Antigorite is a lamellated, monoclinic mineral in the Silicate mineral serpentine subgroup with the ideal chemical formula of (Mg,Fe2+)3Si2O5(OH)4.
Geologic occurrences
Antigorite is found in low-temperature, high-pressure (or high-deformation) environments, including both extensional and compressional
Tectonics regimes.
Serpentines are commonly found in the ultramafic greenschist facies of subduction zones, and are visible on the Earth's surface through secondary exhumation. Serpentinites that contain antigorite are usually highly deformed and show distinct textures, indicative of the dynamic region where they were formed. Antigorite serpentinites commonly have associated minerals of
magnetite,
Chlorite group, and
.
Olivine under hydrothermal action, low grade metamorphism and weathering will transform into antigorite, which is often associate with talc and carbonate.
- + + →
- + → + +
Physical properties
Lamellated antigorite occurs in tough, pleated masses. It is usually dark green in color, but may also be yellowish, gray, brown or black. It has a Mohs scale hardness of 3.5–4 and its lustre is vitreous to greasy.
Antigorite has a specific gravity of 2.5–2.6. The monoclinic crystals show micaceous cleavage, a distinguished property of phyllosilicates, and fuse with difficulty.
Serpentinite rocks that consist of mostly antigorite are commonly
. The antigorite grains that make up these rocks are very fine (on the order of 1 to 10
Micrometre) and are fibrous, which defines a texture in the rock caused by lattice preferred orientation.
Gemstone properties
Antigorite is used as gemstones or for carvings when it appears pure and translucent, although many crystals have black specks of magnetite suspended within. The gem types of antigorite are
Bowenite and Williamsite. Bowenite, known for George T. Bowen from Rhode Island (the variety's type locality), who first analyzed the mineral, is translucent and light to dark green, often mottled with cloudy white patches and darker veining. It is the serpentine most frequently encountered in carving and jewelry, and is the state mineral of
Rhode Island, United States. A bowenite
cabochon featured as part of the "Our Mineral Heritage Brooch", was presented to U.S. First Lady Mrs. Lady Bird Johnson in 1967. Williamsite is very translucent and has a medium to deep apple-green color. Somewhat resembling jade, Williamsite is often cut into
and beads.
Crystal structure
The magnesian serpentines (antigorite,
lizardite,
chrysotile) are trioctahedral hydrous phyllosilicates. Their structure is based on 1:1 octahedral-tetrahedral layer structures. Antigorite is monoclinic in the space group Pm.
Although the magnesian serpentines have similar compositions, they have significantly different crystallographic structures, which are dependent on how the SiO
4 tetrahedra sheets fit in with the octahedral sheets.
Antigorite's basic composition has a smaller ratio of octahedral to tetrahedral cations (relative to lizardite and chrysotile),
allowing the structure to compensate for the misfit of sheets through periodic flipping of the curved tetrahedra layers, and subsequently their polarity.
Polysomes of antigorite are defined by the number of individual tetrahedra (denoted as the value
m) which span a
wavelength of the direction of curvature.
The sheets of tetrahedra allow the platy, fibrous crystals to separate parallel to the 001 (basal) plane, giving antigorite its perfect cleavage.
See also
-
Serpentine subgroup
-
Serpentinite
-
Subduction zone metamorphism – Hydrous minerals of a subducting slab
