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...

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Bibliographic Details
Main Authors: Shah, A. A, Bell, T. H
Format: Article
Language:English
Published: 2014
Subjects:
Online Access:https://hdl.handle.net/10356/106125
http://hdl.handle.net/10220/23972
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Institution: Nanyang Technological University
Language: English