Dome Formation During Crustal Extension in the Himalaya: Kinematic and Pressure-Temperature-Time-Deformation Constraints on Extensional Exhumation Along the Southern Margin of the Tibetan Plateau
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- Published
- 2012-01-01
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- 0
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- 157
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- https://api.semanticscholar.org/CorpusID:127872443
References
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- The geodynamic equation of state: What and how
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- Gneiss domes, metamorphic core complexes, and wrench zones: Thermal and structural evolution of the Niğde Massif, central Anatolia
- The role of extension during brittle deformation within the NW Indian Himalaya
- Exhumation history of the deepest central Himalayan rocks, Ama Drime range: Key pressure‐temperature‐deformation‐time constraints on orogenic models
- An internally consistent thermodynamic data set for phases of petrological interest
- Exhumation of the ultrahigh‐pressure Tso Morari unit in eastern Ladakh (NW Himalaya): A case study
- Middle to late Miocene extremely rapid exhumation and thermal reequilibration in the Kung Co rift, southern Tibet
- Isotopic characteristics of the Gurla Mandhata metamorphic core complex: Implications for the architecture of the Himalayan orogen
- Orogen-parallel extension in Himalaya: Is it the indicator of collapse or the product in process of compressive uplift?
- The eastern Tonale fault zone: a ‘natural laboratory’ for crystal plastic deformation of quartz over a temperature range from 250 to 700 °C
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- Tectonics and structural zonation of southern Tibet, China
- Tectonic controls on metamorphism, partial melting, and intrusion: timing and duration of regional metamorphism and magmatism in the Niğde Massif, Turkey
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