Transpressional deformation, strain partitioning and fold superimposition in the southern Chinese Altai, Central Asian Orogenic Belt
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- 作者：Pengfei Lia ; pengfei@hku.hk" class="auth_mail" title="E-mail the corresponding author ; pengfeili2013@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Min Suna ; Gideon Rosenbaumb ; Keda Caic ; Ming Chena ; Yulin Hea
- 关键词：Central Asian Orogenic Belt ; Chinese Altai ; Irtysh Shear Zone ; Transpression ; Strain partitioning
- 刊名：Journal of Structural Geology
- 出版年：2016
- 出版时间：June 2016
- 年：2016
- 卷：87
- 期：Complete
- 页码：64-80
- 全文大小：7817 K
文摘
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Four generations of structures are recognized in the southern Chinese Altai.
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S1 and S2 may result from crustal thickening and thinning.
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F3 and F4 are linked with partitioning of transpressional deformation.
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Sub-parallelism of F3 with the shear zone results from high degree of partitioning.
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Less efficient strain partitioning leads to the obliquity of F4 with the shear zone.
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