Sanidine(K; Na)(Al; Si)4 O8c 2001 Mineral Data Publishing, ver sion 1.2°

Crystal Data: Monoclinic. Point Group: 2=m: Crystals commonly tabular on f010g, with asquare cross section, to 50 cm. Acicular in spherulites. Twinning: Carlsbad twins are common,
Baveno and Manebach twins rarer.
Physical Properties:
Cleavage: Perfect on f001g, distinct on f010g; parting on f100g.
Fracture: Conchoidal to uneven. Tenacity: Brittle. Hardness = 6 D(meas.) = 2.56{2.62D(calc.) = [2.56]
Optical Properties: Transparent. Color: Colorless to white; colorless in thin section.
Streak: White. Luster: Vitreous, pearly on cleavage.
Optical Class: Biaxial ({). Orientation: Y = b; Z ^ c ' ¡20 ± (low); Z = b; Y ^ c ' ¡21 ±(high).
Dispersion: r < v or r > v; weak. ® = 1.518{1.524 ¯ = 1.522{1.529° = 1.522{1.530 2V(meas.) = 18± {42± (low); 15± {63± (high)Cell Data: Space Group: C2=m (high).
¯ = 116:03(2)± Z = 4

a = 8.603(2)b = 13.036(4)c = 7.174(2)

X-ray Powder Pattern: Locality unknown.
3.326 (100), 3.284 (60), 3.788 (57), 4.235 (53), 3.225 (52), 2.584 (35), 3.458 (31)Chemistry:
SiO2
Al 2 O3
FeO + Fe2 O 3CaO

(1)
64.79
18.50

(2)
67.27
18.35
0.92
0.15

(1)
Na 2 O
K 2O
H2 O+H2 O¡
Total

16.79

(2)
6.45
7.05
0.08
0.08

100.08100.35(1) Buck claims, Bernic Lake, Canada; by electron microprobe, average of analyses on six crystals;
corresponds to K0:99 Al 1:01 Si 3:00 O 8: (2) Mitchell Mesa rhyolite, Texas, USA; corresponds to(Na0:56 K0:40 Ca0:01 )§=0:97 (Al 0:97 Fe3+0:03 ) §=1:00 Si 3: 01 O8 :Polymorphism & Series:
Mineral Group:

High sanidine forms a series with high albite.

Feldspar (alkali) group; (Al,Si) completely disordered.

Occurrence: Most common in felsic volcanic and hypabyssal rocks as rhyolites, phonolites,trachytes; as spherulites in volcanic glass. Also from ultrapotassic ma¯c, high-temperature contact
metamorphic (sanidinite facies), and hydrothermally altered rocks. From eclogite nodules inkimberlite.
Association:Quartz, sodic plagioclase, muscovite, biotite, \hornblende," magnetite.

Distribution: Not uncommon, but rare in crystals of any size. In Germany, from Drachenfels,Siebengebirge, Rhine; and at Hohenfels, Mendig, Mayen, and elsewhere around the Laacher See,
Eifel district. In France, at Mt. Dore, Auvergne, and Puy Gros du Laney, Puy-de-D^o me. From
Vesuvius and Monte Somma, Campania, and Monte Cimine, Lazio, Italy. At Daichi, Wakayama
Prefecture, Japan. From Kanchin-do, Meisem-gun, northeast Korea. In the USA, at Tooele,Tooele Co., Utah; Cottonwood Canyon, Peloncillo Mountains, Cochise Co., Arizona; as large
crystals in Rabb Canyon and near the crest of the Black Range, Grant Co., New Mexico. From
Bernic Lake, Manitoba, and Mont Saint-Hilaire, Quebec, Canada. In the Sierra de San Francisco,Durango, Mexico.
Name:

From the Greek for tablet or board, in allusion to the mineral's common habit.

References: (1) Dana, E.S. (1892) Dana's system of mineralogy, (6th edition), 318.
(2) Deer, W.A., R.A. Howie, and J. Zussman (1963) Rock-forming minerals, v. 4, frameworksilicates, 6{93. (3) Phillips, W.R. and D.T. Gri®en (1981) Optical mineralogy, 342{344.
·(4) Ferguson, R.B., N.A. Ball, and P. Cern¶y (1991) Structure re¯nement of an adularian
end-member high sanidine from the Buck Claim pegmatite, Bernic Lake, Manitoba.
Can. Mineral., 29, 543{552. (5) Scheel, H.J. (1971) Lead feldspar. Zeits. Krist., 133, 264{272.
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