Structural evolution of the Irtysh Shear Zone (northwestern China) and implications for the amalgamation of arc systems in the Central Asian Orogenic Belt
详细信息 查看全文
- 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 ; Yang Yua
- 关键词：Central Asian Orogenic Belt ; Irtysh Shear Zone ; Chinese Altai ; Junggar ; Accretionary orogen ; Structural synthesis
- 刊名：Journal of Structural Geology
- 出版年：2015
- 出版时间：November 2015
- 年：2015
- 卷：80
- 期：Complete
- 页码：142-156
- 全文大小：5008 K
文摘
- •
The Irtysh Shear Zone is a major tectonic boundary in the Central Asia Orogenic Belt.
- •
Three episodes of late Paleozoic deformation (D1–D3) were recognized.
- •
D1–D3 were associated with convergence of arc systems.
- •
D1–D3 represent orogenic thickening, collapse and transpressional deformation.
- •
D3 was possibly reactivated in the Mesozoic to Cenozoic.