17 results on '"Bell, T. A."'
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2. Distinguishing and correlating multiple phases of metamorphism across a multiply deformed region using the axes of spiral, staircase and sigmoidal inclusion trails in garnet
3. Spiral and staircase inclusion trail axes within garnet and staurolite porphyroblasts from schists of the Bolton Syncline, Connecticut: timing of porphyroblast growth and the effects of fold development
4. How useful are 'millipede' and other similar porphyroblast microstructures for determining synmetamorphic deformation histories?
5. Episodic gravitational collapse and migration of the mountain chain during orogenic roll-on in the Himalayas
6. The inter-relationships between long-lived metamorphism, pluton emplacement and changes in the direction of bulk shortening during orogenesis
7. The development of spiral‐shaped inclusion trails during multiple metamorphism and folding
8. Porphyroblast inclusion-trail orientation data: eppure non son girate!
9. Shear sense.
10. Episodic metamorphic reactions during orogenesis: the control of deformation partitioning on reaction sites and reaction duration
11. Dissolution, solution transfer, diffusion versus fluid flow and volume loss during deformation/metamorphism.
12. Porphyroblast inclusion trails: the key to orogenesis.
13. The role of deformation partitioning in the deformation and recrystallization of plagioclase and K-feldspar in the Woodroffe Thrust mylonite zone, central Australia.
14. Foliation development and refraction in metamorphic rocks: reactivation of earlier foliations and decrenulation due to shifting patterns of deformation partitioning.
15. Porphyroblast nucleation, growth and dissolution in regional metamorphic rocks as a function of deformation partitioning during foliation development.
16. Deformation partitioning and porphyroblast rotation in meta-morphic rocks: a radical reinterpretation.
17. 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.
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