Ninety million years of orogenesis, 250 million years of quiescence and further orogenesis with no change in PT: Significance for the role of deformation in porphyroblast growth
In situ dating of monazite grains preserved as inclusions within foliations defining FIAs (foliation inflection/intersection axes preserved within porphyroblasts) contained within garnet, staurolite, andalusite and cordierite porphyroblasts provides a chronology of ages that matches the FIA success...
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| Format: | Journal Article |
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Indian Academy of Sciences
2012
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| Online Access: | http://www.ias.ac.in/jess/dec2012/1365.pdf http://hdl.handle.net/20.500.11937/12774 |