Structural Evolution of the Western Makran

• 作 者: CHU Yang CHEN Lin WAN Bo LIN W
• 机 构: InstituteofGeologyandGeophysics,InstituteforEarthSciences
• 出 处: 地质学报:英文版
• 发表日期: 2020年S01期
• 关键词: MAKRAN structural analysis polyphase deformation CENOZOIC
• 基金项目: granted by the National Natural Science Foundation of China(91855103,91855207 and 91855212),the Ministry of Science and Technology(2016YFC0600401 and 2016YFC0600102),the State Key Laboratory of Lithos

The Makran represents a huge accretionary wedge in SE Iran that resulted from the long-lasting subduction of the Neotethys Ocean since the Mesozoic. From west to east, this accretionary wedge extends ~1000 km between the Minab Fault in Iran, and the Ornac