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Van Roermund, H.L.M et al. (2000): Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultradeep (>6GPa) origin. Journal of Metamorphic Geology 18: 135-147

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Year2000
Original EntryVan Roermund, H.L.M et al. (2000): Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultradeep (>6GPa) origin. Journal of Metamorphic Geology 18: 135-147
Mindat Ref. ID16021388Long-form Identifiermindat:1:5:16021388:7
GUID0
Full ReferenceVan Roermund, H.L.M et al. (2000): Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultradeep (>6GPa) origin. Journal of Metamorphic Geology 18: 135-147
Plain TextVan Roermund, H.L.M et al. (2000): Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultradeep (>6GPa) origin. Journal of Metamorphic Geology 18: 135-147

Map of Localities

Mineral Occurrences

LocalityMineral(s)
Uglvik peridotite body, Uglvik, Otrøya, Midsund, Molde, Møre og Romsdal, Norwayⓘ Clinopyroxene Subgroup, ⓘ Rutile

See Also

These are possibly similar items as determined by title/reference text matching only.

Van Roermund, H.L.M., Drury, M.R., Barnhoorn, A. and De Ronde, A. A. (2000): Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultradeep (>6GPa) origin. Journal of Metamorphic Geology 18: 135-147
Van Roermund, , Drury, , Barnhoorn, , De Ronde, (2000) Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultra-deep (>6 GPa) origin. Journal of Metamorphic Geology, 18 (2) 135-147 doi:10.1046/j.1525-1314.2000.00251.x
Van Roermund, H. L. M., Drury, M. R., Barnhoorn, A., De Ronde, A. (2000) Non-silicate inclusions in garnet from an ultra-deep orogenic peridotite. Geological Journal, 35 (3) 209-229 doi:10.1002/gj.858
Brueckner, H.K., Carswell, D.A., Griffin, W.L., Medaris, L.G., Van Roermund, H.L.M., Cuthbert, S.J. (2010) The mantle and crustal evolution of two garnet peridotite suites from the Western Gneiss Region, Norwegian Caledonides: An isotopic investigation. Lithos, 117 (1) 1-19 doi:10.1016/j.lithos.2010.01.011
Spengler, Dirk, van Roermund, Herman L.M., Scheffler, Franziska (2019) Pyroxene exsolution microstructures in garnet from the Almklovdalen peridotite, SW Norway. Lithos, 350. 105217 doi:10.1016/j.lithos.2019.105217
VAN ROERMUND, H. L. M. (2001) Relict Majoritic Garnet Microstructures from Ultra-Deep Orogenic Peridotites in Western Norway. Journal of Petrology, 42 (1) 117-130 doi:10.1093/petrology/42.1.117
ZHANG, Cong, Van ROERMUND, Herman (2015) Orogenic Garnet Peridotite - Tools to Reconstruct Paleo-geodynamic Settings of Continental Collision Zones. Acta Geologica Sinica - English Edition, 89. 110 doi:10.1111/1755-6724.12308_66
Song, S. (2005) Sodic amphibole exsolutions in garnet from garnet-peridotite, North Qaidam UHPM belt, NW China: Implications for ultradeep-origin and hydroxyl defects in mantle garnets. American Mineralogist, 90 (5) 814-820 doi:10.2138/am.2005.1684
Gilio, Mattia, Clos, Frediano, van Roermund, Herman L.M. (2015) The Friningen Garnet Peridotite (central Swedish Caledonides) A good example of the characteristic PTt path of a cold mantle wedge garnet peridotite. Lithos, 230. 1-16 doi:10.1016/j.lithos.2015.05.003
Krogh Ravna, (2000) The garnet-clinopyroxene Fe2+-Mg geothermometer: an updated calibration. Journal of Metamorphic Geology, 18 (2) 211-219 doi:10.1046/j.1525-1314.2000.00247.x
Schmädicke, Esther, Gose, Jürgen (2019) Low water contents in garnet of orogenic peridotite: clues for an abyssal or mantle-wedge origin?. European Journal of Mineralogy, 31 (4) 715-730 doi:10.1127/ejm/2019/0031-2880
 
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