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Estimation of the diagenetic smectite to illite transformation

Journal Article · · American Mineralogist; (United States)
OSTI ID:6991558
 [1];  [2]
  1. Ecole Normale Superieure, Paris (France)
  2. Centre de Geologie et Geophysique, Cedex (France)
A model is proposed to estimate the change in expandability of illite/smectite (I/S) minerals during burial diagenesis. The model uses a classical, first-order kinetic formulation. The values of activation energy and the preexponential constant are derived empirically by fitting the expandability of I/S minerals in samples from six deep wells in three sedimentary basins (USA and Japan) that had various burial rates. The series range in age at greatest depth from 4 to 150 Ma. Present thermal gradients are assumed to have pertained during the burial history of the sediments investigated, i.e., the upper three-fourths of the basin history. The derived kinetic values were tested on a seventh, older well (France, 210 Ma at greatest depth). A one-step reaction model cannot be fitted to all of the different wells. Following mineralogical, crystallographic indications and the results of experimental studies, the I/S series was divided into two reactions: one involving the disordered R = 0 structure minerals (100 - 50% expanding layers) and the other ordered R = 1 I/S (50-0% expanding layers). Reduction of expandability of the R = 0 minerals is assumed to determine the initiation of the second reaction. The second reaction shows progressive illitization of the ordered, R = 1 mineral that initially contained 50% smectite.
OSTI ID:
6991558
Journal Information:
American Mineralogist; (United States), Journal Name: American Mineralogist; (United States) Vol. 77:9-10; ISSN AMMIAY; ISSN 0003-004X
Country of Publication:
United States
Language:
English