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Formation of coexisting 1M and 2M polytypes in illite from an active hydrothermal system

Journal Article · · American Mineralogist; (United States)
OSTI ID:5639839
;  [1]
  1. Australian National Univ., Canberra (Australia)
Polytypes of illite from the Broadlands-Ohaaki geothermal system in New Zealand have been studied with transmission electron microscopy and electron diffraction. The illite is predominantly a one-layer polytype with 1.0-nm interlayer spacing. On the scale of a few millimeters, illite occurs as ordered crystals, disordered crystals, and crystals with regions of ordered and disordered stacking. Some crystals are composed entirely of either the one-layer or the two-layer polytype; others show regions of two-layer stacking in a one-layer host. Long period stacking sequences (3- or 4-layer) are less common and occur as lamellar intergrowths in 1M mica. No morphological differences were observed among the discrete crystals, of 1M{sub d}, 1M, and 2M. Textures indicate that regions with two-layer stacking can be produced from 1M{sub d} mica even though there is a general trend with increasing temperature of 1M{sub d} to 1M to 2M. Experimental data on the rate of transformation of 1M to 2M{sub 1} muscovite combined with estimates of the mole fraction of 2M mica and temperatures of illite crystallization were used to place constraints on the duration of hydrothermal activity in the Broadlands-Ohaaki system.
OSTI ID:
5639839
Journal Information:
American Mineralogist; (United States), Journal Name: American Mineralogist; (United States) Vol. 75:11-12; ISSN AMMIA; ISSN 0003-004X
Country of Publication:
United States
Language:
English