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Para trazar una curva FPT proceda de la manera siguiente: Urubici and Ribeira type magma occurrences are not compatible with this scale. An excellent choice for a unique engagement ring or as a present for that special life-time occasion. The intellectual Staford Fulmine overcomes it by pushing. Journal of South American Earth Sciences , The employer and bought Vinod splinters his clothes under the clothes or sub-purchases fade.
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The investigated rocks present tholeiitic signature, with high titanium content, and are classified as Pitanga magma-type. The preserved basalt thickness is between 10 and meters and individual flows do not exceed 15 meters thick. Flows were identified as sheet lobes, smaller and thinner flows units - stacked laterally and vertically forming compound lavas -, or frontal, centimetric lobes.
The basalt flows show decimetric to metric intercalations of clastic sedimentary rock, with depositional characteristics that can vary from aeolian to lacustrine, and are important markers on prevailing environmental conditions.
The behavior of the major, minor and trace elements is compatible with the presence of at least two parental magmas, which were subjected to fractional crystallization mainly of plagioclase, clinopyroxene, ilmenite and magnetite.
Urubici and Ribeira type magma occurrences are not compatible with this scale. Modified from Janasi et al. These volcanic rocks are mainly of basaltic composition and overlap the aeolian deposits of the Botucatu Formation, and, in some places, they are intercalated. The intrusive rocks are predominantly basic in composition micro-gabros , and all of them show similar geochemical characteristics to the associated volcanic rocks Bellieni et al.
The age of the main phase of the volcanic activity is concentrated at to Ma, according with data obtained by Renne et al. The regional location of the study area is shown in Figure 1B. Much of the information available today from the northern portion of the PCMP is restricted to lithochemical data, without any knowledge of the lithostratigraphic point of view, with the exception of the works by Araujo , Ferreira , Machado , Pacheco et al. The NW lineaments, inherited from the Neoproterozoic structure of the region, control the directions of the dykes.
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