Hendricksite

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Hendricksite
General
CategoryMineral
Formula
(repeating unit)
KZn3(Si3Al)O10(OH)2
IMA symbolHds[1]
Strunz classification09.EC.20
Dana classification71.2.2b.6
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
Space groupB2/m
Unit cell499.58 ų
Identification
Formula mass493.25
ColorCopper-, bronze brown, dark reddish brown to reddish black
CleavagePerfect on {001}
Mohs scale hardness2.5 - 3
DiaphaneityTranslucent
Specific gravity2.86 - 3.43
Optical propertiesBiaxial (-)
Refractive indexnα = 1.598 - 1.624 nβ = 1.658 - 1.686 nγ = 1.660 - 1.697
Birefringence0.062 - 0.073
PleochroismX = pale yellow, Y = light chestnut brown, Z = light chestnut brown
2V angleMeasured 2°- 8°, calculated 20°- 44°
DispersionSlight, r < v
Common impuritiesTi, Fe, Ca, Ba, Li, Na, F

Hendricksite is a member of the trioctahedral micas group. The mineral was named by Clifford Frondel and Jun Ito in honor of Sterling Brown Hendricks, who studied micas. Zinc in the formula can be replaced with manganese(II) or magnesium. Currently, this is the only mica known for its zinc dominancy.[2] It was approved in 1966 by the IMA. It has a barely detectable, 1% radioactivity measured by GRapi (Gamma Ray American Petroleum Institute Units). It mostly consists of oxygen (38.92%), zinc (18.56%), silicon (15.37%) and manganese (10.02%), but otherwise contains potassium (7.13%) which gives the gem its irradiative attributes, aluminium (7.11%), magnesium (2.46%) and hydrogen (0.41%). It has pleochroic attributes, which is an optical phenomenon that makes gems to be seen a different color depending on the axis it is seen. On the X axis, it can be seen in a pale brown color, while on the Y and Z axis it is seen in a light chestnut brown color.[3]

References[]

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85: 291–320.
  2. ^ "Hendricksite". www.mindat.org. Retrieved 2021-02-11.
  3. ^ "Hendricksite Mineral Data". webmineral.com. Retrieved 2021-02-11.


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