FORMATION OF RINGWOODITE DURING SHOCK-WAVE LOADING OF TWO-MICA QUARTZ SCHIST: EXPERIMENTAL DATA
| dc.contributor.author | Kozlov E.A. | |
| dc.contributor.author | Sazonova L.V. | |
| dc.contributor.author | Fel'dman V.I. | |
| dc.contributor.author | Dubrovinskaya N.A. | |
| dc.contributor.author | Dubrovinskii L.S. | |
| dc.date.accessioned | 2022-01-15T07:43:07Z | |
| dc.date.available | 2022-01-15T07:43:07Z | |
| dc.date.issued | 2003 | |
| dc.description.abstract | Ringwoodite, a compact modification of olivine (γ-olivine), was experimentally synthesized under static loads (within the interval 6-24 GPa, depending on the composition and the olivine-ringwoodite conversion temperature) [1]. During the joint experimental study of shock metamorphism of rocks conducted by researchers from the All-Russia Research Institute of Technical Physics (Russian Federal Nuclear Center) and the Department of Petrology (Moscow State University), ringwoodite was first obtained under shock-wave loading conditions. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=13438641 | |
| dc.identifier.citation | Doklady Earth Sciences, 2003, 390, 4, 571-573 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/34337 | |
| dc.title | FORMATION OF RINGWOODITE DURING SHOCK-WAVE LOADING OF TWO-MICA QUARTZ SCHIST: EXPERIMENTAL DATA | |
| dc.type | Статья |