作者: Marcel Maruntiu , Vera Johan , Viorica Iancu , Patrick Ledru , Alain Cocherie
DOI: 10.1016/S1251-8050(99)80182-7
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摘要: A kyanite-bearing eclogite from the pre-Alpine basement of Southern Carpathians (Leaota Mountains, Romania) shows a complete prograde metamorphic evolution, reaching pressures in excess 20 kbar, followed by retrograde path with decreasing pressure and temperature. It brings new evidence that this constitutes continental collision belt, probably Variscan age.