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J. Avouac, E. Burov (1996)
Erosion as a driving mechanism of intracontinental mountain growthJournal of Geophysical Research, 101
O. Zienkiewicz, R. Taylor, J. Zhu, Elsevier Bl, Ttfrworth Hhintalann (1977)
The finite element method
I. Likhanov, O. Polyansky, V. Reverdatto, I. Memmi (2004)
Evidence from Fe‐ and Al‐rich metapelites for thrust loading in the Transangarian region of the Yenisey Ridge, eastern SiberiaJournal of Metamorphic Geology, 22
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ISSN 1028-334X, Doklady Earth Sciences, 2006, Vol. 408, No. 4, pp. 652â656. © Pleiades Publishing, Inc., 2006. Original Russian Text © S.N. Korobeinikov, O.P. Polyansky, I.I. Likhanov, V.G. Sverdlova, V.V. Reverdatto, 2006, published in Doklady Akademii Nauk, 2006, Vol. 408, No. 4, pp. 512â516. GEOCHEMISTRY S. N. Korobeinikova, b, O. P. Polyanskyc, I. I. Likhanovc, V. G. Sverdlovac, and Academician of the RAS V. V. Reverdattoc Received January 12, 2006 DOI: 10.1134/S1028334X06040325 Regional structural features of the Yenisei Ridge are traditionally displayed as a NW-trending linear system of tectonic sheets that are thrust over one another and separated by faults where collision of blocks occurs (Fig. 1). As a result, low- and moderate-pressure series of regional metamorphism turn out to be juxtaposed. Moderate-pressure metamorphism related to collision [1] is locally superimposed on low-pressure metamorphic rocks. Therefore, andalusite is progressively replaced with kyanite, and new mineral assemblages of moderate pressure and deformational microstructures are formed. The replacement of andalusite by kyanite in the Yenisei Ridge is not a common phenomenon, because the stationary continental geotherm, as a rule, does not intersect the andalusiteâkyanite equilibrium line. According to the results of mineralogicalâpetrographic and structural studies and the geothermobarometric data obtained
Doklady Earth Sciences – Springer Journals
Published: May 1, 2006
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