Article ID Journal Published Year Pages File Type
6443722 Gondwana Research 2013 14 Pages PDF
Abstract
► Northern protoliths were Carboniferous, whereas in the south deposition was Permian. ► Detrital zircon LuHf and O isotopes indicate mature crustal igneous source rocks. ► Devonian accretion north of 39°S was coeval with subduction to the south.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Authors
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