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WILLIGERS, B. J. A., KROGSTAD, E. J., WIJBRANS, J. R. (2001) Comparison of Thermochronometers in a Slowly Cooled Granulite Terrain: Nagssugtoqidian Orogen, West Greenland. Journal of Petrology, 42 (9) 1729-1749 doi:10.1093/petrology/42.9.1729

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Reference TypeJournal (article/letter/editorial)
TitleComparison of Thermochronometers in a Slowly Cooled Granulite Terrain: Nagssugtoqidian Orogen, West Greenland
JournalJournal of Petrology
AuthorsWILLIGERS, B. J. A.Author
KROGSTAD, E. J.Author
WIJBRANS, J. R.Author
Year2001 (September)Volume42
Page(s)1729-1749Issue9
PublisherOxford University Press (OUP)
DOIdoi:10.1093/petrology/42.9.1729Search in ResearchGate
Mindat Ref. ID178427Long-form Identifiermindat:1:5:178427:9
GUID6d778949-6d97-41b0-aa2a-790630515574
Full ReferenceWILLIGERS, B. J. A., KROGSTAD, E. J., WIJBRANS, J. R. (2001) Comparison of Thermochronometers in a Slowly Cooled Granulite Terrain: Nagssugtoqidian Orogen, West Greenland. Journal of Petrology, 42 (9) 1729-1749 doi:10.1093/petrology/42.9.1729
Plain TextWILLIGERS, B. J. A., KROGSTAD, E. J., WIJBRANS, J. R. (2001) Comparison of Thermochronometers in a Slowly Cooled Granulite Terrain: Nagssugtoqidian Orogen, West Greenland. Journal of Petrology, 42 (9) 1729-1749 doi:10.1093/petrology/42.9.1729
In(2001, September) Journal of Petrology Vol. 42 (9) Oxford University Press (OUP)

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

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Mengel, F. C. (1983). Chemistry of coexisting mafic minerals in granulite facies amphibolites from West Greenland: clues to conditions of metamorphism. Neues Jahrbuch für Mineralogie, Abhandlungen147, 315–340.
Milodowski, A. E. & Hurst, A. (1989). The authigenesis of phosphate minerals in some Norwegian hydrocarbon reservoirs; evidence for the mobility and redistribution of rare earth elements (REE) and Th during sandstone diagenesis. Proceedings, International Symposium on Water–Rock Interaction6, 491–494. Edmonton, AB, International: International Association of Geochemistry and Cosmochemistry and Alberta Research Council, Sub- Group on Water–Rock Interaction,pp.
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Purdy, J. W. & Jäger, E. (1976). K–Ar ages on rocks forming minerals from the central Alps. Memorie degli Istituti di Geologia e Mineralogia dell’Universita di Padova30, 1–321.
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Van Gool, J. A. M., Manatschal, G. & Stünitz, H. (1997). Big shear zones—weak fabrics, little shear zones—strong fabrics: an evaluation of mid- to deep crustal shear zones in the Nagssugtoqidian orogen of West Greenland. International Meeting on Deformation Mechanisms in Nature and Experiment, Basel, March, 1997.
Van Gool, J. A. M., Connelly, J. N., Mengel, F. C. & Scott, D. J. (1998). The Nagssugtoqidian Orogen, West Greenland: tectonic development and regional correlations. In: ESCOOT Report of Transect Meeting, 4–5 May 1998, Merrickville, Ont. Lithoprobe Report68, 1.
Wagner, G. A., Reimer, G. M. & Jäger, E. (1977). Cooling ages derived by apatite fission track, mica Rb–Sr and K–Ar dating: the uplift and cooling history of the central Alps. Memorie degli Istituti di Geologia e Mineralogia dell’Universita di Padova30, 1–28.
Wijbrans, J. R., Pringle, M. S., Koppers, A. A. P. & Scheveers, R. (1995). Argon geochronology of small samples using the Vulkaan argon laserprobe. Proclamaties van de Koninklijke Nederlandse Academie van Wetenschappen98, 185–218.
Willigers, B. J. A. (1999). The orogenic and post-orogenic thermal evolution of the Paleoproterozoic Nagssugtoqidian orogen, West Greenland, assessed by 40Ar/39Ar and U–Pb geochronology. Ph.D. thesis, University of Copenhagen, 110 pp.


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