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 successi...
| Main Authors: | , |
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| Format: | Journal Article |
| Language: | English |
| Published: |
2014
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| Subjects: | |
| Online Access: | https://hdl.handle.net/10356/106125 http://hdl.handle.net/10220/23972 |