Comment on “Folding in high-grade rocks due to back-rotation between shear zones” by Lyal B. Harris
Author:
Publisher
Elsevier BV
Subject
Geology
Reference13 articles.
1. From continental margin extension to collision orogen: structural development and tectonic rotation of the Hengchun peninsula, southern Taiwan;Chang;Tectonophysics,2003
2. The development of flanking folds during simple shear and their use as kinematic indicators;Grasemann;Journal of Structural Geology,2001
3. Folding in high-grade rocks due to back-rotation between shear zones;Harris;Journal of Structural Geology,2003
4. Mechanisms for folding of high-grade rocks in extensional tectonic settings;Harris;Earth-Science Reviews,2002
5. Near-orthogonal foliation development in orogens: meaningless complexity, or reflection of fundamental dynamic processes?;Johnson;Journal of Structural Geology,1999
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1. Geostatistical Determination of Ore Shoot Plunge and Structural Control of the Sizhuang World-Class Epizonal Orogenic Gold Deposit, Jiaodong Peninsula, China;Minerals;2019-04-04
2. The role of deformation in the formation of banded iron formation-hosted high-grade iron ore deposits, Hamersley Province (Australia);Precambrian Research;2017-07
3. Multiple faults in ductile simple shear: analogue models of flanking structure systems;Geological Society, London, Special Publications;2006
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