Mid-Neoproterozoic (ca. 830-800 Ma) metamorphic P-T paths link Tarim to the circum-Rodinia subduction-accretion system
Long-lived exterior accretionary orogeny shapes tectonothermal evolution of the peripheral building blocks of supercontinents and leads to considerable crustal growth. However, such accretionary orogeny has only been locally recognized for the Rodinia supercontinent. Here a suite of newly discovered...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
American Geophysical Union
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/36013 |