On the Formation of K-Feldspar Augens - An Example from the Central Crystallines of the Bhutan Himalaya
Abstract
Mesoscopic and microscopic studies on the K-feldspar augens of Thimphu augengneiss of Bhutan suggests microshearing followed by a rotational mechanism. Megacrysts of K-feldspar are often broken into smaller segments by ductile shear faulting, followed by a combination of simple shear and flattening deformation giving rise to the augens.Downloads
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Research Papers
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Published
1985-09-01
How to Cite
Roy, A. (1985). On the Formation of K-Feldspar Augens - An Example from the Central Crystallines of the Bhutan Himalaya. Journal of Geological Society of India, 26(9), 652–658. Retrieved from https://geosocindia.com/index.php/jgsi/article/view/65834