Unknown mechanisms of granitization of basalts / S. L. Shvartsev

Уровень набора: Herald of the Russian Academy of SciencesОсновной Автор-лицо: Shvartsev, S. L., Russian hydrogeologist, Doctor of Geological and Mineralogical sciences, Professor of the TPU, Member of the Academy of Natural sciences, 1936-, Stepan LvovichКоллективный автор (вторичный): Национальный исследовательский Томский политехнический университет (ТПУ), Институт природных ресурсов (ИПР), Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)Язык: английский.Страна: .Резюме или реферат: Back 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..Примечания о наличии в документе библиографии/указателя: [References: p. 525-526 (32 tit.)].Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | базальты | граниты | термодинамическое равновесие | вода-порода | взаимодействие | гидрогеохимия | basalts | granites | thermodynamic equilibrium | water–rock system | evolution in nonliving matter | stages of interaction between water and basalts | time of interaction | hydrogeochemistry Ресурсы он-лайн:Щелкните здесь для доступа в онлайн
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[References: p. 525-526 (32 tit.)]

Back 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.

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