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Nielsen, Frank M., Wilson, J. Richard (1991) Crystallization processes in the Bjerkreim-Sokndal layered intrusion, south Norway: evidence from the boundary between two macrocyclic units. Contributions to Mineralogy and Petrology, 107 (3) 403-414 doi:10.1007/bf00325107

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Reference TypeJournal (article/letter/editorial)
TitleCrystallization processes in the Bjerkreim-Sokndal layered intrusion, south Norway: evidence from the boundary between two macrocyclic units
JournalContributions to Mineralogy and Petrology
AuthorsNielsen, Frank M.Author
Wilson, J. RichardAuthor
Year1991 (May)Volume107
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00325107Search in ResearchGate
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Mindat Ref. ID76634Long-form Identifiermindat:1:5:76634:0
GUID0
Full ReferenceNielsen, Frank M., Wilson, J. Richard (1991) Crystallization processes in the Bjerkreim-Sokndal layered intrusion, south Norway: evidence from the boundary between two macrocyclic units. Contributions to Mineralogy and Petrology, 107 (3) 403-414 doi:10.1007/bf00325107
Plain TextNielsen, Frank M., Wilson, J. Richard (1991) Crystallization processes in the Bjerkreim-Sokndal layered intrusion, south Norway: evidence from the boundary between two macrocyclic units. Contributions to Mineralogy and Petrology, 107 (3) 403-414 doi:10.1007/bf00325107
In(1991, May) Contributions to Mineralogy and Petrology Vol. 107 (3) Springer Science and Business Media LLC

See Also

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Jensen, J.C., Nielsen, F.M., Duchesne, J.C., Demaiffe, D., Wilson, J.R. (1993) Magma influx and mixing in the Bjerkreim-Sokndal layered intrusion, South Norway: evidence from the boundary between two megacyclic units at Storeknuten. Lithos, 29 (3) 311-325 doi:10.1016/0024-4937(93)90025-8
NIELSEN, FRANK M., CAMPBELL, IAN H., MCCULLOCH, MALCOLM, WILSON, J. RICHARD (1996) A Strontium Isotopic Investigation of the Bjerkreim—Sokndal Layered Instrusion, Southwest Norway. Journal of Petrology, 37 (1) 171-193 doi:10.1093/petrology/37.1.171
Wilson, J. Richard, Overgaard, Gitte (2005) Relationship between the Layered Series and the overlying evolved rocks in the Bjerkreim-Sokndal Intrusion, southern Norway. Lithos, 83 (3) 277-298 doi:10.1016/j.lithos.2005.03.006
Wilson, J.R., Robins, B., Nielsen, F.M., Duchesne, J.C., Vander Auwera, J. (1996) The Bjerkreim-Sokndal Layered Intrusion, Southwest Norway. In Developments in Petrology. Elsevier. p.231-255. doi:10.1016/s0167-2894(96)80009-1
Vander Auwera, Jacqueline, Longhi, John (1994) Experimental study of a jotunite (hypersthene monzodiorite): constraints on the parent magma composition and crystallization conditions (P, T, f O 2) of the Bjerkreim-Sokndal layered intrusion (Norway) Contributions to Mineralogy and Petrology, 118 (1) 60-78 doi:10.1007/bf00310611
Barling, J, Weis, D, Demaiffe, D (2000) A Sr-, Nd- and Pb-isotopic investigation of the transition between two megacyclic units of the Bjerkreim–Sokndal layered intrusion, south Norway. Chemical Geology, 165 (1) 47-65 doi:10.1016/s0009-2541(99)00163-1
Resources of apatite, ilmenite and magnetite in the Bjerkreim Sokndal Layered Intrusion, Rogaland, South Norway. Norges geologiske undersøkelse, NGU-report:.2001.092. 33 pages
Paludan, Johanne (1995): Structural evolution of the Bjerkreim-Sokndal layered intrusion, SW Norway: micro to macro scale studies. Thesis
Wilmart, Edith, Clocchiatti, Robert, Duchesne, Jean-Clair, Touret, Jacques L. R. (1991) Fluid inclusions in charnockites from the Bjerkreim-Sokndal massif (Rogaland, southwestern Norway): fluid origin and in situ evolution. Contributions to Mineralogy and Petrology, 108 (4) 453-462 doi:10.1007/bf00303449
Robins, B (1997) The Bjerkreim-Sokndal Layered Intrusion, Rogaland, SW Norway: Evidence from marginal rocks for a jotunite parent magma. Lithos, 39 (3) 121-133 doi:10.1016/s0024-4937(96)00021-7
Duchesne, J.-C., Wilmart, E. (1997) Igneous Charnockites and Related Rocks from the Bjerkreim-Sokndal Layered Intrusion (Southwest Norway): a Jotunite (Hypersthene Monzodiorite)-Derived A-type Granitoid Suite. Journal of Petrology, 38 (3) 337-369 doi:10.1093/petroj/38.3.337
 
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