Serpentinization is a geological low-temperature metamorphic process involving heat and water in which low-silica mafic and ultramafic rocks are oxidized (anaerobic oxidation of Fe2+ by the protons of water leading to the formation of H2) and hydrolyzed with water into serpentinite.
Serpentinization ແມ່ນຂະບວນການ metamorphic ທີ່ມີຄວາມຕໍ່າຂອງສະພາບພູມິສາດທີ່ກ່ຽວຂ້ອງກັບຄວາມຮ້ອນແລະນ້ໍາທີ່ມີຕ່ໍາ silica mafic ແລະ ultramafic rocks ຖືກ oxidized, oxidation anaerobic ຂອງ Fe2 + ໂດຍໂປຣຕີນຂອງນ້ໍາທີ່ນໍາໄປສູ່ການສ້າງ H2) ແລະ hydrolyzed ກັບນ້ໍາເຂົ້າ serpentinite.