<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Tamara Dudar</style></author><author><style face="normal" font="default" size="100%">Valentin Verkhovtsev</style></author><author><style face="normal" font="default" size="100%">Georgii Lysychenko</style></author><author><style face="normal" font="default" size="100%">Yurii Tyshchenko</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Radon Emanation as a Source of Radiation Hazard to the Environment: The Case of the Ukrainian Shield</style></title><secondary-title><style face="normal" font="default" size="100%">Information &amp; Security: An International Journal</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Central Ukrainian Uranium Province</style></keyword><keyword><style  face="normal" font="default" size="100%">radon emanation</style></keyword><keyword><style  face="normal" font="default" size="100%">Ukrainian Shield</style></keyword><keyword><style  face="normal" font="default" size="100%">uranium ore deposits</style></keyword><keyword><style  face="normal" font="default" size="100%">uranium ore manifestations</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><volume><style face="normal" font="default" size="100%">40</style></volume><pages><style face="normal" font="default" size="100%">51-57</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The article examines uranium ore manifestations, mining and associated radon emanation potential from the point of view of radiation hazard to the environment in the region of the Ukrainian Shield and its slopes, namely within the Central Ukrainian Uranium Province. The maximum amount of radon is established in the geodynamically active zones in overlapping rocks associated with new tectonic anomalies in parent rocks. Most hazardous are areas where new tectonic activation zones and uranium ore manifestations occur relatively close to the surface. The approach towards &amp;lsquo;radon-prone areas&amp;rsquo; in accordance with the European Basic Safety Standards is emphasized.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Valentin Verkhovtsev</style></author><author><style face="normal" font="default" size="100%">O. Kramar</style></author><author><style face="normal" font="default" size="100%">Yuliia Yuskiv</style></author><author><style face="normal" font="default" size="100%">Yevhen Krasnov</style></author><author><style face="normal" font="default" size="100%">Yurii Tyshchenko</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">New tectonics of the Belanovskyi iron and Kremenchuk uranium deposits (in Ukrainian)</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Geophysics</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><volume><style face="normal" font="default" size="100%">4</style></volume><pages><style face="normal" font="default" size="100%">136-148</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record></records></xml>