New data of typomorphic features of diamonds from placers in North Timan

The morphological and spectral-optical properties of diamond crystals from placers in North Timan rivers have been studied with IR-spectroscopy and cathode luminescence methods. As a result, correlation between external characteristics of diamonds (size and degree of mechanical damage) and number of optically active centers has been revealed. The habit and the type of distribution of structural defects in diamond crystals studied are comparable with those in diamonds from the Archangelsk Region and North Timan’s placers. Based on the obtained data, origin issues and possible primary sources of diamonds from North Timan’s placers are discussed.     

Development and evolution of water vapor vesicles during fast thermal breakdown of muscovite

At 1,175°C-1 bar, muscovite in natural granite powders is completely transformed after 5 min. Due to the overlapping of several processes such as dehydroxylation, mineralogical transformations, collapse and sintering of transformed lamellae, a few parts per thousand of H₂O vapor are trapped, generating bubbles in muscovite pseudomorphs. For short durations (5–40 min), the crystallographic properties of the precursor muscovite control the geometry of the bubbles that may be compared to thick disks with a rounded shape in basal sections and an elongated shape in lateral section, parallel to the former cleavage planes of muscovite. With longer durations the bubbles change from thick disks to spheres, which can be explained by the release of constraints perpendicular to basal planes upon growth of the high temperature Si–Al oxides. With time, the number of bubbles decreases while the bubble size and the porosity of the pseudomorphs increase. Bubble behavior was analyzed in terms of ripening, shape transformations and coalescence.