Time‐scale of deformation and intertectonic phases revealed by P–T–D–t relationships in the orogenic middle crust of the Orlica‐Śnieżnik Dome, Polish/Czech Central Sudetes

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JOURNAL OF METAMORPHIC GEOLOGY, Vol. 32, Iss. 9, 2014-12 ,pp. : 981-1003

John Wiley & Sons Inc

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P–T–t–D record of crustal‐scale horizontal flow and magma‐assisted doming in the SW Mongolian Altai

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JOURNAL OF METAMORPHIC GEOLOGY, Vol. 33, Iss. 4, 2015-05 ,pp. : 359-383

John Wiley & Sons Inc

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Subduction- and non-subduction-related igneous rocks in the Central European Variscides: geochemical and Nd isotope evidence from the Klodzko Metamorphic Complex, Polish Sudetes

By Kryza R.   Mazur S.   Pin C.  

Geodinamica Acta, Vol. 16, Iss. 1, 2003-01 ,pp. : 39-57

Elsevier

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P-T-X evolution in garnet pyroxenites from Tin Begane (Central Hoggar, Algeria)

By Derridj A.   Ouzegane K.   Kienast J.-R.   Belhai D.  

Journal of African Earth Sciences and the Middle East, Vol. 37, Iss. 3, 2003-10 ,pp. : 257-268

Elsevier

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Use of T_max as a thermal maturity indicator in orogenic successions and comparison with clay mineral evolution

By Dellisanti F.   Pini G. A.   Baudin F.  

Clay Minerals, Vol. 45, Iss. 1, 2010-03 ,pp. : 115-130

Mineralogical Society

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