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| 001 | 180307 | ||
| 005 | 20231029194901.0 | ||
| 035 | _a(RuTPU)RU\TPU\book\195459 | ||
| 035 | _aRU\TPU\book\194785 | ||
| 090 | _a180307 | ||
| 100 | _a20100513d2007 k y0rusy50 ca | ||
| 101 | 1 |
_aeng _crus |
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| 102 | _aRU | ||
| 135 | _adrnn ---uucaa | ||
| 200 | 1 |
_aDiorites as an intermediate in gold-producing fluid-magmatic granite-doleritic complexes _bElectronic resource _fI. V. Kucherenko |
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| 203 |
_aText _celectronic |
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| 215 | _a1 файл (1.2 Мб) | ||
| 225 | 1 | _aEarth science | |
| 230 | _aЭлектронные текстовые данные (1 файл : 1.2 Мб) | ||
| 300 | _aЗаглавие с титульного листа | ||
| 300 | _aЭлектронная версия печатной публикации | ||
| 320 | _a[Bibliography: p. 11 (14 titles)] | ||
| 330 | _aOn the example of the Kedrovskiy deposit of North Transbaikalia, conditions of gold-producing fluid-magmatic granite-dolerite complex's making are concretized. Participation in its structure of average igneous rocks, emphasizing in magmatism's generalized antidrome scheme an evolutionary change of early ultrametamorphical granodiorites and quartz diorites of focal-dome construction by moderately alkali quartz diorite porphyrites and further - accompanied by ore-formation of moderate alkaline basaltoids in dyke's facio is shown and is discussed. Presence of diorites in other mesothermal gold deposits reflects, as it is represented, prevalence of the phenomenon of evolutionary transition from early to late magmatities of the discussed fluid-magmatic complexes and explains the expediency of its further studying. | ||
| 337 | _aAdobe Reader | ||
| 461 | 1 |
_0(RuTPU)RU\TPU\book\169973 _tBulletin of the Tomsk Polytechnic University _fTomsk Polytechnic University (TPU) _d2006-2007 |
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| 463 | 1 |
_0(RuTPU)RU\TPU\book\195457 _tVol. 310, № 1 _v[P. 6-11] _d2007 _p201 p. |
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| 610 | 1 | _adiorites | |
| 610 | 1 | _aintermediate | |
| 610 | 1 | _agold-producing complexes | |
| 610 | 1 | _afluid-magmatic complexes | |
| 610 | 1 | _agranite-doleritic complexes | |
| 610 | 1 | _aKedrovskiy deposit | |
| 610 | 1 | _aNorth Transbaikalia | |
| 610 | 1 | _aigneous rocks | |
| 610 | 1 | _aantidrome scheme | |
| 610 | 1 | _amagmatism | |
| 610 | 1 | _aultrametamorphical granodiorites | |
| 610 | 1 | _aquartz diorites | |
| 610 | 1 | _afocal-dome constructions | |
| 610 | 1 | _aquartz porphyrites | |
| 610 | 1 | _adiorite porphyrites | |
| 610 | 1 | _aore-formation | |
| 610 | 1 | _aalkaline basaltoids | |
| 610 | 1 | _adyke's facio | |
| 610 | 1 | _amesothermal gold deposits | |
| 610 | 1 | _aevolutionary transition | |
| 610 | 1 | _amagmatities | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aэлектронный ресурс | |
| 675 |
_a553.411.071:552.322 _v3 |
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| 700 | 1 |
_aKucherenko _bI. V. _cGeologist _cProfessor and consultant of Tomsk Polytechnic University, Doctor of geological and mineralogical sciences _f1937- _gIgor Vasilyevich _2stltpush _3(RuTPU)RU\TPU\pers\32569 |
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| 801 | 1 |
_aRU _b63413507 _c20090623 _gPSBO |
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| 801 | 2 |
_aRU _b63413507 _c20160212 _gPSBO |
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| 856 | 4 | _uhttp://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v310eng/i1/01.pdf | |
| 942 | _cCF | ||