Dmitry D. BADJUKOV1*, Franz BRANDSTA¨ TTER2, Jouko RAITALA3, and Gero KURAT2
1V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry RAS, 19, Kosygin str., 119991, Moscow, Russia
2Naturhistorisches Museum, Burgring 7, Wien A-1010, Austria
3Astronomy, Department of Physical Sciences, P.O. box 3000, FIN-90014 University of Oulu, Oulu, Finland
(Received 12 November 2009; revision accepted 13 August 2010)
Abstract–A large number of micrometeorites (MMs) was recovered from glacier deposits located at the north-eastern passive margin of the Novaya Zemlya glacier sheet. Melted, scoriaceous, and unmelted micrometeorites (UMMs) are present. Unmelted micrometeorites are dominated mostly by chondritic matter, but also a few achondritic MMs are present.
Here we report the discovery of four UMMs that, according to their texture, mineralogy, and chemistry, are identified as basaltic breccias...