –Pb evaporation ages in zircons, ranging from c. 575 to c. g. So¨llner et al. 1991; Nalini-Junior et al. 2000b; Noce et al. 2000; Whittington et al. 2001; Silva et al. 2002, 2005; De Campos et al. 2004; Vieira 2007; Novo 2009; Petitgirard et al. 2009). New U– Pb zircon ages for the Manhuac¸u stock and Estrela-Muniz Freire batholith are presented in this work.
2001; Noce et al. 2004; Pedrosa-Soares et al. 2006a, b; Silva et al. 2005, 2007; and new data presented below). New U –Pb geochronological data G3 supersuite One important feature, commonly observed in outcrop, is the re-melting process of G2 S-type granites, leading to the formation of G3 leucogranites An outcrop along a road cut located close to Nanuque (N in Fig. 1a) was sampled in order to compare the ages of G3 and G2 granites in the same outcrop. The G2 sample was collected from a foliated porphyroclastic garnet– biotite granite of GRANITES AND PEGMATITES, EASTERN BRAZIL 35 Fig.
2001a, 2007, 2008), De Campos et al. (2004), Silva et al. (2005) and Alkmim et al. (2006). The most remarkable feature of this crustal segment is the huge amount of different plutonic igneous rocks of Late Neoproterozoic up to Cambro– Ordovician ages, depicting a long lasting (c. 630– 480 Ma) succession of granite production events. Granitic rocks cover one third of the orogenic region, and built up the outstanding Eastern Brazilian Pegmatite Province (Fig. 1b) and the most important dimension stone province of Brazil.
Granite-Related Ore Deposits - Special Publication 350 by A. N. Sial, J. S. Bettencourt, C. P. De Campos, V. P. Ferreira