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- W2178887795 abstract "The ductile shear zones in Thailand are commonly expressed by the NW–SE and NNE–SSW trending strike–slip systems such as the Mae Ping, Three Pagodas, Ranong, and Khlong Marui shear zones. The meso- and microstructures of the mylonites within the shear zones, which present the strong kinematic indicators and dynamic recrystallization, were combined with the geochronologic data. The result shows that the sinistral shear along the NW–SE Mae Ping and Three Pagodas shear zones occurred in the Eocene–Oligocene, and the dextral shear along the NNE–SSW Ranong and Khlong Marui shear zones occurred in the Eocene. Dextral shear in the Ranong shear zone could have also been in the Late Cretaceous." @default.
- W2178887795 created "2016-06-24" @default.
- W2178887795 creator A5033086086 @default.
- W2178887795 date "2015-10-09" @default.
- W2178887795 modified "2023-10-14" @default.
- W2178887795 title "Strike-slip ductile shear zones in Thailand" @default.
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