Ultra-high temperature granulite-facies metamorphic rocks from the Mozambique belt of SW Tanzania
Review articleOpen access
H. Sommer - No affiliation found
2013/06/01 Full-length article DOI: 10.1016/j.lithos.2013.02.014
Highlights•We present here for the first time a 5 segment P–T path.•New evidence for a continent–continent collision setting in the studied area.•Orogenic collapse and related rifting after continent–continent collision.•The beginning of the collision of East and West Gondwana at ~ 730 Ma.
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