Deformation partitioning and porphyroblast rotation in meta-morphic rocks: a radical reinterpretation
Author:
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1525-1314.1985.tb00309.x/fullpdf
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2. T. T. Bell , 1985 , Foliation development and refraction in metamorphic rocks: reactivation of earlier foliations and decrenulation due to shifting patterns of deformation partitioning .J. metamorphic Geol. (submitted).
3. Development of P-T prograde and P-retrograde, T-prograde isogradic surfaces during blueschist to eclogite regional deformation/metamorphism in New Caledonia, as indicated by progressively developed porphyroblast microstructures
4. T.H. Bell, P.D. Fleming, and M.J. Rubenach , 1985 . Porphyroblast nucleation, growth and dissolution in regional metamorphic rocks as a function of deformation partitioning during foliation development .J. metamorphic Geol.(submitted).
5. Sequential porphyroblast growth and crenulation cleavage development during progressive deformation
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