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Gabon red soil samples

Gabon red soil samples

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mineral
mineral resources
Mineralogy Science Popularization
Hematite ore

Gabonese laterite is an important mineral resource, mainly distributed in the Gabonese region of Africa. Llaterite is a type of soil rich in iron and aluminum that is commonly formed in tropical and subtropical regions. Gabonese laterite is mainly composed of iron oxides and aluminum oxides and is rich in minerals such as hematite and bauxite. Due to the large amount of iron oxides, Gabonese laterites are usually red or brownish red. The laterite is formed by long-term weathering and leaching under tropical climatic conditions. The parent rock on the surface gradually decomposes in an alternating wet and dry environment, forming a soil layer rich in iron and aluminum.

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Gabon red soil samples

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Gabonese laterite is an important mineral resource, mainly distributed in the Gabonese region of Africa. Llaterite is a type of soil rich in iron and aluminum that is commonly formed in tropical and subtropical regions. Gabonese laterite is mainly composed of iron oxides and aluminum oxides and is rich in minerals such as hematite and bauxite. Due to the large amount of iron oxides, Gabonese laterites are usually red or brownish red. The laterite is formed by long-term weathering and leaching under tropical climatic conditions. The parent rock on the surface gradually decomposes in an alternating wet and dry environment, forming a soil layer rich in iron and aluminum.
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It is a kind of magmatic rock, which belongs to neutral deep intrusive rock. light gray, with grainy, porphyritic structure. The content of silica (about 60%) and the diorite is quite, but the alkali (sodium oxide, potassium oxide) is slightly higher than the diorite. It is mainly composed of feldspar, hornblende and biotite, with no or very little quartz. Alkaline feldspar (usually orthoclase, microcline, striated feldspar) accounts for more than 70% of the feldspar. It is often a small rock strain, which forms a complex with basic rocks and alkaline rocks.
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Syenite is a kind of magmatic rock, which belongs to neutral deep intrusive rock. light gray, with grainy, porphyritic structure. The content of silica (about 60%) and the diorite is quite, but the alkali (sodium oxide, potassium oxide) is slightly higher than the diorite. It is mainly composed of feldspar, hornblende and biotite, with no or very little quartz. Alkaline feldspar (usually orthoclase, microcline, striated feldspar) accounts for more than 70% of the feldspar. It is often a small rock strain, which forms a complex with basic rocks and alkaline rocks.
Syenite in alkaline rock mass

Syenite in alkaline rock mass

Syenite is a kind of magmatic rock, which belongs to neutral deep intrusive rock. light gray, with grainy, porphyritic structure. The content of silica (about 60%) and the diorite is quite, but the alkali (sodium oxide, potassium oxide) is slightly higher than the diorite. It is mainly composed of feldspar, hornblende and biotite, with no or very little quartz. Alkaline feldspar (usually orthoclase, microcline, striated feldspar) accounts for more than 70% of the feldspar. It is often a small rock strain, which forms a complex with basic rocks and alkaline rocks.

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