Reply to J. Berger's comment on the article “Discovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif” by Thiéry, V. et al.,. (2015), Gondwana Research 28, 954–960

Author:

Thiéry V.,Rolin P.,Dubois M.,Caumon M.-C.,Goncalves P.

Publisher

Elsevier BV

Subject

Geology

Reference28 articles.

1. Experimental evidence of decompression melting during exhumation of subducted continental crust;Auzanneau;Contributions to Mineralogy and Petrology,2006

2. Comment on “Discovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif Central.”;Berger;Gondwana Research,2015

3. Ocean-floor hydrothermal metamorphism in the Limousin ophiolites (western French Massif Central): evidence of a rare preserved Variscan oceanic marker;Berger;Journal of Metamorphic Geology,2005

4. Comment on “Diamond, former coesite and supersilicic garnet in metasedimentary rocks from the Greek Rhodope: a new ultrahigh-pressure metamorphic province established” by E.D. Mposkos and D.K. Kostopoulos [Earth Planet. Sci. Lett. 192 (2001) 497–506].;Beyssac;Earth and Planetary Science Letters,2003

5. Pressure–temperature phase diagram of elemental carbon;Bundy;Physica A: Statistical Mechanics and its Applications,1989

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