HYPERSTHENE HORNFELSES OF THE KANDYGATAI COMPLEX, EASTERN KAZAKHSTAN
| dc.contributor.author | Sukhorukov V.P. | |
| dc.contributor.author | Plotnikov A.V. | |
| dc.date.accessioned | 2022-07-25T04:36:24Z | |
| dc.date.available | 2022-07-25T04:36:24Z | |
| dc.date.issued | 2004 | |
| dc.description.abstract | The Kandygatai metamorphic block is situated within the Zharma strike-slip zone, which separates the Hercynides of the Zaisan and Caledonides of the Chingiz-Tarbagatai fold systems. Metapelites of the Kandygatai Complex have already been considered in the literature. Based on findings of hypersthenesillimanite, corundum-garnet, and hypersthene-clinopyroxene assemblages, this complex was attributed to the high-pressure granulites (T = 950-1000°C, P = 10-12 kbar and interpreted as an ancient sialic basement unique for this region. The present paper considers new petrological data, which make it possible to attribute this complex to the high-temperature-lowpressure rocks and propose a two-stage model of its formation. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=13461971 | |
| dc.identifier.citation | Doklady Earth Sciences, 2004, 398, 7, 973-977 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38386 | |
| dc.title | HYPERSTHENE HORNFELSES OF THE KANDYGATAI COMPLEX, EASTERN KAZAKHSTAN | |
| dc.type | Статья |