Emplacement of deep upper-mantle rocks into cratonic lithosphere by convection and diapiric upwelling

Journal of Petrology

Volumn 42, Issue 1, 2001, Pages 131-140

  Drury, M R ^a   Van Roermund, H L M ^a   Carswell, D A ^b   De Smet, J H ^a   Van Den Berg, A P ^a   Vlaar, N J ^a  

^a UTRECHT UNIVERSITY   (Netherlands)

^b UNIVERSITY OF SHEFFIELD   (United Kingdom)

Author keywords

Asthenosphere diapris; Cratonic lithosphere; Deep upper mantle; Majoritic garnet

Indexed keywords

CONVECTION; CRATON; DIAPIRISM; EMPLACEMENT; UPPER MANTLE;

NORWAY; OTROY; WESTERN GNEISS REGION;

EID: 0035112626     PISSN: 00223530     EISSN: None     Source Type: Journal    
DOI: 10.1093/petrology/42.1.131     Document Type: Article

References (65)

1. Implications of a two-component marble-cake mantle
2. Depleted spinel harzburgite xenoliths in Tertiary dykes from East Greenland: Restite from high degree melting
3. Mantle peridotites from continental rifts to ocean basins to subduction zones
4. Compositional distinction between oceanic and cratonic lithosphere
5. Composition and structure of the Kaapvaal lithosphere
6. Evidence for a 150-200 km thick Archaean lithosphere from diamond inclusion barometry
7. Clinoenstatite in Alpe Arami peridotite: Additional evidence of very high pressure
8. A tale of two orogens: The contrasting T-P-t history and geochemical evolution of mantle in high and ultra-high pressure metamorphic terranes of the Norwegian Caledonides and the Czech Variscides
9. Experimental evidence for the exsolution of cratonic peridotite from high temperature harzburgite
10. Possible primary upper mantle peridotite in Norwegian basal gneiss
11. Garnet pyroxenite lens within Ugelvik layered garnet peridotite
12. The metamorphic evolution of Mg-Cr type Norwegian garnet peridotites
13. Textural studies of garnet lherzolites: Evidence of exsolution origin from high temperature harzburgites
14. Stability and growth of continental shields in mantle convection models including recurrent melt production
15. Evolution of continental roots in numerical thermo-chemical mantle convection models including differentiation by partial melting
16. Early formation and long-term stability of continents resulting from decompression melting in a convecting mantle
17. Alpe Arami: A peridotite massif from depths of more than 300 km
18. Trace-element zoning in garnets from sheared xenoliths
19. Secular variation in the composition of subcontinental lithospheric mantle: Geophysical and geodynamic implications
20. Superkimberlites: A geodynamic diamond window to the Earth's core
21. Ultradeep (greater than 300 km) ultramafic upper mantle xenoliths
22. Evolution of clinopyroxene and garnet in an eclogite nodule from the Roberts Victor kimberlite pipe
23. Lower mantle mineral associations in diamonds from Sao Luiz
24. Lithospheric peridotites of the Kaapvaal craton
25. Phase equilibria of common rocks in the crust and mantle
26. Phase equilibrium constraints on the origin of basalts, picrites, and komatiites
27. Evidence for Archean ocean crust with low high field strength elements signature from diamondiferous eclogite xenoliths
28. Anorthositic oceanic crust in the Archean Earth
29. Chronology of the high-pressure metamorphism of Norwegian garnet peridotites/ pyroxenites
30. Mineralogies, densities, and seismic velocities of garnet lherzolites and their geophysical implications
31. Silica enrichment in the continental upper mantle via melt/rock reaction
32. Homogenisation of the mantle by convective mixing and diffusion
33. 3, between magnesian silicate perovskite and magnesiowustite: Implications for the origin of inclusions in diamond and the composition of the lower mantle
34. Le massif ultrabasique des Beni Bouchera (Rif Interne, Maroc): Etude des peridotites de haute temperature et de haute pression, et des pyroxenolites, a grenat ou sans grenat
35. HP and UHP eclogites and garnet peridotites in the Scandinavian Caledonides
36. Two Roberts Victor cumulate eclogites and their re-equilibration
37. Ultradeep xenoliths from African kimberlites: Sr and Nd isotopic compositions suggest complex history
38. Composition and thermal evolution of cratonic mantle beneath the central Archean Slave Province
39. Mineralogy and composition of the upper mantle
40. A geothermobarometric investigation of garnet peridotites in the Western Gneiss Region of Norway
41. Metasomatic and enrichment processes in lithospheric peridotites, an effect of asthenosphere-lithosphere interaction
42. Archean, Protcrozoic, and Phanerozoic lithosphere
43. Pyroxene solid solution in garnets included in diamonds
44. Ultrahigh pressure garnet inclusions in Monastery diamonds: Trace element abundance patterns and conditions of origin
45. Structure and petrology of peridotites: Clues to their geodynamic environment
46. Petrogenesis of the granular and sheared ultrabasic nodule suite in kimberlites
47. Is there an Icelandic mantle plume?
48. The age of continental roots
49. Graphitized diamonds from a peridotite massif in Morocco and implications for anomalous diamond occurrences
50. The high pressure ultramafic-mafic-carbonate suite of Cima Lunga-Adula
51. Origin of diamonds in old enriched mantle
52. Constitution and evolution of the mantle
53. Origin of kimberlites and related magmas
54. Cooling kinetics of garnet websterites from the Freychinede orogenic lherzolite massif
55. Ultradeep (>300 kilometres) ultramafic xenoliths: Petrological evidence from the transition zone
56. Nature of the mantle roots beneath the North American craton: Mantle xenolith evidence from Somerset Island kimberlites
57. Kimberlites near Ororroo, South Australia
58. Compositional heterogencities in minerals of sheared xenolith inclusions from African kimberlites
59. Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle
60. Speculations on the Archean mantle: Missing link between komatiite and depleted garnet peridotite
61. Evidence for a Proterozoic mantle plume and a thermotectonic model for exhumation of garnet peridotites
62. Ultra-high pressure (P >6 GPa) garnet peridotites in Western Norway: Exhurnation of mantle rocks from more than 185 km
63. Super-silicic garnet microstructures from an orogenic peridotite, evidence for an ultra-deep origin
64. Relict majoritic garnet microstructures from ultra-deep orogenic peridotites in Western Norway
65. Melting of garnet peridotite and the origin of komatiite and depleted lithosphere