Rare tabular and prismatic crystals. Usually occurs as fibrous, parallel veins that break off into cleavage fragments. Also occurs as grainy, massive, or nodular masses
Anhydrite, or anhydrous calcium sulfate, is a mineral with the chemical formula CaSO4. It is in the orthorhombic crystal system, with three directions of perfect cleavage parallel to the three planes of symmetry. It is not isomorphous with the orthorhombic barium (baryte) and strontium (celestine) sulfates, as might be expected from the chemical formulas. Distinctly developed crystals are somewhat rare, the mineral usually presenting the form of cleavage masses. The Mohs hardness is 3.5, and the specific gravity is 2.9. The color is white, sometimes greyish, bluish, or purple. On the best developed of the three cleavages, the lustre is pearly; on other surfaces it is glassy. When exposed to water, anhydrite readily transforms to the more commonly occurring gypsum, (CaSO4·2H2O) by the absorption of water. This transformation is reversible, with gypsum or calcium sulfate hemihydrate forming anhydrite by heating to around 200 °C (400 °F) under normal atmospheric conditions.[6] Anhydrite is commonly associated with calcite, halite, and sulfides such as galena, chalcopyrite, molybdenite, and pyrite in vein deposits.
Occurrence
Crystal structure of anhydrite
Anhydrite is most frequently found in evaporite deposits with gypsum; it was, for instance, first discovered in 1794 in a salt mine near Hall in Tirol. In this occurrence, depth is critical since nearer the surface anhydrite has been altered to gypsum by absorption of circulating ground water.
From an aqueous solution, calcium sulfate is deposited as crystals of gypsum, but when the solution contains an excess of sodium or potassium chloride, anhydrite is deposited if the temperature is above 40 °C (104 °F). This is one method by which the mineral has been prepared artificially and is identical with its mode of origin in nature. The mineral is common in salt basins.
Tidal flat nodules
Anhydrite occurs in a tidal flat environment in the Persian Gulfsabkhas as massive diagenetic replacement nodules. Cross sections of these nodular masses have a netted appearance and have been referred to as chicken-wire anhydrite. Nodular anhydrite occurs as replacement of gypsum in a variety of sedimentary depositional environments.[7]
Salt dome cap rocks
Massive amounts of anhydrite occur when salt domes form a caprock. Anhydrite is 1–3% of the minerals in salt domes and is generally left as a cap at the top of the salt when the halite is removed by pore waters. The typical cap rock is a salt, topped by a layer of anhydrite, topped by patches of gypsum, topped by a layer of calcite.[8] Interaction of anhydrite with hydrocarbons at high temperature in oil fields can reduce sulfate (SO2– 4) into hydrogen sulfide (H2S) with a concomitant precipitation of calcite.[9] The process is known as thermochemical sulfate reduction (TSR).
Hand sample of gypsum and anhydrite from diapir caprock showing "chicken wire" texture.
The name anhydrite was given by A. G. Werner in 1804, because of the absence of water of crystallization, as contrasted with the presence of water in gypsum. Some obsolete names for the species are muriacite and karstenite; the former, an earlier name, being given under the impression that the substance was a chloride (muriate). A peculiar variety occurring as contorted concretionary masses is known as tripe-stone, and a scaly granular variety, from Volpino, near Bergamo, in Lombardy, as vulpinite; the latter is cut and polished for ornamental purposes.
A semi-transparent light blue-grey variety from Peru is referred to by the trade name angelite.[11]
Other uses
Relief carving of an anhydrite kiln, made from a piece of anhydrite, by Ophelia Gordon Bell
Extensive structural damage in the German city of Staufen im Breisgau has occurred since a 2007 geothermal drilling project allowed subsurface water to invade a layer of anhydrite below the city, causing extensive but uneven ground swelling as pockets of the anhydrite converted to gypsum.
^Saunders, James A.; Thomas, Robert C. (September 1996). "Origin of 'exotic' minerals in Mississippi salt dome cap rocks: results of reaction-path modeling". Applied Geochemistry. 11 (5): 667–676. Bibcode:1996ApGC...11..667S. doi:10.1016/S0883-2927(96)00032-7.
^Luhr, James F. (2008). "Primary igneous anhydrite: Progress since its recognition in the 1982 El Chichón trachyandesite". Journal of Volcanology and Geothermal Research. 175 (4): 394–407. Bibcode:2008JVGR..175..394L. doi:10.1016/j.jvolgeores.2008.02.016.
