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Transformation of the Surface Structure of Marble under the Action of a Shock Wave


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

The structure of marble fracture fragments formed after the destruction under the action of a shock wave have been analyzed by Raman, infrared, and luminescence spectroscopic techniques. It has been found that calcite I in the surface layer of fragments with thicknesses of about 2 μm is transformed into high-pressure phase calcite III. At the same time, concentrations of Mn2+, Eu3+, and other ions decrease to about onefourth of their initial values.

Авторлар туралы

I. Shcherbakov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 194021

V. Vettegren

Ioffe Institute

Хат алмасуға жауапты Автор.
Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 194021

A. Bashkarev

Peter the Great St. Petersburg Polytechnic University

Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 195251

R. Mamalimov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 194021

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