Deformation of partially molten granite: A review and comparison of experimental and natural case studies

International Journal of Earth Sciences

Volumn 90, Issue 1, 2001, Pages 60-76

  Rosenberg, C L ^a  

^a Fachrichtung Allgemeine Geologie   (Germany)

Author keywords

Experimental deformation; Granite; Magmatic microstructure; Melt; Melt topology; Synmagmatic deformation

Indexed keywords

DEFORMATION MECHANISM; GRANITE; MAGMATISM; MELT; OROGENIC BELT; RHEOLOGY;

EID: 0034939587     PISSN: 14373254     EISSN: None     Source Type: Journal    
DOI: 10.1007/s005310000164     Document Type: Article

References (96)

1. Shape fabrics of particles in low concentration suspensions: 2D analogue experiments and application to tiling in magma
2. Critical phenomena in the rheology of partially melted rocks
3. Introduction
4. Steady state creep of fine grain granite aggregate at partial melting
5. Granite rheology: Magma flow and melt migration
6. Experimental investigation of the rheology of partially molten peridotite at upper mantle pressures and temperatures
7. Rheological transitions and the progress of melting of crustal rocks
8. Structures and melt fractions as indicators of reheology in cordierite-bearing migmatites of the Bayerische Wald (Variscan Belt, Germany)
9. Shear criteria in granite and migmatite deformed in the magmatic and solid states
10. Submagmatic fractures in granites
11. A test of the low of effective stress for crystalline rocks of low porosity
12. The role of deformation in the movement of granitic melt: Views from the laboratory and the field
13. Topology of syntectonic melt flow networks in the deep crust: Inferences from three-dimensional images of leucosome geometry in migmatites
14. Crustal anatexis and melt extraction during deformation in the restitic xenoliths at El Joyazo (SE Spain)
15. Granitic melt viscosity and silicic magma dynamics in contrasting tectonic settings
16. Solution-precipitation enhanced diffusional creep of partially molten olivine-basalt aggregates during hot-pressing
17. Flow and fabric development during the diapiric rise of magma
18. Influence of deformation on melt topology in peridotites
19. Role of melt in the formation of a deep-crustal compressive shear zone: The MacLaren Glacier metamorphic belt, South Central Alaska
20. Synmagmatic folding of the base of the Bergell pluton: Evidence from the Western contact
21. Experimental deformation of partially melted granitic aggregates
22. Transition from dislocation creep to melt-enhanced diffusion creep in fine-grained granitic aggregates
23. High-temperature creep of partially molten plagioclase aggregates
24. Relative rheological evolution of chemically contrasted coeval magmas: Example of the Tichka plutonic complex (Morocco)
25. 3D biotite shape fabric experiments under simple shear strain
26. Theoretical and experimental study of fabrics developed by different shaped markers in two dimensional simple shear
27. Fracture-mechanism maps for materials which cleave: F.C.C., B.C.C. and H.C.P. metals and ceramics
28. Quartz fabric transition in a cooling syntectonic granite (Hermitage, France)
29. Experimental investigation of melt topology in partially melted quartzo-feldspathic aggregates under hydrostatic and non-hydrostatic stress
30. The exhumation of cross sections of the continental crust: Structure, kinematics and rheology
31. Deformation of incompletely crystallized magma systems: Granitic gneisses and their tectonic implications
32. Fracturing and diking in incompletely crystallized granitic plutons
33. Experimental constraints on the dynamics of the partially molten upper mantle: Deformation in the diffusion creep regime
34. Experimental constraints on the dynamics of the partially molten upper mantle 2. Deformation in the dislocation creep regime
35. Melt enhanced deformation: A major tectonic process
36. 2O infiltration in the aureole of the Ballachulish Igneous Complex
37. Water contents of felsic melts: Application to the rheological properties of granitic magmas
38. Granite emplacement mechanisms and tectonic controls: Inferences from deformation studies
39. Rigid particles in simple shear flow: Is their preferred orientation periodic or steady-state?
40. Melt topology in partially molten mantle peridotite during ductile deformation
41. The rheological properties of suspensions of rigid particles
42. Melt topology and seismic anisotropy in mantle peridotites of the Oman ophiolite
43. Rheology of partially molten mantle rocks
44. Flow differentiation in igneous dikes and sills; profiles of velocity and phenocryst concentration
45. Modelling the seismic properties of fast-spreading ridge crustal Low-Velocity Zones: Insights from Oman Gabbro textures
46. Wetting angles, equilibrium melt geometry, and the permeability threshold of partially molten crustal protholiths
47. Rheology of crystal-bearing silicate melts: An experimental study at high viscosities
48. On the crystallinity, probability of occurence, and rheology of lava and magma
49. Synkinematic microscopy of transparent polycrystals
50. Deformation of partially-molten synthetic granite: Laboratory evidence for granular flow
51. Initial melting at grain boundaries of quartz and feldspar in gneisses and granulites
52. Which deformation mechanisms control the flow of granitoid rocks at low (<30%) melt fractions?
53. Some new rheological experiments on igneous rocks at temperatures up to 1,120°C
54. The effect of temperature on the strength at high confining pressure of granodiorite containing free and chemically-bound water
55. Partially molten middle crust beneath southern Tibet: Synthesis of project INDEPTH results
56. Kinematics in magmatic rocks with special reference to gabbros
57. Flow mechanism and viscosity in basaltic magma chambers
58. Experimental deformation of partially melted granitic rocks at 600-900°C and 250 MPa confining pressure
59. Effect of partial melting on rock deformation: Experimental and natural evidences on rocks of granitic compositions
60. Direct observation of deformation processes in crystal mushes
61. Crystal rotation and growth during grain flow in a deforming crystal mush
62. A theory for granular flow accommodated by material transfer via an intergranular fluid
63. A granular flow theory for the deformation of partially melted rock
64. Rates of processes in magmatic arcs: Implications for the timing and nature of pluton emplacement and wall rock deformation
65. A review of criteria for the identification of magmatic and tectonic foliations in granitoids
66. Interpreting magmatic fabric patterns in plutons
67. On the rheological critical melt fraction
68. The viscosity of suspensions of rigid spheres
69. Syntectonic melt pathways in granite, and melt-induced transition in deformation mechanisms
70. Syntectonic melt pathways during simple shearing of a partially-molten rock analogue (norcamphor-benzamide)
71. Partial melt topology in statically and dynamically recrystallized granite
72. Mechanisms and orientation of melt segregation paths during pure shearing of a partially molten rock analogue (norcamphor-benzamide)
73. Melt segregation in the lower crust: How have experiments helped us?
74. The influence of deformation on the extraction of crustal melts: A consideration of the role of melt-assisted granular flow
75. Experimental deformation of partially molten Westerly granite under fluid-absent conditions, with implications for the extraction of granitic magmas
76. Criteria for the recognition of partial melting
77. Melt segregation in the continental crust: Distribution and geometry of melt in anatectic rocks
78. Rheological properties of granitic magmas in their crystallization range
79. Phase equilibrium constraints on the viscosity of silicic magmas. 1. Volcanic-plutonic comparison
80. An illustration of the advantages of a complete texture analysis described by the orientation distribution function (ODF) using quartz pole figure data
81. The geometry of the Central Andean backarc crust: Joint interpretation of cross-section balancing and seismic refraction data
82. Shear thickening dilatancy in crystal-rich flows
83. Strain and fabric analyses based on porphyroclast interaction
84. Significance of a hiatus in downtemperature fabric development within syn-tectonic quartz diorite complexes, Channel Islands, UK
85. Water assisted dynamic recrystallization and weakening in polycrystalline bischofite
86. Dynamic recrystallization of minerals
87. Experimental deformation of partially-melted granite
88. Termination of a continental-scale strike-slip fault in partially melted crust: The west Pernambuco shear zone, northeast Brazil
89. Review of microstructural evidence of magmatic and solid-state flow
90. Rheological transitions during partial melting and crystallization with application to felsic magma segregation and transfer
91. Reply to the comment by Kerr RC and Lister JR on "On the relationship between dike width and magma viscosity
92. The segregation and emplacement of granitic magmas
93. Three S-type volcanic suites from the Lachlan fold belt, Southeast Australia
94. Melt distribution in mantle rocks deformed in shear