Thermo-rheological, shear heating model for leucogranite generation, metamorphism, and deformation during the ProterozoiTrans-Hudson orogeny, Black Hills, South Dakota

Tectonophysics

Volumn 342, Issue 3-4, 2001, Pages 371-388

  Nabelek, Peter I ^a   Liu, Mian ^a   Sirbescu, Mona Liza ^a  

^a UNIVERSITY OF MISSOURI   (United States)

Author keywords

Anatexis; Black Hills; Leucogranites; Metamorphism; Numerical modeling; Rheology; Shear heating

Indexed keywords

ANATEXIS; HEAT SOURCE; LEUCOGRANITE; METAMORPHISM; PROTEROZOIC; RHEOLOGY; SHEAR;

UNITED STATES;

EID: 0035693552     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0040-1951(01)00171-8     Document Type: Article

References (73)

1. Crustal structure and evolution of the Trans-Hudson orogen: Results from seismic reflection profiling
2. Lateral extrusion of lower crust from under high topography in the isostatic limit
3. The generation, segregation, ascent and emplacement of granite magma: The migmatite-to-crustally-derived granite connection in thickened orogens
4. Granite ascent and emplacement during contractional deformation in convergent orogens
5. Shear-zone systems and melts: Feedback relations and self-organization in orogenic belts
6. Friction of rocks
7. Heat-producing elements and the thermal and baric patterns of metamorphic belts
8. Step-leach Pb-Pb dating of inclusion-bearing garnet and staurolite, with implications for Early Proterozoic tectonism in the Black Hills collisional orogen, South Dakota, United States
9. When did the Wyoming Province collide with Laurentia?: New clues from step-leach Pb-Pb dating of garnet independent of its inclusions
10. New constraints on the timing of Early Proterozoic tectonism in the Black Hills (South Dakota), with implications for docking of the Wyoming province with Laurentia
11. Isotopic study of the Manaslu granite (Himalaya, Nepal): Inferences on the age and source of Himalayan leucogranites
12. Thermal modeling in low-pressure/high-temperature metamorphic belts
13. Proterozoic granite-pegmatite magmatism, Black Hills, South Dakota: Structure and geochemical zonation
14. The interpretation of inverted metamorphic isograds using simple physical calculations
15. Pressure-temperature-time paths of regional metamorphism I. Heat transfer during the evolution of regions of thickened crust
16. Material and thermal roles of basalt in crustal magmatism: Case study from Eastern Nevada
17. Geochemical constraints on the bimodal origin of High Himalayan leucogranites
18. Trace element modeling of pelite-derived granites
19. Decompression and anatexis of Himalayan metapelites
20. New insights into the origin of two contrasting Himalayan belts
21. A model for the origin of Himalayan anatexis and inverted metamorphism
22. Petrogenesis of Early Proterozoic pelitic schists of the Southern Black Hills, South Dakota: Constraints on regional low-pressure metamorphism
23. Heat generation associated with collision of two plates: The Himalayan geothermal belt
24. Subdivision of the Churchill province and extent of the Trans-Hudson orogen
25. Stability of andalusite and the aluminum silicate phase diagram
26. The role of melt in the uplift and exhumation of orogenic belts
27. 39Ar evidence for Middle Proterozoic (1300-1500 Ma) slow cooling of the Southern Black Hills, South Dakota, midcontinent, North America: Implications for Early Proterozoic P-T evolution and posttectonic magmatism
28. The thermal structure of collisional orogens as a response to accretion, erosion, and radiogenic heat production
29. Barrovian regional metamorphism: Where's the heat?
30. Rheology of the lithosphere: Selected topics
31. High closure temperatures of the U-Pb system in large apatites from the Tim Mountain pegmatite, Black Hills, South Dakota, USA
32. Evidence of heterogeneous crustal sources: The Harney Peak Granite, South Dakota, U.S.A
33. Lead isotopic evidence for mixed sources of Proterozoic granites and pegmatites, Black Hills, South Dakota, USA
34. Stress concentration in the upper lithosphere caused by underlying visco-elastic creep
35. Crustal temperature and heat production-implications of the linear heat-flow relation
36. Fluid-absent (dehydration) melting of biotite in metapelites in the early stages of crustal anatexis
37. Himalayas, the collided orogen. Present knowledge of the continental arc
38. Crustal generation of the Himalayan leucogranites
39. Crustal shortening and Eocene extension in the Southeastern Canadian Cordillera: Some thermal and rheological considerations
40. Role of plutonism in low-pressure metamorphic belt formation
41. Time-dependent effects of heat advection and topography on cooling histories during erosion
42. Chronology and styles of multiple deformation, plutonism, and polymetamorphism in the Merrimack Synclinorium of Western Maine
43. Petrologic and geochemical links between the post-collisional Proterozoic Harney Peak leucogranite, South Dakota, USA, and its source rocks
44. REE-depleted leucogranites, Black Hills, South Dakota: A consequence of disequilibrium melting of monazite-bearing schists
45. Petrogeneis of leucogranites in the Black Hills, South Dakota, as the consequence of shear heating during thrusting
46. Fluid inclusions in the Harney Peak Granite, Black Hills, South Dakota, USA: Implications for solubility and evolution of magmatic volatiles and crystallization of leucogranite magmas
47. The generation and crystallization conditions of the Proterozoic Harney Peak leucogranite, Black Hills, South Dakota, USA: Petrologic and geochemical constraints
48. Stable isotope evidence for the petrogenesis and fluid evolution in the Proterozoic Harney Peak leucogranite, Black Hills, South Dakota
49. Relations of zoned pegmatites to other pegmatites, granite, and metamorphic rocks in the Southern Black Hills, South Dakota
50. Experimental constraints on Himalayan anatexis
51. Thermal modeling of metamorphic pressure-temperature-time paths: A forward approach, in metamorphic pressure-temperature-time paths
52. The Phillips Pluton, Maine, USA: Evidence of heterogeneous crustal sources, and implications for granite ascent and emplacement mechanisms in convergent orogens
53. U-Th-Pb zircon and monazite ages and preliminary interpretation of the tectonic development of Precambrian rocks in the Black Hills
54. The steady state thermal structure of eroding orogenic belts and accretionary prisms
55. Pressure-temperature-time paths from two-dimensional thermal models: Prograde, retrograde, and inverted metamorphism
56. The role of tectonic grain size reduction in the rheological stratification of the lithosphere
57. Badrinath-Gangotri plutons (Garhwal, India): Petrological and geochemical evidence for fractionation processes in high Himalayan leucogranite
58. Rheology and deformation of an isotropic mica schist
59. Granite ascent in convergent orogenic belts: Testing a model
60. Metamorphic phase equilibria and pressure-temperature-time paths
61. A petrogenetic grid for pelitic schists in the system
62. The high temperature liquid and glass heat contents and heats of fusion of diopside, albite, sanidine, and nepheline
63. Heat generation of Cretaceous metamorphism in the Eastern Alps-A discussion
64. Pressure-temperature-time path related to the thermotectonic evolution of an Early Proterozoic metamorphic terrane, Black Hills, South Dakota
65. Melting of the continental crust: Some thermal and geological constraints on anatexis in continental collision zones and other tectonic settings
66. Modelling of temperatures in continental convergence zones
67. Nature of the crust in Maine, USA: Evidence from the Sebago batholith
68. Thermal controls on early-tertiary, short-lived, rapid regional metamorphism in the NW Himalaya, Pakistan
69. Timing of prograde metamorphism in the Zanskar Himalaya
70. Shear deformation along major transform faults and subduction slabs
71. Crustal magma generation and low-pressure high-temperature regional metamorphism in an extensional environment; possible application to the Lachlan Belt, Australia
72. Injection of Indian crust into Tibetan lower crust; a two-dimensional finite element model study
73. Shear heating and partial melting of granite: Thermal structure of overthrusted terrains in the Greater Himalaya