Mid-Neoproterozoic (ca. 830-800 Ma) metamorphic P-T paths link Tarim to the circum-Rodinia subduction-accretion system

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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...

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Bibliographic Details
Main Authors:	Ge, R., Zhu, W., Wilde, Simon
Format:	Journal Article
Published:	American Geophysical Union 2016
Online Access:	http://hdl.handle.net/20.500.11937/36013

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