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Broughton talc mine (Luzcan mine; Carrière rang XV), Saint-Pierre-de-Broughton (West Broughton), Les Appalaches RCM, Chaudière-Appalaches, Québec, Canada
|System:||Monoclinic||Hardness:||2 - 2½|
A group of mostly monoclinic (also triclinic or orthorhombic) micaceous phyllosilicate minerals with a structure consisting of T-O-T layers with two layers having their silicate tetrahedral apices pointing towards each other, separated by an interlayer that may be simple octahedrally coordinated cations or which may be a brucite-*like* layer of two sheets of closely packed OH groups with the interstices between sheets providing the octahedral cordination site; the T-O-T layers and interlayer are bonded by electrostatic and hydrogen bonding forces; as the "a" and "b" directions of the T-O-T layer may be oriented to the interlayer "a" and "b" directions in twelve different stacking sequences, resulting in twelve different polytype possibilities (not all of which have been found in Nature yet for each species).
The general formula may be stated A5-6T4Z18, where A = Al, Fe2+, Fe3+, Li, Mg, Mn, or Ni, while T = Al, Fe3+, Si, or a combination of them, and Z = O and/or OH.
The most common species in the chlorite group are clinochlore and chamosite.
The Árkai index (ÁI; Árkai, 1991) is an index for the estimation of very low metamorphic grade in rocks, based on the evolution of chlorite. It is often used to complement the Kübler index (KI), earlier called the 'illite crystallinity' for the characterisation of pelites, and can also be applied in metabasites.
Classification of Chlorite Group
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Physical Properties of Chlorite Group
|Hardness (Mohs):||2 - 2½|
|Density (measured):||2.6 - 3.3 g/cm3|
Crystallography of Chlorite Group
Relationship of Chlorite Group to other Species
Other Names for Chlorite Group
|Health Warning:||No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.|
References for Chlorite Group
Dodge, F.C.W. (1973), Chlorites from the granitic rocks of the central Sierra Nevada batholith: Mineralogical Magazine: 39: 58-64.
Post, J.L. and Janke, N.C. (1974) Properties of “swelling chlorite” in some Mesozoic formations of California. Lays and Clay Minerals: 22: 67-77.
Hazen, R.M. and Finger, L.W. (1978) The crystal structures and compressibilities of layer minerals at high pressure. II. Phlogopite and chlorite. American Mineralogist: 63: 293-296.
Spinnler, G.E. (1985) HRTEM study of antigorite, pyroxene-serpentine reactions and chlorite, 248 p. PhD Thesis, Arizona State University, Tempe, Arizona.
Schreyer, W., Fransolet, A.M., and Abraham, K. (1986) A miscibility gap in trioctahedral Mn-Mg-Fe chlorites: evidence from the Lienne Valley manganese deposit, Ardennes, Belgium. Contributions to Mineralogy and Petrology: 94: 333-342.
Bailey, S. W. (1988): Chlorites: Structures and crystal chemistry. Reviews in Mineralogy 19, 347-403.
Wiewiora, A. & Weiss, Z. (1990): Crystallochemical classifications of phyllosilicates based on the unified system of projection of chemical composition: II. The chlorite group. Clay Minerals 25, 83-92.
Árkai, P. (1991): Chlorite crystallinity: an empirical approach and correlation with illite crystallinity, coal rank and mineral facies as exemplified by Palaeozoic and Mesozoic rocks of northeast Hungary. J. Metamorphic Geology 9, 723-734.
Hillier, S. and Velde, B. (1991) Octahedral occupancy and the chemical composition of disgenetic (low-temperature) chlorite. Clay Minerals: 26: 149-168.
Árkai, P. and Ghabrial, D. (1997): Chlorite crystallinity as an indicator of metamorphic grade of low-temperature meta-igneous rocks; a case study from the Bükk Mountains, Northeast Hungary. Clay Minerals, 32, 205-222.
Li, G., Peacor, D.R., and Essene, E.J. (1998) The formation of sulfides during alteration of biotite to chlorite-corrensite. Clays and Clay Minerals: 46: 649-657.
Lougear, A., M. Grodzicki, C. Bertoldi, A.X. Trautwein, K. Steiner, and G. Amthauer (2000), Mössbauer and molecular orbital study of chlorites: Physica and Chemistry of Minerals: 27: 258-269.
Bertoldi, C., Benisek, A., Cemic, L., and Dachs, E. (2001) The heat capacity of two natural chlorite group minerals derived from differential scanning calorimetry. Physics and Chemistry of Minerals: 28: 332-336.
http://www.zeno.org/Meyers-1905/A/Chlor%C4%ABt [Link Broken? Dec 2014]
Internet Links for Chlorite Group
|Specimens:||The following Chlorite Group specimens are currently listed for sale on minfind.com.|
Localities for Chlorite Group
The map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.