Petrotectonic evolution of the high- to ultrahigh-pressure Maksyutov Complex, Karayanova area, south Ural Mountains: structural and oxygen isotope constraints-Reference-Cited by-同舟云学术

Petrotectonic evolution of the high- to ultrahigh-pressure Maksyutov Complex, Karayanova area, south Ural Mountains: structural and oxygen isotope constraints

Published:2000-04 Issue:1-4 Volume:52 Page:235-252
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Leech Mary L,Ernst W.G

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference43 articles.

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2. Mineral assemblages and retrograde P–T path for high- to ultrahigh-pressure metamorphism in the lower unit of the Maksyutov Complex, southern Ural Mountains, Russia;Beane;Isl. Arc,1995

3. Orogenic evolution of the Ural Mountains: results from an integrated seismic experiment;Berzin;Science,1996

4. Crustal-scale structure and evolution of an arc–continent collision zone in the southern Urals, Russia;Brown;Tectonics,1998

5. The structural architecture of the footwall to the Main Uralian Fault, southern Urals;Brown;Earth Sci. Rev.,1996

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