serpentiniitiksi
Serpentiniitiksi is a term that refers to a mineral aggregate composed primarily of serpentine minerals. Serpentine minerals are a group of phyllosilicate minerals that are formed by the hydration and alteration of magnesium-rich ultramafic rocks such as peridotite and dunite. This process, known as serpentinization, typically occurs at low temperatures and high pressures, often associated with tectonic plate boundaries or deep within the Earth's crust.
The appearance of serpentiniitiksi can vary greatly depending on the specific serpentine minerals present, the degree
Serpentiniitiksi is a common rock type in many geological settings, particularly in ophiolites, which are fragments