Serpentinites of the Ural: Mineralogical Features, Petrophysical Properties and Subduction Processes

Авторы: Posukhova T.V., Panasian L.L., Sas I.E.
Журнал: Open Journal of Geology
Том: 3
Номер: 3
Год издания: 2013
Первая страница: 250
Последняя страница: 261
DOI: 10.4236/ojg.2013.33029
Аннотация: The article presets the results of study of composition, structure and properties of three genetic types of serpentinites from Ural: developed by chromite-bearing ultrabasic rocks, by metamorphic zones of carbonate rocks and within the zone of weathering of ultrabasic rocks. The samples were selected from deposits, located along the Main Ural Fault – the Paleozoic subduction zone (named GUR). Peculiarities of microstructure, chemical composition and properties of serpentinites formed in different geological conditions were investigated and their comparative study was held. Were devided three groups of serpentinites with oriented and non-oriented structure which formed by different protholites: mantle, lithosphere and crust.
Добавил в систему: Посухова Татьяна Владимировна

	ИСТИНА	Войти в систему Регистрация
	ИСТИНА ИНХС РАН
	Главная Поиск Статистика О проекте Помощь

ИСТИНА