HIGH-TI AMPHIBOLE AS A PETROGENETIC INDICATOR OF MAGMA CHEMISTRY: EVIDENCE FOR MILDLY ALKALIC-HYBRID MELTS DURING EVOLUTION OF VARISCAN BASIC–ULTRABASIC MAGMATISM OF CENTRAL IBERIA

MOLINA, J., SCARROW, J., & MONTERO, P.G.. (2009). HIGH-TI AMPHIBOLE AS A PETROGENETIC INDICATOR OF MAGMA CHEMISTRY: EVIDENCE FOR MILDLY ALKALIC-HYBRID MELTS DURING EVOLUTION OF VARISCAN BASIC–ULTRABASIC MAGMATISM OF CENTRAL IBERIA. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 158(-), 69-98. SID. https://sid.ir/paper/627466/en

MOLINA J., SCARROW J., MONTERO P.G.. HIGH-TI AMPHIBOLE AS A PETROGENETIC INDICATOR OF MAGMA CHEMISTRY: EVIDENCE FOR MILDLY ALKALIC-HYBRID MELTS DURING EVOLUTION OF VARISCAN BASIC–ULTRABASIC MAGMATISM OF CENTRAL IBERIA. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY[Internet]. 2009;158(-):69-98. Available from: https://sid.ir/paper/627466/en

J. MOLINA, J. SCARROW, and P.G. MONTERO, “HIGH-TI AMPHIBOLE AS A PETROGENETIC INDICATOR OF MAGMA CHEMISTRY: EVIDENCE FOR MILDLY ALKALIC-HYBRID MELTS DURING EVOLUTION OF VARISCAN BASIC–ULTRABASIC MAGMATISM OF CENTRAL IBERIA,” CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, vol. 158, no. -, pp. 69–98, 2009, [Online]. Available: https://sid.ir/paper/627466/en