naa a22 4500 510736513 CHVBK 20180411083012.0 cr unu---uuuuu 180411e20131201xx s 000 0 eng 10.1134/S1075701513080059 doi (NATIONALLICENCE)springer-10.1134/S1075701513080059 Morphological evidence for diffusion-controlled growth of garnet from metapelites [Elektronische Daten] [Yu. Gulbin, A. Glazov] The surface microtopography of garnet from metamorphic schists of the northern Ladoga region has been investigated. The morphology of garnet is distinguished by a rough stepped surface on dodecahedral faces {110} and by the absence of sharp crystal edges. As follows from experimental results on crystal growth under hydrothermal conditions, the microtopography pattern gives evidence for a highly oversaturated inter-granular medium and the important role of diffusion as a factor controlling garnet growth. Pleiades Publishing, Ltd., 2013 Gulbin Yu St. Petersburg State Mining University, 21-aya liniya 2, St. Petersburg, 199106, St. Petersburg, Russia aut Glazov A. St. Petersburg State Mining University, 21-aya liniya 2, St. Petersburg, 199106, St. Petersburg, Russia aut Geology of Ore Deposits Springer US; http://www.springer-ny.com 55/8(2013-12-01), 686-691 1075-7015 55:8<686 2013 55 11477 https://doi.org/10.1134/S1075701513080059 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1134/S1075701513080059 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Gulbin Yu St. Petersburg State Mining University, 21-aya liniya 2, St. Petersburg, 199106, St. Petersburg, Russia aut NATIONALLICENCE 700 1- Glazov A. St. Petersburg State Mining University, 21-aya liniya 2, St. Petersburg, 199106, St. Petersburg, Russia aut NATIONALLICENCE 773 0- Geology of Ore Deposits Springer US; http://www.springer-ny.com 55/8(2013-12-01), 686-691 1075-7015 55:8<686 2013 55 11477 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer