From: Computerized geochemical modeling of burial diagenesis of the Eocene turbidite reservoir elements: Urucutuca Formation, Espírito Santo Basin, southeastern Brazil passive margin
Mineral
Sandstone (%)
Shale (%)
Quartz
46.35
21.15
K-feldspar
8.40
3.2
Plagioclase
12.00
4.0
Albie
0.3
4.1
Calcite
2.7
Dolomite
1.10
1.9
Kaolinite
4.35
3.15
Illite
5.5
49.5
Chlorite
0.5
4.5