Article ID Journal Published Year Pages File Type
4732873 Journal of Asian Earth Sciences 2006 14 Pages PDF
Abstract
The gneisses have been formed from a granitic protolith by a continuous fabric transformation on a retrograde metamorphic path. All structures in the gneisses can be assigned to the ascent and emplacement of batholiths in an active strike-slip belt.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
The formation of gneisses in the Southern East Uralian Zone-a result of Late Palaeozoic granite ascent and emplacement
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