The crystal system of dolerite is generally considered to be the holocrystalline equivalent of basalt, which means that it typically has a fine-grained or microcrystalline texture that does not allow for the identification of crystal faces. Therefore, it does not have a clearly defined crystal systeRead more
The crystal system of dolerite is generally considered to be the holocrystalline equivalent of basalt, which means that it typically has a fine-grained or microcrystalline texture that does not allow for the identification of crystal faces. Therefore, it does not have a clearly defined crystal system. However, the individual mineral crystals that make up dolerite (such as plagioclase feldspar and pyroxene) have well-defined crystal systems, which are typically triclinic for plagioclase and monoclinic or orthorhombic for pyroxene.
The crystal system of dolerite is generally considered to be the holocrystalline equivalent of basalt, which means that it typically has a fine-grained or microcrystalline texture that does not allow for the identification of crystal faces. Therefore, it does not have a clearly defined crystal systeRead more
The crystal system of dolerite is generally considered to be the holocrystalline equivalent of basalt, which means that it typically has a fine-grained or microcrystalline texture that does not allow for the identification of crystal faces. Therefore, it does not have a clearly defined crystal system. However, the individual mineral crystals that make up dolerite (such as plagioclase feldspar and pyroxene) have well-defined crystal systems, which are typically triclinic for plagioclase and monoclinic or orthorhombic for pyroxene.
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