Braz. J. Geol. vol.46 número4

envolvidas na manifestação cultural 211. É evidente que, na prática, estas pesquisas e métodos são quase impossíveis de serem realizados sem uma efetiva investigação de campo

Relembramos que as suas áreas de atuação não são unívocas nos trâmites da comunicação organizacional: os seus diferentes públicos e o “novo espaço de fluxos”

he Canastra Group, within the studied area, is represented only by the Paracatu formation quartzites and phyllites, thrusted over the carbonatic-pelitic rocks of the Vazante

(A) Seismic facies A, interpreted as shelf-margin deltas/shoreface deposits; (B) seismic facies B, interpreted as slope clinoforms with tangential (oblique) geometry; (C)

Given those prior studies, this work sought to charac- terize the geometry of the diabase sills of the Serra Geral Formation, Early Cretaceous age, which occur in the strati-

Kaolinite, gibbsite, goethite and anatase are the main minerals in the bauxitic clay (Figs. 3A and 3B); goethite, hematite, gibbsite and anatase are the main minerals in the

The probability of attending school four our group of interest in this region increased by 6.5 percentage points after the expansion of the Bolsa Família program in 2007 and

The theoretical results are compared with the experimental data of Vogel and Eaton (J. of Heat Transfer, Transactions of ASME, vol.107, pp. The paper shows that the