1978

NOME: EVALDO DE ANDRADE COELHO GUEIROS
ORIENTADOR: CARLOS EDUARDO DE MORAES FERNANDES
TÍTULO: "GEOLOGIA DE UM PALEO 'CANYON' SUBMARINO DA BACIA DO ESPÍRITO SANTO"
ABSTRACT: The REGÊNCIA CANYON is a submarine feature, of Late Cretaceous age, located in the southern portion of the Rio Doce mouth, in Espírito Santo Basin. According to seismic reflection data and four dry holes drilled down to the cristaline basement, it was possible to set up the probable geologic history for the canyon. Sand turbidites were mapped and these show very good possibilities for hydrocarbon prospecting.

1980

NOME: ROGÉRIO CARVALHO DE GODOY
ORIENTADOR: WENDELIN FRANZ LOTZE
TÍTULO: "VARIAÇÃO SECULAR DA INTENSIDADE DO CAMPO GEOMAGNÉTICO NO BRASIL"
BANCA EXAMINADORA: CARLOS EDUARDO DE MORAES FERNANDES, ANTONIO SALDANHA DE SOUZA NEVES
JOSÉ DE SÁ BORGES FILHO DATA DA DEFESA: 29 DE DEZEMBRO
NO DO PROCESSO: 36.237/80
ABSTRACT: A survey of available data, useful for computations of geomagnetic models in Brazil was done. Site descriptions as well as well as observed values in repeat stations and annuel mean values of geomagnetic observatories were revised, corrected, coded and organized in digital files. Two models of the total intensity of geomagnetic field and four models of its secular variation were computed using the data files. The models are evaluted according to geomagnetic observatory data and compared with other models. Conclusions on changes in field work methodology and about future work flow are derived.

1981

NOME: JANDYR DE MENEZES TRAVASSOS
ORIENTADOR: AUGUSTO CESAR BITTENCOURT PIRES
TÍTULO: "DISTORÇÃO DO CAMPO GAMA PRIMÁRIO NA CAMADA ATMOSFÉRICA SUPERFICIAL CAUSADA PELA BIOMASSA AÉREA DE UMA FLORESTA"
BANCA EXAMINADORA: WENDELIN FRANZ LOTZE, ANTONIO SALDANHA DE SOUZA NEVES, JOSÉ DE SÁ BORGES FILHO
DATA DA DEFESA: 25 DE NOVEMBRO
NO DO PROCESSO: 39.772/81
ABSTRACT: The screening effect of a forest cover is determined for local and extended gamma-field sources in the soil. We choose a tropical rain forest on the "terra firme"near Manaus with a biomass of 10g/cm2 . The screening is estimated assuming a layered structure of the aerial phytomass. This has shown that can be considered independent of survey altitude in the range 100 - 200m, with less tha 10% errors. The anisotropy on trunks of trees is estimated using Monte Carlo method. It has shown that anisotropy can kead toerrors in the estimated screening effect reaching 20%. Radioactive properties of the stand were analysed. This has shown to reach 10% of the radiation from gamma-field sources in the soil.

1989

NOME: HUGO RICHARD BERTETE AGUIRRE
ORIENTADOR: WENDELIN FRANZ LOTZE
TÍTULO: "LEVANTAMENTO GRAVIMÉTRICO, MODELAMENTO BI-DIMENSIONAL AUTOMÁTICO E INTERPRETAÇÃO NA REGIÃO OCIDENTAL DA BAIXADA DE JACAREPAGUÁ - RJ"
ABSTRACT: The aim of the present investigations enclose three principal aspect: 1) gravimetry survey, 2) methodology development of automatic two-dimensional modellig, and 3) interpretation of gravity anomalies. The chosen area for the application was the occidental region of the "Baixada de Jacarepaguá-RJ". Based on geological and geomorphological data of the area, and on the gravity interpretations results was possible to detect: a) maximum depth of the sediments, which is aproximately of 150 m; b) regions were the basament is practicaly emerging; c) possible secondary paleo-canals with and average depth of 70-80 m. The area presents gravity anomalies bigger than the one initialy expected. The maximum amplitude verified was 2.7 mgal. Computers programs were developeded in the present thesis for the gravimetry reductions, prefencialy to the automatic two-dimensional gravity modelling. The original algorithm (Qureshi, 1971) was modified in this work to improve the convergence and reability of the results.

1992

NOME: PAULA LUCIA FERRUCIO DA ROCHA
ORIENTADOR: CARLOS EDUARDO DE MORAES FERNANDES
TÍTULO: "MAPA PRELIMINAR DE CONTORNO DO TOPO DO EMBASAMENTO CRISTALINO, COM BASE EM PROSPECÇÃO GRAVIMÉTRICA, DA BAIXADA DE JACAREPAGUÁ - RJ - BRASIL"
ABSTRACT: In this work, we present the results of a geophysical survey, by gravimetric measurements, in a 6 km by 17 km area, at Baixada de Jacarepaguá (Rio de Janeiro - Brazil) aiming to determine depths for the basement complex. Measurements were performed at 66 sites with an Autograv CG-3 Scintrex gravimeter, owned by UFRJ, the distance between nearest sites being typically 1 km. The results of the survey allowed us to construct a contour map for the crystalline basement, in a 1:25.000, scale. Detailed computations, based on geological, geomorphological and gravimetric data revealed the existence of an irregular paleorelief, corresponding to the original subsurface which then formed the bottom of part of a sedimentary basin (Pliocene, according to Roncarati and Neves, 1976) in which sedimentation was beginning. The possible existence of faults and intruding bodies in the basement is also discussed. The contour map is considered to be preliminary due to the fact that our interpretation lacks depth control to basement by boring and also due to the fact that the station density for the area is not sufficient to completely cover the rock interface irregularities.

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