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Clay Minerals; March 2001; v. 36; no. 1; p. 140
© 2001 Mineralogical Society of Great Britain and Ireland
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FORTHCOMING PAPERS

The first 20% of the full text of this article appears below.

The following are some papers to be published in future issues of Clay Minerals:

M. Burkhard and N. Badertscher. Finite strain has no influence on the illite crystallinity of tectonized Eocene limestone breccias of the Morcles nappe, Swiss Alps

M. Burkhard and D. Goy-Eggenberger. Near vertical iso-illite-crystallinity surfaces cross-cut the recumbent fold structure of the Morcles nappe, Swiss Alps

B. Kübler and D. Goy-Eggenberger. Aggradation . . . [Full Text of this Article]






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