An anticlockwise
P–T–t
path at high‐pressure, high‐temperature conditions for a migmatitic gneiss from the island of Fjørtoft, Western Gneiss Region, Norway, indicates two burial events during the Caledonian orogeny
1998 ◽
Vol 278-281
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pp. 612-617
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1978 ◽
Vol 15
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pp. A6
1999 ◽
Vol 8
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2002 ◽
Vol 116
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pp. 2166-2174
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2010 ◽
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1999 ◽
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pp. 415-422
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2006 ◽
Vol 246
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pp. 317-325
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