P–T–t evolution of spinel–cordierite–garnet gneisses from the Sauwald Zone (Southern Bohemian Massif, Upper Austria): is there evidence for two independent late-Variscan low-P/high-T events in the Moldanubian Unit?

By Tropper P.   Deibl I.   Finger F.   Kaindl R.  

International Journal of Earth Sciences, Vol. 95, Iss. 6, 2006-11 ,pp. : 1019-1037

Springer Publishing Company

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Retrograde metamorphism of the Wongwibinda Complex, New England Fold Belt and the implications of 2.5D subsurface geophysical structure for the metamorphic history

By Danis C. R.   Daczko N. R.   Lackie M. A.   Craven S. J.  

Australian Journal of Earth Sciences, Vol. 57, Iss. 3, 2010-04 ,pp. : 357-375

Taylor & Francis Ltd

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Tracing the high pressure stage in the polymetamorphic Texel Complex (Austroalpine basement unit, Eastern Alps): P–T–t–d constraints

By Habler G.   Thöni M.   Sölva H.  

Mineralogy and Petrology, Vol. 88, Iss. 1-2, 2006-09 ,pp. : 269-296

Springer Publishing Company

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P–T and fluid evolution of barren and lithium pegmatites from Vlastějovice, Bohemian Massif, Czech Republic

By Ackerman Lukáš   Zachariáš Jiří   Pudilová Marta  

International Journal of Earth Sciences, Vol. 96, Iss. 4, 2007-08 ,pp. : 623-638

Springer Publishing Company

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Subduction-related P–T path for eclogites and garnet glaucophanites from the Samaná Peninsula basement complex, northern Hispaniola

By Escuder-Viruete J.   Pérez-Estaún A.  

International Journal of Earth Sciences, Vol. 95, Iss. 6, 2006-11 ,pp. : 995-1017

Springer Publishing Company

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