Mantle magma-thermofluidodynamic and intracrustal granitoid-hydrothermal-metasomatic auriferous systems
| Parent link: | Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007 Vol. 311, № 1.— 2007.— [P. 34-42] |
|---|---|
| প্রধান লেখক: | |
| সংক্ষিপ্ত: | Заглавие с титульного листа Электронная версия печатной публикации Contents of typical models of formation of abyssal and intra-core ore-forming systems are discussed. As it has been already marked, the interaction between core and mantle ore-forming systems occurred at formation of large and unique golden-ore deposits. The interaction of the abyssal mantle substance with formations of the Earth's crust has been carried out by penetration of high-temperature gas-fluids, magmatic melts and solid bodies, forming diapiric magma-thermofluidodynamic systems on borders of the inner core with the bottom mantle and within the limits of the upper mantle - the Earth's crust |
| ভাষা: | ইংরেজি |
| প্রকাশিত: |
2007
|
| মালা: | Geology and minerals |
| বিষয়গুলি: | |
| অনলাইন ব্যবহার করুন: | http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v311eng/i1/06.pdf |
| বিন্যাস: | বৈদ্যুতিক গ্রন্থের অধ্যায় |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=182495 |