%0 Journal Article
%T Estudio petrogr芍fico y geoqu赤mico del Complejo Plut車nico El Peˋuelo (Cintur車n de Intrusivos de Concepci車n del Oro), noreste de M谷xico
%A Velasco-Tapia
%A Fernando
%A Gonz芍lez-Guzm芍n
%A Rene谷
%A Ch芍vez-Cabello
%A Gabriel
%A Lozano-Serna
%A Javier
%A Valencia-Moreno
%A Mart赤n
%J Bolet赤n de la Sociedad Geol車gica Mexicana
%D 2011
%I Sociedad Geol車gica Mexicana
%X this work presents the petrographic and geochemical data for the el peˋuelo plutonic complex (eppc), which is an intrusive that belongs to concepci車n del oro intrusive belt (coib; northeastern mexico). the eppc is a semi-circular structure, constituted by three emplacement centers, situated in the eastern part of the coib and the northern extension of the taxco-san miguel de allende fault system. however, the complex was not affected by the activity of this fault system. the eppc is constituted by intrusive rocks varying from quartz monzodiorite to quartz syenite, the latter covering most of the complex surface. the eppc was emplaced in upper cretaceous marine sedimentary rocks. the quartz syenite is cut by quartz monzodioritic and porphyritic meso-syenitic dykes. also, this unit contains irregularly distributed monzodioritic microgranular enclaves. additionally, pegmatitic dykes cut the rest of the lithologic units. the eppc mineralogical assemblage shows variable quantities of plagioclase + alkaline feldspar + quartz ㊣ amphibole + biotite ㊣ orthopyroxene + clinopyroxene + fe-ti oxides. intrusive rocks have a chemical composition of sio2 = 45.7-72.0 %, mg# = 39.2-60.2, and n-fe = 0.54-0.73. they show chondrite-normalized ree patterns enriched in light elements [(la/yb)n = 6-11] with no eu anomalies. primitive mantle-normalized multi-element diagrams show lile enriched patterns relative to the hfse. their trace-element geochemistry is comparable to high-ba-sr granitoids: (a) high ba concentration (= 594-2302 ppm) and sr (= 444-2192 ppm); (b) low concentrations of y (= 10-46 ppm) and nb (= 6-17 ppm); and (c) high values for sr/y (= 25-85) and (la/yb = 8.9-16.5) ratios. the origin of eppc has been related to partial melting of an enriched lithospheric mantle, in a post-orogenic setting, followed by fractional crystallization coupled to crustal assimilation.
%K northeastern mexico
%K high-ba-sr granitoids
%K post-orogenic magmatism.
%U http://www.scielo.org.mx/scielo.php?script=sci_abstract&pid=S1405-33222011000200005&lng=en&nrm=iso&tlng=en