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| 001 | 655114 | ||
| 005 | 20231030041330.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\20932 | ||
| 035 | _aRU\TPU\network\19474 | ||
| 090 | _a655114 | ||
| 100 | _a20170703a2016 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 102 | _aUS | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aUnknown mechanisms of granitization of basalts _fS. L. Shvartsev |
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| 203 |
_aText _celectronic |
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| 300 | _aTitle screen | ||
| 320 | _a[References: p. 525-526 (32 tit.)] | ||
| 330 | _aBack in the late 18th century, J.-B. Lamarck, a famous French representative of Neptunism, believed that granites were of aqueous origin, but at that time he could not provide compelling data to substantiate his point of view, and the opinion of Plutonists, who held that granites had a magmatic genesis, won. The latter approach was challenged by V.I. Vernadsky, who considered granites as “traces of bygone biospheres.” However, even today geological science follows the views of Plutonists despite insuperable barriers on this way. The author of this article substantiates a fundamentally new and previously unknown mechanism of granite formation through the transformation of basalts by water. He shows that the water–basalt system always contains a nonequilibrium state that ensures the continuous dissolution of the latter and the formation of new minerals and entire rock massifs, the composition of which depends on the time of evolution of the water–rock system. The granitization of basalts is the final stage of evolution in nonliving matter. | ||
| 333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
| 461 | _tHerald of the Russian Academy of Sciences | ||
| 463 |
_tVol. 86, iss. 6 _v[P. 513–526] _d2016 |
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| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aбазальты | |
| 610 | 1 | _aграниты | |
| 610 | 1 | _aтермодинамическое равновесие | |
| 610 | 1 | _aвода-порода | |
| 610 | 1 | _aвзаимодействие | |
| 610 | 1 | _aгидрогеохимия | |
| 610 | 1 | _abasalts | |
| 610 | 1 | _agranites | |
| 610 | 1 | _athermodynamic equilibrium | |
| 610 | 1 | _awater–rock system | |
| 610 | 1 | _aevolution in nonliving matter | |
| 610 | 1 | _astages of interaction between water and basalts | |
| 610 | 1 | _atime of interaction | |
| 610 | 1 | _ahydrogeochemistry | |
| 700 | 1 |
_aShvartsev _bS. L. _cRussian hydrogeologist, Doctor of Geological and Mineralogical sciences _cProfessor of the TPU, Member of the Academy of Natural sciences _f1936- _gStepan Lvovich _2stltpush _3(RuTPU)RU\TPU\pers\24144 |
|
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bКафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ) _h100 _2stltpush _3(RuTPU)RU\TPU\col\18664 |
| 801 | 2 |
_aRU _b63413507 _c20170703 _gRCR |
|
| 856 | 4 | _uhttp://dx.doi.org/10.1134/S1019331616060149 | |
| 942 | _cCF | ||