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GNEISS DOMES AND GRANITE EMPLACEMENT IN AN OBLIQUELY CONVERGENT REGIME: NEW INTERPRETATION OF THE VARISCAN AGLY MASSIF (EASTERN PYRENEES, FRANCE) (2004)
In this paper, we present a reinterpretation of the Agly dome based on a detailed kinematic study and on new U-Pb dating of zircons from two variably deformed granite bodies, one located in the gneissic core and the other located in the micaschist cover.
Reference:
"Geological Society of America, Special Paper 380, 2004"
"Geological Society of America, Special Paper 380, 2004"
Organization:
Universit Paul Sabatier, 38 rue des Trente-Six-Ponts, 31400, Toulouse, France
France
Universit Paul Sabatier, 38 rue des Trente-Six-Ponts, 31400, Toulouse, France
France
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