Geological Mapping of Mafic Stock Intrusions

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The mafic stocking is an igneous feature that occurs within sedimentary rocks. It is characterized by the intrusion of mafic or basaltic magma into the surrounding sedimentary strata. Mafic rocks are those that are rich in dark-colored minerals such as pyroxene and olivine, and have high concentrations of iron and magnesium. The intrusion of mafic magma into sedimentary rocks typically occurs during periods of tectonic activity, when the Earth's crust is being uplifted and deformed. Mafic magmas are typically more dense than the surrounding sedimentary rocks, which allows them to infiltrate and displace the existing strata. The presence of a mafic stocking can have a significant impact on the surrounding sedimentary rocks.


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The presence of a mafic stocking can have a significant impact on the surrounding sedimentary rocks. The heat from the intrusive magma can cause metamorphism of the surrounding rocks, leading to the development of new minerals and textures. This can result in the formation of contact metamorphic aureoles around the mafic stocking.

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        The mafic stocking

        In addition to metamorphism, the intrusion of mafic magma can also lead to the formation of new structures within the sedimentary rocks. For example, fractures and faults may develop as a result of the expansion and contraction of the rocks due to the heat from the magma. These structures can have an impact on the permeability and porosity of the rocks, affecting their ability to store and transport fluids such as water and hydrocarbons. The size and shape of a mafic stocking can vary considerably, ranging from small intrusions to large, batholith-like bodies. The shape of the stocking can be influenced by the pre-existing structures and lithology of the surrounding rocks. Overall, the mafic stocking is an intriguing geological feature that highlights the complex interactions between igneous and sedimentary rocks. Its presence can have important implications for the geology and geothermal potential of a given area..

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