| Carswell, D. A., Brueckner, H. K., Cuthbert, S. J., Mehta, K., O'Brien, P. J. (2003) The timing of stabilisation and the exhumation rate for ultra-high pressure rocks in the Western Gneiss Region of Norway. Journal of Metamorphic Geology, 21 (6) 601-612 doi:10.1046/j.1525-1314.2003.00467.x | Journal (article/letter/editorial) | pressure rocks in the Western Gneiss Region of Norway D. A. CARSWELL,1 H. K. BRUECKNER,2,3 S. J. CUTHBERT...(UHP) eclogites within the Western Gneiss Region of Norway probably occurred within the 400–410 Ma time frame...pressure (UHP); Norway. INTRODUCTION The Western Gneiss Region (WGR) of western Norway comprises a large...GU GU GU GU GU Saltaneset Vetrhus Måløy efjord jord GU Selje Mold Storf Hareidlandet Ulsteinvik...of formation of UHP eclogites within the WGR of Norway. These ages are then utilised in conjunction with | | Carswell, D. A, Krabbendam, M., Cuthbert, S. J., Eide, E. A, Brueckner, H. K., Medaris Jr, L. G (2003) Guidebook to the Field Excursions in the Nordfjord-Stadlandet-Almklovdalen Area. Norges Geologiske Undersøkelse. Rapport 2003.056. Norges Geologiske Undersøkelse (NGU) | Report (issue) | Geological Survey of Norway N-7441 Trondheim, Norway Tel.: 47 73 90 40 00 Telefax 47 73 92 16 20 REPORT...the Alice Wain Memorial West Norway Eclogite Field Symposium held in Selje from June 21st-28th, 2003. Eskola...peridotites that outcrop in the coastal region of west Norway between Bergen and Trondheim. These occurrences...MEMORIAL WEST NORWAY ECLOGITE FIELD SYMPOSIUM JUNE 21st – 28th, 2003 in SELJE, WEST NORWAY GUIDEBOOK TO...Pressure Eclogites in the Western Gneiss Region of Norway. Chapter 2: Excursion to the UHP Eclogites at | | | Journal (article/letter/editorial) | of Geology, UniÕersity of Tromsø, Tromsø 9000, Norway d Department of Earth Sciences, UniÕersity of Oxford...province’’ in the Stadlandet area of coastal SW Norway ŽFig. 1.. Subsequently, Wain Ž1997a; b. expanded...approximately 5 = 10 4 km2 along the coast of southwest Norway between Bergen and Trondheim ŽFig. 1.. The WGR...enclosed within schists or gneisses. are quartz, rutile, zoisiterclinozoisite, phengite, paragonite, kyanite...zone as a SW–NE-trending strip to the east of Nordpollen which swings westward across Sørpollen. Based | | | Book (edition) | substitutes somewhat for Ti, residual titanates (such as rutile) may cause depletions of Nb in subduction-zone...orthopyroxene, high-Al/Cr spinel, magnetite, ilmenite, rutile, zircon, plagioclase (in low-P inclusions), carbonate...orthopyroxene, highAl/Cr spinel, magnetite, ilmenite, rutile, zircon, amphibole, phlogopite, and plagioclase...these inclusions are Ti-rich kaersutite, diopside, rutile, ilmenite, and magnesite. Schiano et al. (1994)...which those elements are highly compatible, such as rutile. These HFSEs may also be sequestered in residual |
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