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GGU281
GGU281
http://dx.doi.org/10.1093/GJI/GGU281
Normal thickness of the upper mantle transition zone in NE Brazil does not favour mantle plumes as origin for intraplate Cenozoic volcanism
P356
Q57977474-DBADF8AE-7C68-410E-BF6E-A2A2DADC5071
P356
GGU281
http://dx.doi.org/10.1093/GJI/GGU281