Recent geological, geochronological and isotopic studies allow the identification of four important crustal segments in the basement of the São Francisco Craton in Bahia. The oldest is the Gavião block in the WSW part of the studied area, and comprises granitic, granodioritic and migmatitic continental crust including remnants of 3.4 Ga TTGs which are amongst the oldest rocks in South America, and are associated with Archean greenstone belts. The youngest segment is exposed in the Itabuna-Salvador-Curaça belt which extends from SE Bahia along the Atlantic coast to Salvador, then northwards into NE Bahia. It is mainly composed of a low-K calc-alkaline plutonic suite, and also contains strips of intercalated metasediments and ocean floor/back-arc basin gabbro and basalt. In the SSW part of the area the Jequié block comprises granulitic migmatites with inclusions of supracrustal rocks, intruded by many charnockite plutons. In the NE, the Serrinha block is composed of orthogneisses and migmatites which form the basement for Paleoproterozoic greenstone belts. During the Paleoproterozoic Transamazonian Cycle, these four crustal segments collided, resulting in the formation of an important mountain belt. The regional metamorphism, resulting from the crustal thickening associated with the collision, occurred at around 2.0 Ga. Major mineralizations were formed during the evolution of the four Archean blocks, and also during and after the Paleoproterozoic collision.

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Recent geological, geochronological and isotopic research has identified four important Archean crustal segments in the basement of the São Francisco Craton in the State of Bahia. The oldest Gavião Block occurs in the WSW part, composed essentially of granitic, granodioritic and migmatitic rocks. It includes remnants of TTG suites, considered to represent the oldest rocks in the South American continent (∼ 3, 4Ga) and associated Archean greenstone belt sequences. The youngest segment, termed the Itabuna-Salvador-Curaçá Belt is exposed along the Atlantic Coast, from the SE part of Bahia up to Salvador and then along a NE trend. It is mainly composed of tonalite/trondhjemites, but also includes stripes of intercalated metasediments and ocean-floor/back-arc gabbros and basalts. The Jequié Block, the third segment, is exposed in the SE-SSW area, being characterized by Archean granulitic migmatites with supracrustal inclusions and several charnockitic intrusions. The Serrinha Block (fourth segment) occurs to the NE, composed of orthogneisses and migmatites, which represent the basement of Paleoproterozoic greenstone belts sequences. During the Paleoproterozoic Transamazonian Orogeny, these four crustal segments collided, resulting in the formation of an important mountain belt. Geochronological constrains indicate that the regional metamorphism resulting from crustal thickening associated with the collision process took place around 2.0 Ga.

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In this study, we evaluated the combination of transient isotachophoresis with on-line solid-phase extraction capillary electrophoresis time-of-flight mass spectrometry (SPE-tITP-CE-TOF-MS) to improve sensitivity of peptide analysis, using several opioid peptides as model compounds. First, standard solutions were analyzed in order to establish the tITP-CE methodology using UV and TOF-MS detection. The volume and composition of the leading and terminating electrolytes (i.e. LE and TE) for an efficient tITP were investigated to obtain optimum detection sensitivity and electrophoretic separation. In the best cases, LODs in tITP-CE-TOF-MS were tenfold better than those obtained in CE-TOF-MS (i.e. 5 versus 50 ng/mL). Afterwards, the tITP-CE-TOF-MS methodology was adapted to perform SPE-tITP-CE-TOF-MS. Repeatability, linearity and LODs were investigated and compared to the values obtained by SPE-CE-TOF-MS. Furthermore, human plasma samples fortified with the opioid peptides were analyzed in order to show the potential of SPE-tITP-CE-TOF-MS for peptide analysis in biological fluids. The LODs attained in standard solutions and plasma samples for some of the studied peptides (i.e. 0.01 and 0.1 ng/mL, respectively) were tenfold better than those obtained in SPE-CE-TOF-MS, proving the enhanced sensitivity that could be achieved when both on-line preconcentration approaches were combined together.

The aim of this work was to evaluate the microemulsification as sample preparation procedure for determination of Cu, Fe, Ni and Zn in vegetable oils samples by High-Resolution Continuum Source Flame Atomic Absorption Spectrometry (HR-CS FAAS). Microemulsions were prepared by mixing samples with propan-1-ol and aqueous acid solution, which allowed the use of inorganic aqueous standards for the calibration. To a sample mass of 0.5g, 100μL of hydrochloric acid and propan-1-ol were added and the resulting mixture diluted to a final volume of 10mL. The sample was manually shaken resulting in a visually homogeneous system. The main lines were selected for all studied metals and the detection limits (3σ, n=10) were 0.12, 0.62, 0.58 and 0.12mgkg(-1) for Cu, Fe, Ni and Zn, respectively. The relative standard deviation (RSD) ranged from 5% to 11 % in samples spiked with 0.25 and 1.5μgmL(-1) of each metal, respectively. Recoveries varied from 89% to 102%. The proposed method was applied to the determination of Cu, Fe, Ni and Zn in soybean, olive and sunflower oils.

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