Shear zone vs folding origin for spiral inclusion trails in the Canton Schist

Journal of Structural Geology

Volumn 23, Issue 12, 2001, Pages 1845-1864

  Stallard, Aaron ^a,b   Hickey, Ken ^a  

^a JAMES COOK UNIVERSITY   (Australia)

^b SHIZUOKA UNIVERSITY   (Japan)

Author keywords

Folding; Foliations; Porphyroblast rotation; Shear zones; Spiral inclusion trails

Indexed keywords

TRAILS;

BELTS; GARNETS; INCLUSIONS;

GEOLOGY;

INCLUSION; OVERPRINTING; PORPHYROBLAST; SCHIST;

EID: 0035545885     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0191-8141(01)00031-1     Document Type: Article

References (62)

1. Stratigraphy of the area around the Austell-Frolona Antiform, West-Central Georgia
2. Porphyroblast non-rotation during crustal extension in the Variscan Lys-Caillaouas Massif. Pyrenees
3. Interpretation of porphyroblast inclusion trails: Limitations imposed by growth kinetics and strain rates
4. Geology of the Tate Quadrangle, Georgia
5. Foliation development: The contribution, geometry and significance of progressive bulk inhomogeneous shortening
6. Deformation partitioning and porphyroblast rotation in metamorphic rocks: A radical reinterpretation
7. Sequential porphyroblast growth and crenulation cleavage development during progressive deformation
8. Porphyroblast inclusion trails: The key to orogenesis
9. Distribution of pre-folding linear movement indicators around the Spring Hill Synform, Vermont: Significance for mechanism of folding in this portion of the Appalachians
10. Porphyroblast nucleation, growth and dissolution in regional metamorphic rocks as a function of deformation partitioning during foliation development
11. Porphyroblast inclusion-trail orientation data: Eppure non son girate!
12. Do smoothly curving, spiral-shaped inclusion trails signify porphyroblast rotation
13. Distinguishing and correlating multiple phases of metamorphism across a multiply deformed region using the axes of spiral, staircase and sigmoidally curved inclusion trails in garnet
14. Rotated staurolite porphyroblasts in the Littleton Schist at Bolton, Connecticut, USA
15. 39Ar incremental-release ages of horneblende and biotite across the Georgia inner Piedmont: Their bearing on late paleozoic-early Mesozoic tectonothermal history
16. Regional slaty cleavage formation and fold axis rotation by reuse and
17. Rotations of elongate rigid particles in slow non-newtonian flows
18. Fold fabrics and emplacement of an Archean granitoid pluton. Cleft lake,
19. The geology of the northeastern portion of the Dahlonega Gold Belt
20. The geology of gold occurrences in the West-Central Georgia Piedmont
21. Reorientation of inclusions by a combination of pure shear and simple
22. The three-dimensional geometry of simulated porphyroblast inclusion
23. Shear-sense indicators: A Review
24. Microstructural analysis of the classic snowball garnets of southeast
25. Syn-deformational grain growth: Matrix coarsening during foliation
26. Behaviour of rigid objects during deformation and metamorphism: A test
27. Resolving complexities associated with timing macroscopic folds in
28. A brief excursion between two thrust stacks that comprise most of the
29. Porphyroblast inclusion trail geometries in the grand Canyon: Evidence
30. Flow variation in layered rocks subjected to bulk flow of various
31. Lack of porphyroblast rotation in the Otago Schists, New Zealand:
32. Sequential porphyroblast growth during progressive deformation and low-P
33. Unravelling the spirals: A serial thin-section study and
34. Testing models for the development of spiral-shaped inclusion trails in
35. Porphyroblast microstructures: A review of current and future trends
36. Near-orthogonal foliation development in orogens: Meaningless complexity,
37. Progressive metamorphism in a crustal-scale shear zone: An example from
38. Non-rotation of garnet porphyroblasts and 3-D inclusion trail data: An
39. The partitioning of deformation in flowing rock masses
40. Syntectonic growth of porphyroblasts over crenulation cleavages-an
41. Are crenulation cleavage zones mylonites on the microscale?
42. Development of snowball structure: Numerical simulation of inclusion
43. Geology of the Greater Atlanta region
44. Reversed structures and bounce structures: Are they recognizable? Are
45. The kinematic interpretation of obliquely transected porphyroblasts: An
46. Porphyroblast rotation: Eppur si muove?
47. On the geometry of S-shaped inclusion trails in garnet porphyroblasts
48. Relationships between garnet shape, rotational inclusion fabrics and
49. The geometry and mechanics of formation of 'similar' type folds
50. The techniques of modern structural geology
51. Garnet rotations due to the major Paleozoic deformations in Southeast
52. Rotated garnets in metamorphic rocks
53. Bewegungspuren in porphyroblasten kristalliner schiefer
54. Strain and kinematic analysis in general shear zones
55. Fold mechanisms in the Canton Schist: Constraints on the contribution of
56. Experimental investigation of the effects of fluid heterogeneity upon the
57. The rotation of garnet porphyroblasts around a single fold. Lukmanier
58. Garnet rotation and the development of axial plane crenulation cleavage
59. Rotating garnets
60. On the determination of polymetamorphic mineral associations and its