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List of figures for Volume 3: CONTINENTAL BASINS
Chapter 14: SÃO FRANCISCO BASIN
Fig. 14.1 Map of the São Francisco Basin
and surrounding basement.
Fig. 14.2 Map of the Bambui Group.
Fig. 14.3 Lithostratigraphy of the São Francisco
Basin.
Fig. 14.4 Geological column of the São Francisco
Basin.
Fig. 14.5 Bouguer anomaly map.
Fig. 14.6 Geological map of the Alvorado do Norte
Area.
Fig. 14.7. Geological sections across the Alvorada
do Norte Area.
Chapter 15: PARANA BASIN
Fig. 15.1 Surface geology map of the Paraná
Basin.
Fig. 15.2 Outline map of the Paraná Basin.
Fig. 15.3 Well location map.
Fig. 15.4 Summary of exploration history.
Fig. 15.5 General lithostratigraphy.
Fig. 15.6 Chronostratigraphy .
Fig. 15.7 Well correlation 2-CM-1-PR, 2-RI-1-PR,
2-TB-1-SP, 2-LA-1-SSP, 2-AR- 1-SP and 2-OL-1-SP.
Fig. 15.8 Well correlation 2-AO-1-RS, 2-LV-1-RS,
1-ES-1-RS, 2-LA-1-SC, 1-BN-2- SC, 1-BN-1-SC.
Fig. 15.9 Regional correlation of the wells ASU-2,
2-RI-PR, and 2-AN-1-PR.
Fig. 15.10 Type sections of the Rio Ivai, Furnas
and Vila Maria Formations.
Fig. 15.11 Isopach maps of the Rio Ivai, Furnas
and Vila Maria Formations.
Fig. 15.12 Structural sections showing the Silurian
sequence in the central Paraná.
Fig. 15.13 Isopach map of the Ponta Grossa Formation.
Fig. 15.14 Stratigraphy of the Itararé Group.
Fig. 15.15 Proposed type section of the Lagoa Azul
Formation.
Fig. 15.16 Isopach map of the Tarabai Member.
Fig. 15.17 Isopach map of the Campo Mourão
Formation.
Fig. 15.18 Isopach map of the Taciba Formation.
Fig. 15.19 Isopach map of the Rio Segredo Member
of the Taciba Formation.
Fig. 15.20 Isopach map of the Chapeu do Sol and
Rio do Sul Members.
Fig. 15.21 Well correlation of the Itaré
Group.
Fig. 15.22 Well correlation of the Itaré
Group.
Fig. 15.23 Well correlation of the Itaré
Group.
Fig. 15.24 Well correlation of the Itaré
Group.
Fig. 15.25 Well correlation of the Itaré
Group.
Fig. 15.26 Well correlation of the Itaré
Group.
Fig. 15.27 Log of the Rio Bonito Sandstone.
Fig. 15.28 Isopach map of potential sandstones
in the Itararé Formation.
Fig. 15.29 TOC levels in the Irati Formation wells
1-RP-1-PR and 2-RI-1-PR.
Fig. 15.30 Isopach map of the Irati Formation.
Fig. 15.31 Isopach map of the potential source
rocks in the Irati Formation.
Fig. 15.32 Map of TOC levels in the Irati Formation.
Fig. 15.33 Map of the source rock thickness x TOC
of the Irati Formation.
Fig. 15.34 Map of distribution of organic matter
in the Irati Formation.
Fig. 15.35 Isopach map of potential source rocks
in the Ponta Grossa Formation.
Fig. 15.36 Map of TOC levels in the Ponta Grossa
Formation.
Fig. 15.37 Map of thickness of potential source
rocks x TOC content Ponta Grossa Formation.
Fig. 15.38 Map of the type of organic matter in
the Ponta Grossa Formation.
Fig. 15.39 Gas and oil chromatograms recovered
from tar sands and Irati shales.
Fig. 15.40 Map of maturity of the Ponta Grossa
Formation using method 1 Waples.
Fig. 15.41 Map of maturity of the Ponta Grossa
Formation using method 2 Waples.
Fig. 15.42 Map of cumulative thickness of igneous
intrusions in the Ponta Grossa Formation.
Fig. 15.43 Map of maturity of the Irati Formation.
Fig. 15.44 Map of the maturity of the Irati Formation
using method 1 Waples.
Fig. 15.45 Map of maturity of the Irati Formation
iusing method 2 Waples.
Fig. 15.46 Map of cumulative thickness of intrusives
in the Irati Formation.
Fig. 15.47 a) Time-temperature-depth plot of well
2-RI-1-PR
b) Maturation profile showing effects of igneous
intrusions.
Fig. 15.48 Present day geothermal gradients.
Fig. 15.49 Spatial distribution of the “three”
Paraná Basins.
Fig. 15.50 a) Total subsidence and back-stripped
curves for well 3-CB-3-CP.
b) Burial curves for six wells.
Fig. 15.51 Schematic structural evolution of the
Paraná Basin.
Fig. 15.52 Schematic structural evolution of the
Paraná Basin.
Fig. 15.53 Tentative map of the basement geology
of the Paraná Basin.
Fig. 15.54 Schematic map of the basement structures
in and around the Paraná Basin.
Fig. 15.55 Map of lineaments in and around the
Paraná Basin.
Fig. 15.56 a) Compressional structures produced
by Andean Collision .
b) Seismic section showing reverse Tertiary faulting
in the Pantanal Basin.
Fig. 15.57 Geomorphological structures in and around
the Paraná Basin.
Fig. 15.58 Structural section between Rio Urugai
and Rio Iguaçu.
Fig. 15.59 Distribution of Mesozoic/Cenozoic magmatism
in and around the Paraná Basin.
Fig. 15.60 Seismic section 225-RL-93.
Fig. 15.61 Possible hydrocarbon trap in anticlinal
structure over a dextral strike-slip fault.
Fig. 15.62 Possible hydrocarbon trap associated
with NE sinistral strike-slip fault.
Fig. 15.63 Possible hydrocarbon trap associated
with footwall uplift next to a Mesozoic fault.
Fig. 15.64 Possible hydrocarbon trap in an anticline
associated with reverse faulting.
Fig. 15.65 Regional seismic section across the
central Paraná Basin.
Fig. 15.66 Seismic section 225-01 showing deformation
associated with magmatic intrusion.
Fig. 15.67 Models of trapping mechanisms in the
Paraná basin.
Fig. 15.68 Schematic diagram showing generation
and migration of hydrocarbons.
figs: 14.1
- 15.68 / 16.1 -
17.37 / 18.1 - 21.53
/ 22.1 - 26.4
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