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Serpentine parent rock refers to a type of metamorphic rock that is primarily composed of serpentine minerals, which are formed from the alteration of ultramafic rocks, such as peridotite. This process, known as serpentinization, typically occurs under high-pressure and low-temperature conditions, often in the presence of water. Serpentine rocks are characterized by their green color and can be associated with geological settings such as ophiolite complexes and subduction zones. They are also significant in mineralogy and are often studied for their potential role in carbon sequestration.

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What metamorphic rock contains serpentine?

The parent rock of serpentine is called peridotite which is an ultramafic rock


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The parent rock for Serpentine is ultramafic rock, such as peridotite or dunite. Serpentine forms through the metamorphism of these ultramafic rocks under high pressure and temperature conditions.


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