Metamorphic constraints on the character and displacement of the South Tibetan fault system, central Bhutanese Himalaya
The South Tibetan fault system, a family of primarily extensional faults that separates the metamorphic core of the Himalaya (expressed as the Greater Himalayan sequence) from overlying, predominantly unmetamorphosed Tibetan sedimentary sequence units, has been mapped for over 2000 km coincident wit...
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Veröffentlicht in: | Lithosphere 2013-02, Vol.5 (1), p.67-81 |
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