Dear All,
In relation with the paper from Pattison and
al " polymetamorphic origin of muscovite + cordierite + Staurolite +
biotite " (1999), I would like to know yours opinions about this thins
section (attachment) found in " la Montagne Noire " (France) where the
equilibrium at Tmax seems to be obvious.
Do you know some other examples like
this?
Sincerely
______________________________
Régnier Jean-Luc
Johannes
Gutenberg-Universität
Institut für Geowissenschaften, FB
22
Graduiertenkolleg
Becherweg 21, 55099 Mainz
tel:
(0049)-6131-39-24767 (office)
tel: (0049)-6131-216469
(home)