Cosmostructural model of the Kalgutinskiy rare-metal deposit area (Mountainous Altai)

Bibliographic Details
Parent link:Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007
Vol. 311, № 1.— 2007.— [P. 42-49]
Other Authors: Potseluev A. A., Ananyev Yu. S. Yuri Sergeyevich, Annikova I. Yu., Vladimirov A. G., Vasilevskiy A. N., Vitte L. V.
Summary:Заглавие с титульного листа
Электронная версия печатной публикации
Cosmostructures of the Kalgutinskiy rare-metal deposit area (Mountainous Altai) have been studied on the materials of multispectral space survey Landsat ETM+ and radar-tracking survey SRTM. The area is localized inside of the large ring structure of a complex construction, characterized by the long multistage (multipulse) development. Immersing of the root (focus) part of the structure from the north - northwest to the east - southeast is established. Position of the ring structure is controlled by the crossing knot of fracture zones of northwest, northeast and northeast - sublatitudinal directions. The Kalgutinskiy granite massif and the deposit itself are located in the internal belt of the structure in the ring 15,2 km in diameter. The perspective of ore-bearing ability of the southeast part of the area is highly evaluated in connection with development of small ring structures of the second type
Published: 2007
Series:Geology and minerals
Subjects:
Online Access:http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v311eng/i1/07.pdf
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=182500