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1

Dino, Rodolfo, and Yann Le Gallo. "CCS project in Recôncavo Basin." Energy Procedia 1, no. 1 (2009): 2005–11. http://dx.doi.org/10.1016/j.egypro.2009.01.261.

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2

De Bona, J., N. Dani, J. M. Ketzer, and L. F. De Ros. "Dickite in shallow oil reservoirs from Recôncavo Basin, Brazil: diagenetic implications for basin evolution." Clay Minerals 43, no. 2 (2008): 213–33. http://dx.doi.org/10.1180/claymin.2008.043.2.06.

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AbstractFluvial and aeolian sandstones of the Sergi Formation are the most important reservoirs of the Recôncavo Basin, Brazil. Optical and scanning electron microscopy, X-ray diffraction and infrared spectroscopy revealed the occurrence of dickite, a clay mineral indicative of deep burial conditions (T >100ºC), in the shallow Buracica (630–870 m) and Água Grande (1300–1530 m) oilfields. Vermicular dickite replaces K-feldspar and plagioclase grains, and fills intra- and inter-granular pores. Its vermicular habit is a product of pseudomorphic kaolinite transformation during burial. The prese
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Oliveira, Naiane Pereira de, and Amin Bassrei. "SEISMIC TRAVELTIME TOMOGRAPHY IN THE DOM JOÃO FIELD, RECÔNCAVO BASIN, BRAZIL." Revista Brasileira de Geofísica 33, no. 1 (2015): 89. http://dx.doi.org/10.22564/rbgf.v33i1.604.

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ABSTRACT. Tomography was incorporated in Exploration Geophysics with the intention of providing high-resolution images of regions in Earth’s subsurface that are characterized as potential reservoirs. In this work, seismic traveltime tomography in the transmission mode was applied to real data from the Dom João Field, Recôncavo Basin, State of Bahia, Brazil. This basin represents a landmark of oil exploration in Brazil and has been intensively studied since the 1950’s. Today, the Recôncavo Basin is still the principal oil producer in the State of Bahia, but there is a demand for new technologie
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4

Pereira, Ricardo, Ismar S. Carvalho, Antonio Carlos S. Fernandes, and Débora A. Azevedo. "Chemotaxonomical aspects of lower Cretaceous amber from Recôncavo Basin, Brazil." Journal of the Brazilian Chemical Society 22, no. 8 (2011): 1511–18. http://dx.doi.org/10.1590/s0103-50532011000800015.

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5

Balbinot, M., and W. Kalkreuth. "Organic geochemistry and petrology of the Gomo Member, Recôncavo Basin, Brazil." International Journal of Coal Geology 84, no. 3-4 (2010): 286–92. http://dx.doi.org/10.1016/j.coal.2010.09.008.

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6

de Lima, Olivar A. L. "Geophysical evaluation of sandstone aquifers in the Recôncavo‐Tucano Basin, Bahia—Brazil." GEOPHYSICS 58, no. 11 (1993): 1689–702. http://dx.doi.org/10.1190/1.1443384.

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The upper clastic sediments in the Recôncavo‐Tucano basin comprise a multilayer aquifer system of Jurassic age. Its groundwater is normally fresh down to depths of more than 1000 m. Locally, however, there are zones producing high salinity or sulfur geothermal waters. In other areas, the system is being exploited heavily to support a petrochemical center and related industries. Analysis of electrical logs of more than 150 wells enabled the identification of the most typical sedimentary structures and the gross geometries for the sandstone units in selected areas of the basin. Based on this inf
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7

Câmara, Roberto José Batista, Aldo Luiz Silva, George Câmara, et al. "Preliminary assessment of surface conditions for carbon dioxide injection projects from pre-selected fields in the Recôncavo Basin, Brazil." International Journal of Technology Management & Sustainable Development 19, no. 2 (2020): 123–45. http://dx.doi.org/10.1386/tmsd_00019_1.

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Energy-intensive industries have had to increase their production to meet global demands, consequently increasing their emissions of greenhouse gases (GHGs) such as CO2. Carbon dioxide is the raw material used in enhanced oil recovery (EOR) techniques, which have been gaining importance, taking into account the issues of global climate change and the potential to store CO2. The aim of this study was to develop a project analysis framework and assess the surface characteristics of candidate fields for CO2 injection projects located in the Recôncavo Basin, Bahia, Brazil, while also considering t
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8

Aona, Lidyanne Yuriko Saleme, Grênivel Mota da Costa, Maria do Carmo E. do Amaral, Aparecida Donisete de Faria, Edson Ferreira Duarte, and Volker Bittrich. "Aquatic and marsh plants from the Recôncavo basin of Bahia state, Brazil: checklist and life forms." Check List 11, no. 6 (2015): 1806. http://dx.doi.org/10.15560/11.6.1806.

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Aquatic and marsh plants are those that have the capacity to withstand a continuous or periodic submersion in water, at least of their roots. Such plants are thus able to occupy environments that are at least periodically waterlogged. The knowledge about this plant group is still rather incomplete for various parts of Brazil including the Northeast. The present study was conducted in Bahia state, through collections in 20 municipalities within the Recôncavo basin between 2009 and 2015. All species were classified across six life forms. We report 316 species in 206 genera and 71 families, inclu
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9

Falcão, Lisie Carvalho, and Jorge Carlos Della Favera. "Sublacustrine channel-levee system of the Caruaçu member, southwest Recôncavo Basin, Bahia, Brazil." Revista Brasileira de Geociências 42, no. 3 (2012): 539–46. http://dx.doi.org/10.25249/0375-7536.2012423539546.

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10

Cavalcanti, Susana Silva, and Olivar Antônio Lima De Lima. "STRUCTURAL, LITHOLOGICAL AND PETROPHYSICAL CHARACTERIZATION OF THE RECÔNCAVO AQUIFER SYSTEM IN THE CAPIVARA RIVER BASIN, BAHIA STATE, BRAZIL." Revista Brasileira de Geofísica 31, no. 3 (2013): 375. http://dx.doi.org/10.22564/rbgf.v31i3.325.

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ABSTRACT. The hydrogeophysical features of the Recôncavo aquifer system in the area of the Capivara Grande and Capivara Pequena rivers, in Camac¸ari and Dias D’Ávila counties were studied through the analysis of 64 Schlumberger vertical electrical soundings expanded to AB/2 spacing of 1.000 m. This characterization was also supported by the analysis of lithologic logs of 29 water exploration wells, 14 of which have available geophysical logs. The results were useful to outline the structural configuration of the regional aquifer system in the area, from the surface up to 450 m in depth. The mul
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11

Rostirolla, Sidnei Pires, Antonio Carlos Mattana, and Marcelo Kulevicz Bartoszeck. "Bayesian assessment of favorability for oil and gas prospects over the Recôncavo basin, Brazil." AAPG Bulletin 87, no. 4 (2003): 647–66. http://dx.doi.org/10.1306/10070201068.

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12

Carozzi, A. V., and J. D. R. Fonseca. "A new technique of locating turbidite fans: Candeias formation (lower cretaceous), Recôncavo Basin, Brazil." Journal of South American Earth Sciences 2, no. 3 (1989): 277–93. http://dx.doi.org/10.1016/0895-9811(89)90034-5.

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13

Rodrigues, Taissa, and Alexander Kellner. "Note on the pterosaur material described by Woodward from the Recôncavo Basin, Lower Cretaceous, Brazil." REVISTA BRASILEIRA DE PALEONTOLOGIA 13, no. 2 (2010): 159–64. http://dx.doi.org/10.4072/rbp.2010.2.08.

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14

Freire, Antonio Fernando Menezes, Gabriel Fernando Rocha dos Santos, Carolina Ferreira da Silva, and Wagner Moreira Lupinacci. "Recognition of turbidite stages in the Massapê oil field, Recôncavo Basin - Brazil, using well logs." Journal of Petroleum Science and Engineering 192 (September 2020): 107279. http://dx.doi.org/10.1016/j.petrol.2020.107279.

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15

Della Fávera, Jorge Carlos, Hernani Aquini Fernandes Chaves, Marco André Malmann Medeiros, et al. "STRATIGRAPHIC ANALYSIS OF THE ARATU STAGE (LOWER CRETACEOUS), RECÔNCAVO BASIN (BRAZIL), WITH HYDROCARBON RESERVOIR ROCKS." Journal of Sedimentary Environments 4, no. 2 (2019): 199–219. http://dx.doi.org/10.12957/jse.2019.43784.

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The section between the 7 and 11 electric markers in the Aratu Stage of the Recôncavo Basin (Lower Cretaceous) has been studied in order to perform a stratigraphic analysis. This section bear reservoir rocks known as Imbé, Cambuqui and Miranga sandstones. It produces petroleum in fields like Miranga, Araçás, Taquipe, Miranga Norte and Imbé.The isopach map showed a general trend of increased subsidence for south and southeast. A series of structural lows surround the platform region known as Quiricó High. Southwestward, the Taquipe Canyon is an indication of the lake deepening in that region.In
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16

Rostirolla, Sidnei Pires, Paulo César Soares, and Hung Kiang Chang. "Bayesian and multivariate methods applied to favorability quantification in Recôncavo Basin and Ribeira Belt, Brazil." Nonrenewable Resources 7, no. 1 (1998): 7–24. http://dx.doi.org/10.1007/bf02782505.

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17

Maronezi, Líllian Vasconcellos Brandão, Rosanne Santos, Bruno Medeiros, Rafael Muller, and Alexandre Barroso. "Corrosion inhibitor study for acidification treatment / intervention in onshore wells in the recôncavo baiano basin." Rio Oil and Gas Expo and Conference 20, no. 2020 (2020): 54–55. http://dx.doi.org/10.48072/2525-7579.rog.2020.054.

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18

Pamponet, Vanessa de Carvalho Cayres, Paulo Luiz Souza Carneiro, Paulo Roberto Antunes de Mello Affonso, et al. "A multi-approach analysis of the genetic diversity in populations of Astyanax aff. bimaculatus Linnaeus, 1758 (Teleostei: Characidae) from Northeastern Brazil." Neotropical Ichthyology 6, no. 4 (2008): 621–30. http://dx.doi.org/10.1590/s1679-62252008000400010.

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Few reports are available about the ichthyofauna of typical semi-arid rivers, although the regional diversity has been constantly threatened by human activities, mainly related to impoundment and construction of dams. The goal of the present work was to evaluate using different methods, the population genetic structure of a characin fish, Astyanax aff. bimaculatus, widespread throughout hydrographic basins of Bahia, Northeastern Brazil. Morphological (meristic and morphometric data), cytogenetic (karyotype and Ag-NOR), and molecular (RAPD and SPAR) analyses were carried out in specimens collec
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19

Vita, George, Marco Tulio Oliveira Ferreira, Washington Tavechio, and Gislaine Guidelli. "Fishes from the rio da Dona, a threatened environment in the Recôncavo Sul basin, Bahia, Brazil." Papéis Avulsos de Zoologia 60 (February 4, 2020): e20206008. http://dx.doi.org/10.11606/1807-0205/2020.60.08.

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The rio da Dona is an important water body in the Recôncavo Sul basin used as a water supply for the neighboring towns and for agriculture, recreation and subsistence fishing. The knowledge about the ichthyofauna of this river is scarce. In this paper, an inventory of the fish fauna from rio da Dona basin and an identification key for the species recorded are presented. Additionally, taxonomic and conservationist issues are discussed. The specimens were collected in different sites along the upper, middle and lower courses of the rio da Dona. The fishes were anesthetized, fixed in formalin, co
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20

Scherer, Claiton M. S., Ernesto L. C. Lavina, Dorval C. Dias Filho, Flávio M. Oliveira, Daniela E. Bongiolo, and Eduardo S. Aguiar. "Stratigraphy and facies architecture of the fluvial–aeolian–lacustrine Sergi Formation (Upper Jurassic), Recôncavo Basin, Brazil." Sedimentary Geology 194, no. 3-4 (2007): 169–93. http://dx.doi.org/10.1016/j.sedgeo.2006.06.002.

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21

FIGUEIREDO, FRANCISCO J. DE, and DOUGLAS R. M. RIBEIRO. "Reassessment and Relationships of †Scutatuspinosus itapagipensis (Teleostei, Clupeomorpha, †Ellimmichthyiformes) from the Neocomian of Recôncavo Basin, Northeastern Brazil." Anais da Academia Brasileira de Ciências 89, no. 2 (2017): 799–823. http://dx.doi.org/10.1590/0001-3765201620160310.

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22

Fávera, Jorge C. Della, Hemani A. Fernandes Chaves, Marco André Malmann Medeiros, et al. "Lake level oscillations recorded in Buracica Stage (Barremian, Early Cretaceous) of Recôncavo Basin, Bahia State (N.E. Brazil)." Journal of Sedimentary Environments 5, no. 4 (2020): 425–56. http://dx.doi.org/10.1007/s43217-020-00026-3.

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23

Bitencourt, Jamille de Araújo, Paulo Roberto Antunes de Mello Affonso, Lucia Giuliano-Caetano, and Ana Lucia Dias. "Identification of distinct evolutionary units in allopatric populations of Hypostomus cf. wuchereri Günther, 1864 (Siluriformes: Loricariidae): karyotypic evidence." Neotropical Ichthyology 9, no. 2 (2011): 317–24. http://dx.doi.org/10.1590/s1679-62252011000200008.

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Few chromosomal reports are available for the endemic fish fauna from coastal basins in northeastern Brazil, and regional biodiversity remains partially or completely unknown. This is particularly true for Loricariidae, the most diverse family of armored catfishes. In the present work, allopatric populations of Hypostomus cf. wuchereri (Siluriformes: Loricariidae) from two basins in Bahia (northeastern Brazil) were cytogenetically analyzed. Both populations shared 2n = 76 chromosomes, a karyotype formula of 10m+18sm+48st/a (FN = 104) and single terminal GC-rich NORs on the second metacentric p
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24

Netto, Anna Luisa Abreu, George Câmara, Expedito Rocha, et al. "A first look at social factors driving CCS perception in Brazil: A case study in the Recôncavo Basin." International Journal of Greenhouse Gas Control 98 (July 2020): 103053. http://dx.doi.org/10.1016/j.ijggc.2020.103053.

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Nunes, Elizabete Almeida, Elvia Fadul, and Lucas Santos Cerqueira. "GOVERNANÇA DAS ÁGUAS NA BAHIA: UMA AVALIAÇÃO DA PARTICIPAÇÃO SOCIAL NO COMITÊ DE BACIA DO RECÔNCAVO NORTE E INHAMBUPE." RDE - Revista de Desenvolvimento Econômico 1, no. 39 (2018): 267. http://dx.doi.org/10.21452/rde.v2i40.5440.

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Desde promulgação da Constituição Federal de 1988, os movimentos sociais e outros segmentos da sociedade excluídos do processo decisório do Estado vêm reivindicando mais espaço e mais envolvimento político. Na governança das águas não é diferente, princip
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26

Bongiolo, Daniela E., and Claiton M. S. Scherer. "Facies architecture and heterogeneity of the fluvial–aeolian reservoirs of the Sergi formation (Upper Jurassic), Recôncavo Basin, NE Brazil." Marine and Petroleum Geology 27, no. 9 (2010): 1885–97. http://dx.doi.org/10.1016/j.marpetgeo.2010.07.015.

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27

Almeida da Costa, A., J. Mateo, R. Patel, et al. "Can low salinity water injection be an efficient option for the Recôncavo Basin? An experimental and simulation case study." Journal of Petroleum Science and Engineering 202 (July 2021): 108557. http://dx.doi.org/10.1016/j.petrol.2021.108557.

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28

G. Souza, Rafael, Douglas Riff, and Alexander W. A. Kellner. "Taxonomic revision of Thoracosaurus bahiensis Marsh, 1869, a supposed Gavialoidea (Reptilia, Crocodylia) from Cretaceous deposits of the Recôncavo Basin, Brazil." REVISTA BRASILEIRA DE PALEONTOLOGIA 18, no. 3 (2015): 565–68. http://dx.doi.org/10.4072/rbp.2015.3.17.

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Scherer, Claiton M. S., and Karin Goldberg. "Cyclic cross-bedding in the eolian dunes of the Sergi Formation (Upper Jurassic), Recôncavo Basin: Inferences about the wind regime." Palaeogeography, Palaeoclimatology, Palaeoecology 296, no. 1-2 (2010): 103–10. http://dx.doi.org/10.1016/j.palaeo.2010.06.018.

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Anjos, S. M. Couto, and A. V. Carozzi. "Depositional and diagenetic factors in the generation of the Santiago arenite reservoirs (lower cretaceous): Araçás oil field, Recôncavo Basin, Brazil." Journal of South American Earth Sciences 1, no. 1 (1988): 3–19. http://dx.doi.org/10.1016/0895-9811(88)90012-0.

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31

Silva, João B., Denis C. Costa, and Valéria C. Barbosa. "Gravity inversion of basement relief and estimation of density contrast variation with depth." GEOPHYSICS 71, no. 5 (2006): J51—J58. http://dx.doi.org/10.1190/1.2236383.

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We present a method to estimate the basement relief as well as the density contrast at the surface and the hyperbolic decaying factor of the density contrast with depth, assuming that the gravity anomaly and the depth to the basement at a few points are known. In both cases, the interpretation model is a set of vertical rectangular 2D prisms whose thicknesses are parameters to be estimated and that represent the depth to the interface separating sediments and basement. The solutions to both problems are stable because of the incorporation of additional prior information about the smoothness of
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32

Mendonça, Carlos Alberto. "Inversion of gravity‐field inclination to map the basement relief of sedimentary basins." GEOPHYSICS 69, no. 5 (2004): 1240–51. http://dx.doi.org/10.1190/1.1801940.

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This paper presents a method to map the basement relief of homogeneous sedimentary basins that does not require the knowledge of the basin density contrast. To reach this task, the proposed method relies on the invariance of the inclination of the anomalous gravity field with the density contrast caused by models constituted by two homogeneous media. This invariance occurs because the density contrast appears as a constant factor in both vertical and horizontal gravity components, therefore being canceled out when these components are divided during the evaluation of the field inclination. For
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33

Freire, Antonio Fernando Menezes, Carlson de Matos Maia Leite, Flávio Miranda de Oliveira, et al. "Fluid escape structures as possible indicators of past gas hydrate dissociation during the deposition of the Barremian sediments in the Recôncavo Basin, NE, Brazil." Brazilian Journal of Geology 47, no. 1 (2017): 79–93. http://dx.doi.org/10.1590/2317-4889201720160090.

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ABSTRACT: Empty elliptical vesicles are observed in outcrops of Barremian very fine clayey sandstone to siltstone lacustrine slurry deposits of the Pitanga Member (Maracangalha Formation), exposed in the Maré Island, Southern Recôncavo Basin, Brazil. These sedimentary features have been traditionally interpreted as water escape structures triggered by the diapirism of the underlying shales of the Candeias Formation. This work proposes that vesicles were generated during massive gas hydrate dissociation as a result of tectonic activity in a paleolake system. Tectonic uplift would have triggered
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34

Souza, Pamela, Gelson Fambrini, Renan Queiroz, and Leonardo Oliveira. "GEOLOGIA DA ÁREA NORDESTE DA FOLHA POÇO DA CRUZ, BACIA DE JATOBÁ, NORDESTE DO BRASIL." Estudos Geológicos 30, no. 1 (2020): 45–78. http://dx.doi.org/10.18190/1980-8208/estudosgeologicos.v30n1p45-78.

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The Jatobá Basin is located in the south-central portion of Pernambuco state and northern Bahia and Alagoas, it has an area of approximately 5000 km² in a NE-SW preferred direction and sedimentary record has approximately 3 km. It is a rift basin developed under extensional tectonic events related to the rupture of the Gondwana supercontinent and it marks the northern limit of the aborted Recôncavo-Tucano-Jatobá rift system. The stratigraphic succession in the Campos district, Ibimirim (PE), comprises the Syneclise sequence and Rift Initiation sequence as well as part of the Rift Climax sequen
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Silva, D. R., A. M. P. Mizusaki, E. J. Milani, and M. Pimentel. "Depositional ages of Paleozoic and Mesozoic pre-rift supersequences of the Recôncavo Basin in northeastern Brazil: A Rb–Sr radiometric study of sedimentary rocks." Journal of South American Earth Sciences 37 (August 2012): 13–24. http://dx.doi.org/10.1016/j.jsames.2011.12.006.

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36

Fambrini, Gelson Luís, Virgínio Henrique M. L. Neumann, José Acioli B. Menezes-Filho, Wellington F. Da Silva-Filho, and Édison Vicente De Oliveira. "Facies architecture of the fluvial Missão Velha Formation (Late Jurassic–Early Cretaceous), Araripe Basin, Northeast Brazil: paleogeographic and tectonic implications." Acta Geologica Polonica 67, no. 4 (2017): 515–45. http://dx.doi.org/10.1515/agp-2017-0029.

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Abstract Sedimentological analysis of the Missão Velha Formation (Araripe Basin, northeast Brazil) is the aim of this paper through detailed facies analysis, architectural elements, depositional systems and paleocurrent data. The main facies recognized were: (i) coarse-grained conglomeratic sandstones, locally pebbly conglomerates, with abundant silicified fossil trunks and several large-to-medium trough cross-stratifications and predominantly lenticular geometry; (ii) lenticular coarse-to-medium sandstones with some granules, abundant silicified fossil wood, and large-to-medium trough cross-s
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37

Lyrio, Julio Cesar S. O., Paulo T. L. Menezes, Jorlivan L. Correa, and Adriano R. Viana. "Multiphysics anomaly map: A new data fusion workflow for geophysical interpretation." Interpretation 8, no. 2 (2020): B35—B43. http://dx.doi.org/10.1190/int-2018-0178.1.

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When collecting and processing geophysical data for exploration, the same geologic feature can generate a different response for each rock property being targeted. Typically, the units of these responses may differ by several orders of magnitude; therefore, the combination of geophysical data in integrated interpretation is not a straightforward process and cannot be performed by visual inspection only. The multiphysics anomaly map (MAM) that we have developed is a data fusion solution that consists of a spatial representation of the correlation between anomalies detected with different geophy
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38

Barbosa, Valéria Cristina F., João B. C. Silva, and Walter E. Medeiros. "Gravity inversion of basement relief using approximate equality constraints on depths." GEOPHYSICS 62, no. 6 (1997): 1745–57. http://dx.doi.org/10.1190/1.1444275.

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We present a gravity interpretation method for estimating the relief of an arbitrary interface separating two homogeneous media. The upper medium is discretized into rectangular, juxtaposed prisms whose thicknesses represent the depths to the interface and are the parameters to be estimated from the gravity anomaly. The density contrast of each prism is assumed to be constant and known. To stabilize the inversion, we introduce two kinds of constraints on the depths. The first one requires proximity between the observed and computed depths at isolated points such as those obtained from borehole
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de Lima, Olivar A. L., Michael Ben Clennell, Geraldo Girão Nery, and Sri Niwas. "A volumetric approach for the resistivity response of freshwater shaly sandstones." GEOPHYSICS 70, no. 1 (2005): F1—F10. http://dx.doi.org/10.1190/1.1852771.

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The dc electrical response of freshwater-saturated shaly sandstone is analyzed on the basis of effective volume conductivity concepts for a concentrated mixture of “solid grains” in a continuous electrolyte. The bulk conductivity of this model is physically controlled by (1) the effective porosity and the average electrical tortuosity of its free-pore electrolyte, and (2) the amount and concentration of bound water that coats charged solid surfaces (mainly of clays), and a corresponding averaged electrical surface tortuosity. The latter is combined in an equivalent volume conductivity that is
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40

Leão, Jorge W. D., Paulo T. L. Menezes, Jacira F. Beltrão, and João B. C. Silva. "Gravity inversion of basement relief constrained by the knowledge of depth at isolated points." GEOPHYSICS 61, no. 6 (1996): 1702–14. http://dx.doi.org/10.1190/1.1444088.

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We present an interpretation method for the gravity anomaly of an arbitrary interface separating two homogeneous media. It consists essentially of a downward continuation of the observed anomaly and the division of the continued anomaly by a scale factor involving the density contrast between the media. The knowledge of the interface depth at isolated points is used to estimate the depth [Formula: see text] of the shallowest point of the interface, the density contrast Δρ between the two media, and the coefficients [Formula: see text] and [Formula: see text] of a first‐order polynomial represe
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41

Leal, Adelson Belizário, Bruno Medeiros, Alexandre de Lima Barroso, and Líllian Maronezi. "Otimização na perfuração de poço onshore de alta instabilidade no recôncavo baiano utilizando nano tecnologia e motor de alta performance Drilling optimization of highly unstable onshore well in the reconcavo Baiano basin using nonotechnology and high performance motor." Rio Oil and Gas Expo and Conference 20, no. 2020 (2020): 26–27. http://dx.doi.org/10.48072/2525-7579.rog.2020.026.

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42

Pereira, Ricardo, Ismar de Souza Carvalho, Bernd R. T. Simoneit, and Débora de Almeida Azevedo. "Molecular composition and chemosystematic aspects of Cretaceous amber from the Amazonas, Araripe and Recôncavo basins, Brazil." Organic Geochemistry 40, no. 8 (2009): 863–75. http://dx.doi.org/10.1016/j.orggeochem.2009.05.002.

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Lima, Janderson Carmo, Marilza Neves Nascimenro, Uasley Caldas Oliveira, Anacleto Ranulfo Santos, and Alinsmario Leite Silva. "Macronutrient fertilizers on basil growth and yield." Comunicata Scientiae 11 (May 4, 2020): e3200. http://dx.doi.org/10.14295/cs.v11i0.3200.

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The objective of this work was to determine the macronutrient doses that allow the highest phytomass yield and growth of basil plants. The experiment was carried out in the experimental area of ​​the Federal University of Recôncavo da Bahia, in Cruz das Almas, BA, in a greenhouse. The treatments were obtained according to the Baconian matrix statistical arrangement, in which one of the nutrients is supplied in variable amounts, while the others are kept at a referential level. Six nutrients (nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg) and sulfur (S)) were evaluate
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Suzart Alves, Lucylia, Hans Raj Gheyi, Vital Pedro Da Silva Paz, Alexandre Nascimento dos Santos, Mairton Gomes da Silva, and Samir De Souza Bandeira. "CULTIVO DE MANJERICÃO UTILIZANDO EFLUENTE DOMÉSTICO TRATADO EM SISTEMAS HIDROPÔNICOS SOB DIFERENTES ESPAÇAMENTOS ENTRE PLANTAS." IRRIGA 24, no. 3 (2019): 460–72. http://dx.doi.org/10.15809/irriga.2019v24n3p460-472.

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CULTIVO DE MANJERICÃO UTILIZANDO EFLUENTE DOMÉSTICO TRATADO EM SISTEMAS HIDROPÔNICOS SOB DIFERENTES ESPAÇAMENTOS ENTRE PLANTAS
 
 
 LUCYLIA SUZART ALVES1; HANS RAJ GHEYI2; VITAL PEDRO DA SILVA PAZ2; ALEXANDRE NASCIMENTO DOS SANTOS3; MAIRTON GOMES DA SILVA2 E SAMIR DE SOUZA BANDEIRA2
 
 1 Programa de Pós-Graduação em Engenharia Civil e Ambiental, Universidade Estadual de Feira de Santana-UEFS, Av. Transnordestina, s/n, CEP: 44036-900, Feira de Santana-BA, Brasil. E-mail: lusuzart85@yahoo.com.br
 2 Programa de Pós-Graduação em Engenharia Agrícola, Núcleo de Engenhar
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Rodrigues, Vitor Hugo Serravalle Reis, and Amin Bassrei. "SEISMIC TRAVELTIME TOMOGRAPHY APPLIED TO DATA FROM MIRANGA FIELD, RECÔNCAVO BASIN, BRAZIL." Revista Brasileira de Geofísica 34, no. 3 (2016). http://dx.doi.org/10.22564/rbgf.v34i3.856.

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ABSTRACT. The growing global demand for hydrocarbons has tested the limits of oil exploration and exploitation technologies. Among the seismic methods, tomography is an alternative means for high-resolution characterization of reservoirs, and it enables a more efficient...Keywords: reservoir characterization, traveltime tomography, seismic inversion, regularization, Recôncavo Basin. RESUMO. A crescente demanda mundial por hidrocarbonetos tem testado os limites das tecnologias de exploração e explotação de petróleo. Dentro dos métodos sísmicos, a tomografia surge como alternativa de caracteriza
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Bessoni, Thaíza Pereira, Amin Bassrei, and Luiz Gabriel Souza de Oliveira. "Inversion of satellite gravimetric data from Recôncavo-Tucano-Jatobá Basin System." Brazilian Journal of Geology 50, no. 3 (2020). http://dx.doi.org/10.1590/2317-488920202020190113.

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SOUZA, RAFAEL G. DE, and DIOGENES A. CAMPOS. "New Crocodyliform specimens from Recôncavo-Tucano Basin (Early Cretaceous) of Bahia, Brazil." Anais da Academia Brasileira de Ciências 91, suppl 2 (2019). http://dx.doi.org/10.1590/0001-3765201720170382.

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Amaral, Diego Nery do, José Roberto Cerqueira, Consuelo Lima Navarro de Andrade, et al. "Paleoenvironmental characterization of a Lower Cretaceous section of the Recôncavo Basin, Bahia, Brazil." Brazilian Journal of Geology 50, no. 3 (2020). http://dx.doi.org/10.1590/2317-4889202020190058.

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"Sublacustrine channel-levee system of the Caruaçu member, southwest Recôncavo Basin, Bahia, Brazil." Revista Brasileira de Geociências 42, no. 3 (2012). http://dx.doi.org/10.5327/z0375-75362012000300008.

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Souza, Rafael G., Rodrigo G. Figueiredo, Sérgio A. K. Azevedo, Douglas Riff, and Alexander W. A. Kellner. "Systematic revision of Sarcosuchus hartti (Crocodyliformes) from the Recôncavo Basin (Early Cretaceous) of Bahia, north-eastern Brazil." Zoological Journal of the Linnean Society, August 12, 2019. http://dx.doi.org/10.1093/zoolinnean/zlz057.

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AbstractSarcosuchus hartii was a top predator that inhabited the fluvial and coastal areas of north-eastern Brazil during the Early Cretaceous. Several fossil remains were recovered during the late 19th and early 20th centuries from strata that outcrop in the Recôncavo Basin in the state of Bahia. A re-analysis of this material shows that S. hartii is a valid species. The Brazilian taxon differs from the African Sarcosuchus imperator in the unique pattern of anastomosing ornamentation observed on the enamel surface. The inclusion of S. hartii in a novel phylogenetic analysis recovered it insid
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