The postevaporitic sequence of the southern part of Espírito Santo, Basin, one of the most typical basins of the Brazilianeast coast, is here studied. The material of three drilling cores (1-ESS-5, l-ESS-22 and 1-ESS-23), kindly lent by Petróleo Brasileiro S.A., PETROBRÁS, was studied. The data obtained from the three drillings were integrated into columnar profiles, for a better visualization of the results. Lithostratigraphical units were characterized, after the litologic description of the studied sections was accomplished. Palaeoenvirohments were established for the lithofaciologic units, according to the most diagnostic features of the studied lithofacies, such as granuloraetry, sedimentary structures, colours and distribution of the ...
This article is the first part of an overall theme dealing with different stratigraphic approaches t...
The detailed study of the Brazilian continental margin basins became possible with the advancement o...
Santos Basin is located in the southeast of the Brazilian continental margin and was created by rift...
The postevaporitic sequence of the southern part of Espírito Santo, Basin, one of the most typical b...
Detailed stratigraphic analysis of the Early Permian (Artinskian/Kungurian) succession of the intrac...
Detailed stratigraphic analysis of the Early Permian (Artinskian/Kungurian) succession of the intrac...
An original and detailed study focusing the petrography of evaporites from the Late Aptian deposits ...
The Mesoproterozoic Conselheiro Mata Group is the uppermost sequence of the Proterozoic intracontine...
An original and detailed study focusing the petrography of evaporites from the Late Aptian deposits ...
A number of small Callovian-Albian sedimentary basins occur in the NE-trending Araripe-Potiguar topo...
Paleozoic basins in northern Brazil contain thick sequences of sedimentary rocks, including diamicti...
Two PETROBRÁS oil wells drilled on the State of Ceará (Brazil) continental shelf (Mundaú and Icaraí ...
A number of small Callovian-Albian sedimentary basins occur in the NE-trending Araripe-Potiguar topo...
A number of small Callovian-Albian sedimentary basins occur in the NE-trending Araripe-Potiguar topo...
The Taciba and Rio Bonito (lower Triunfo Mbr) formations are divided into six depositional sequences...
This article is the first part of an overall theme dealing with different stratigraphic approaches t...
The detailed study of the Brazilian continental margin basins became possible with the advancement o...
Santos Basin is located in the southeast of the Brazilian continental margin and was created by rift...
The postevaporitic sequence of the southern part of Espírito Santo, Basin, one of the most typical b...
Detailed stratigraphic analysis of the Early Permian (Artinskian/Kungurian) succession of the intrac...
Detailed stratigraphic analysis of the Early Permian (Artinskian/Kungurian) succession of the intrac...
An original and detailed study focusing the petrography of evaporites from the Late Aptian deposits ...
The Mesoproterozoic Conselheiro Mata Group is the uppermost sequence of the Proterozoic intracontine...
An original and detailed study focusing the petrography of evaporites from the Late Aptian deposits ...
A number of small Callovian-Albian sedimentary basins occur in the NE-trending Araripe-Potiguar topo...
Paleozoic basins in northern Brazil contain thick sequences of sedimentary rocks, including diamicti...
Two PETROBRÁS oil wells drilled on the State of Ceará (Brazil) continental shelf (Mundaú and Icaraí ...
A number of small Callovian-Albian sedimentary basins occur in the NE-trending Araripe-Potiguar topo...
A number of small Callovian-Albian sedimentary basins occur in the NE-trending Araripe-Potiguar topo...
The Taciba and Rio Bonito (lower Triunfo Mbr) formations are divided into six depositional sequences...
This article is the first part of an overall theme dealing with different stratigraphic approaches t...
The detailed study of the Brazilian continental margin basins became possible with the advancement o...
Santos Basin is located in the southeast of the Brazilian continental margin and was created by rift...