Tectonics of the Himalaya and southern Tibet from two perspectives¶
Hodges. (2000). Tectonics of the Himalaya and southern Tibet from two perspectives.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Orogenic Belt
- Reading a transect from north to south exposes the full zonation: the Indus–Yarlung suture marks where the two plates joined; south of it the high-grade metamorphic core (the Greater Himalayan Sequence, amphibolite-to-granulite facies rocks exhumed from depth) forms the hinterland; and the deformation steps outward through a sequence of major thrusts — the Main Central Thrust, then the Main Boundary Thrust, then the active Main Frontal Thrust
This sourceA synthesis of Himalayan and southern-Tibetan tectonics since India-Eurasia collision at ca. 50 Ma.
Supported in partVerified against the publisher's abstract
“This paper is an attempt to synthesize the known geology of this orogenic system, with special attention paid to the tectonic evolution of the Himalaya and southernmost Tibet since India-Eurasia collision at ca. 50 Ma.”
- Reading a transect from north to south exposes the full zonation: the Indus–Yarlung suture marks where the two plates joined; south of it the high-grade metamorphic core (the Greater Himalayan Sequence, amphibolite-to-granulite facies rocks exhumed from depth) forms the hinterland; and the deformation steps outward through a sequence of major thrusts — the Main Central Thrust, then the Main Boundary Thrust, then the active Main Frontal Thrust
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Registry ID ref:dbbf32a3d31a · see in the full table