Defining the Himalayan Main Central Thrust in Nepal
An inverted metamorphic field gradient associated with a crustal-scale south-vergent thrust fault, the Main Central Thrust, has been recognized along die Himalaya for over 100 years. A major problem in Himalayan structural geology is that recent workers have mapped the Main Central Thrust within the...
Những tác giả chính: | Searle, M, Law, R, Godin, L, Larson, K, Streule, M, Cottle, J, Jessup, M |
---|---|
Định dạng: | Journal article |
Ngôn ngữ: | English |
Được phát hành: |
2008
|
Những quyển sách tương tự
-
The structural, metamorphic and magmatic evolution of the Greater Himalayan Sequence and Main Central Thrust, Eastern Nepal Himalaya
Bằng: Streule, M
Được phát hành: (2009) -
Pressure-temperature-time path discontinuity in the Main Central thrust zone, Central Nepal: Comment
Bằng: Searle, M, et al.
Được phát hành: (2002) -
Structure of the Main Central Thrust zone and extrusion of the High Himalayan deep crustal wedge, Kishtwar-Zanskar Himalaya
Bằng: Stephenson, B, et al.
Được phát hành: (2001) -
Locking of southward extrusion in favour of rapid crustal-scale buckling of the Greater Himalayan sequence, Nar valley, central Nepal
Bằng: Godin, L, et al.
Được phát hành: (2006) -
Fluvial sedimentary response to late quaternary climate and tectonics at the Himalayan frontal thrust, Central Nepal
Bằng: Hamahashi, Mari, et al.
Được phát hành: (2023)