The tectono‐metamorphic evolution of the very low‐grade hangingwall constrains two‐stage gneiss dome formation in the Montagne Noire (Southern France)
Publisher: John Wiley & Sons Inc
E-ISSN: 1525-1314|33|1|71-89
ISSN: 0263-4929
Source: JOURNAL OF METAMORPHIC GEOLOGY, Vol.33, Iss.1, 2015-01, pp. : 71-89
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Abstract