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Cesanite Cesanite is the end member of the apatite-wilkeite-ellestadite series that substitutes all of apatite's phosphate ions for sulfate ions and balances the difference in charge by replacing several calcium ions with sodium ions. Currently very few sites bearing cesanite have been found and are limited to a geothermal field in Cesano, Italy from which its name is derived, Măgurici Cave in Romania, and in the San Salvador caves in the Bahamas.

History
Cesanite was first discovered in 1981 while the Italian National Electricity Board was doing exploratory drilling to examine a reservoir of heated brine to determine its potential as a geothermal energy source. When it was first found it was thought to be an apatite until after more thorough examination(Cavaretta et al. 1981).

Structure
Cesanite was originally determined by Tazzoli (1983) to be isotypic to that of hydroxylapatite. This was determined by refining the original unit cell dimensions and comparing them to the atomic coordinates of Holly Springs hydroxylapatite. From this it was extrapolated that although different elements are substituted for cesanite, the structure and cell parameters are nearly the same with some differences in the bond lengths of the tetrahedras (Tazzoli 1983). This similarity was to confirm the space group $\overline{6}$3/m previously assigned to cesanite, this changed in 2002 after a reexamination of cesanite by Piotrowski et al. was prompted by its similarities to a synthetically produced analog. After this study it was found that the crystal structure of cesanite to be infrastructural to this synthetic analog with the chemical formula Ca2Na3[(OH)(SO4)3]. What can be inferred from this is that while hydroxylapatite remains similar in its chemical formula it is not longer to be considered a structural analog. The new correct space group is $\overline{0}$. It can be inferred that the reason the mistake went unnoticed for so long is that cesanite retains pseudo-symmetry in the array of its tetrahedra that closely mimics $\overline{6}$3/m (Piotrowski et al. 2002).

Cesanite's crystal structure is made up of tetrahedra comprised of sulfide cations surrounded by oxygen anions distributed along with hydroxide ions around the Ca and Na ions occupying the M1 through 4 sites(Piotrowski et al. 2002). The M1 and M2 cites create distorted pentagonal bipyramids while the M3 and M4 create tricapped trigonal prisms. The M3 and M4 polyhedra share faces when they are next to each other and form columns parallel to [001] while isolated sulphate tetrahedra alternate along the c axis(Piotrowski et al. 2002).

Physical properties
Cesanite veins are massive in habit and appear white in color with a silky luster. Individual crystals are colorless and transparent to translucent with a greasy luster. These crystals are elongated and begin with a pyramid on {101*0} that is distorted by a flatting that occurs down the length of the crystal which then extends down with two parallel faces until they are cut off by either a pinacoid or an other pyramid (Cavaretta et al. 1981). According to the newest sources the cells spacings for cesanite are 9.4630 along its a-axises and 6.9088 along its c-axis. In thin section cesanite remains transparent and has moderate birefringence (Cavaretta et al. 1981).In addition to is structure at room temperature Cesanite exhibits different crystal structures at different temperatures. Polymorphs occur at 425, 625, and 740 °C. These different forms are cause by expansion along the crystallographic axises as cesanite is heated (Deganello et al. 1982).

Geologic occurrence
Cesanite has been found in only three places to date. The original occurrence was observed as part of a fracture sealing process where cesanite crystals grew to fill in the void. It was found growing in a loosely packed vein of small crystals that became inter grown with those of the neighboring görgeyite crystals(Cavaretta et al. 1981). Further occurrences have been noticed in several caves. First in 2001 inside of Lighthouse Cave located on San Salvador Island filling in gaps in corroded gypsum and in 2003 inside Măgurici Cave in Romania it was found in close association with hydroxylapatite (Onac et al. 2001,2003). It has been presumed that in sequence hydroxylapatite is deposited followed by the formation of cesanite when the solution in which the crystals are being formed is rich in sodium and sulphate and depleted of calcium (Onac et al. 2001).