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

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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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Bibliographic Details
Main Authors:	Shah, Afroz Ahmad, Bell, T. H.
Format:	Journal Article
Published:	Indian Academy of Sciences 2012
Subjects:	FIAs garnet monazite porphyroblast staurolite
Online Access:	http://www.ias.ac.in/jess/dec2012/1365.pdf http://hdl.handle.net/20.500.11937/12774

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