Growth of chloritoid and garnet along a nearly isothermal burial path to 70 km depth: an example from the Bughea Metamorphic Complex, Leaota Massif, South Carpathians

Author:

Negulescu Elena,Săbău GavrilORCID,Massonne Hans-Joachim

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference59 articles.

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2. Balintoni I, Balica C, Ducea MN, Chen F, Hann H, Şabliovschi V (2009) Late Cambrian–Early Ordovician Gondwanan terranes in the Romanian Carpathians: A zircon U–Pb provenance study. Gondwana Res 16:119–133

3. Bernhardt HJ, Massonne H-J, Reinecke T, Reinhardt J, Willner A (1995) Digital element distribution maps, an aid for petrological investigations. Ber Dtsch Mineral Ges, Beih Eur J Mineral 7(1):28

4. Chopin C, Schreyer W (1983) Magnesiocarpholite and magnesiochloritoid: two index minerals of pelitic blueschists and their preliminary phase relations in the model system MgO-Al2O3-SiO2-H2O. Am J Sci 283-A:72–96

5. Connolly JAD (1990) Multivariable phase diagrams: an algorithm based on generalized thermodynamics. Am J Sci 290:666–718

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