Cosmostructural model of the Kalgutinskiy rare-metal deposit area (Mountainous Altai); Bulletin of the Tomsk Polytechnic University; Vol. 311, № 1
| Parent link: | Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007 Vol. 311, № 1.— 2007.— [P. 42-49] |
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| Tác giả khác: | , , , , , |
| Tóm tắt: | 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 |
| Ngôn ngữ: | Tiếng Anh |
| Được phát hành: |
2007
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| Loạt: | Geology and minerals |
| Những chủ đề: | |
| Truy cập trực tuyến: | http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v311eng/i1/07.pdf |
| Định dạng: | Điện tử Chương của sách |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=182500 |
| Mô tả vật lý: | 1 файл (1.2 Мб) |
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| Tóm tắt: | 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 |