Halide mineral

Halide minerals are those minerals with a dominant halide anion (F, Cl, Br and I). Complex halide minerals may also have polyatomic anions.[1]

Halite
Fluorite structure

Examples include the following:[2][3]

Many of these minerals are water-soluble and are often found in arid areas in crusts and other deposits as are various borates, nitrates, iodates, bromates and the like. Others, such as the fluorite group, are not water-soluble. As a collective whole, simple halide minerals (containing fluorine through iodine, alkali metals, alkaline Earth metals, in addition to other metals/cations) occur abundantly at the surface of the Earth in a variety of geologic settings. More complex minerals as shown below are also found.[6]

  1. ^ http://webmineral.com/strunz/strunz.php?class=03 Webmineral Halide Class.
  2. ^ Klein, Cornelis and Cornelius Hurlbut, Jr., Manual of Mineralogy, Wiley, 20th ed., 1985, pp. 320–325, ISBN 0-471-80580-7.
  3. ^ Anthony, J.W., Bideaux, R.A., Bladh, K.W., and Nichols, M.C., Handbook of Mineralogy, Volume III: Halides, Hydroxides, Oxides, 1997, Mineral Data Publishing: Tucson.
  4. ^ Handbook of Mineralogy - Bararite Archived 2016-04-01 at the Wayback Machine.
  5. ^ Handbook of Mineralogy - Cryptohalite Archived 2021-12-02 at the Wayback Machine.
  6. ^ Sorrel, Charles A., Rocks & Minerals (originally Minerals of the World), Chapter "Halides", pp. 118–127, 1973, St Martin's Press: NYC · Racine, WI, ISBN 1-58238-124-0.

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