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Khotin, M. Yu., Sukhanov, M. K. (1984) THE GRANULITES AND ANORTHOSITES OF THE CONTACT ZONE OF THE GERAN MASSIF, STANOVOY RANGE (and the problem of the origin of massif-type anorthosites) International Geology Review, 26 (9) 1056-1070 doi:10.1080/00206818409466629

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Reference TypeJournal (article/letter/editorial)
TitleTHE GRANULITES AND ANORTHOSITES OF THE CONTACT ZONE OF THE GERAN MASSIF, STANOVOY RANGE (and the problem of the origin of massif-type anorthosites)
JournalInternational Geology Review
AuthorsKhotin, M. Yu.Author
Sukhanov, M. K.Author
Year1984 (September)Volume26
Issue9
PublisherInforma UK Limited
DOIdoi:10.1080/00206818409466629Search in ResearchGate
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Mindat Ref. ID305403Long-form Identifiermindat:1:5:305403:5
GUID0
Full ReferenceKhotin, M. Yu., Sukhanov, M. K. (1984) THE GRANULITES AND ANORTHOSITES OF THE CONTACT ZONE OF THE GERAN MASSIF, STANOVOY RANGE (and the problem of the origin of massif-type anorthosites) International Geology Review, 26 (9) 1056-1070 doi:10.1080/00206818409466629
Plain TextKhotin, M. Yu., Sukhanov, M. K. (1984) THE GRANULITES AND ANORTHOSITES OF THE CONTACT ZONE OF THE GERAN MASSIF, STANOVOY RANGE (and the problem of the origin of massif-type anorthosites) International Geology Review, 26 (9) 1056-1070 doi:10.1080/00206818409466629
In(1984, September) International Geology Review Vol. 26 (9) Informa UK Limited

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Sukhanov, M. K. (1988) ASSOCIATIONS OF MASSIF ANORTHOSITES. International Geology Review, 30 (8) 821-834 doi:10.1080/00206818809466063
Bédard, Jean H. (2009) Parental magmas of Grenville Province massif-type anorthosites, and conjectures about why massif anorthosites are restricted to the Proterozoic. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 100 (1). 77-103 doi:10.1017/s1755691009016016
Andreyev, V. P., Sukhanov, M. K. (1983) Anorthosites in the Sal'nyye Tundry (Lapland granulite belt in the Kola Peninsula) International Geology Review, 25 (5) 553-564 doi:10.1080/00206818309466736
Taylor, S. R., Campbell, I. H., McCulloch, M. T., McLennan, S. M. (1984) A lower crustal origin for massif-type anorthosites. Nature, 311 (5984). 372-374 doi:10.1038/311372a0
Vinogradov, V. I. (1986) STRONTIUM ISOTOPE RATIOS AND THE ORIGIN OF ANORTHOSITES. International Geology Review, 28 (1) 39-45 doi:10.1080/00206818609466248
(1993) Proterozoic Massif-Type Anorthosites. In Anorthosites. Springer Berlin Heidelberg. p.82-218. doi:10.1007/978-3-642-77440-9_3
Khotin, M. Yu., Popolitov, E. I., Stepanov, S. S. (1982) Plutonic inclusions in early Archean crystalline schists in the margin of the Dzhugdzhur anorthosite massif. International Geology Review, 24 (12) 1389-1404 doi:10.1080/00206818209467199
Simmons, E. Craig, Hanson, Gilbert N. (1978) Geochemistry and origin of massif-type anorthosites. Contributions to Mineralogy and Petrology, 66 (2) 119-135 doi:10.1007/bf00372151
Khodorevskaya, L. I. (2012). Granulite facies metamorphism and metasomatism in the gabbro-anorthosites of the Kolvitsa massif, Kola Peninsula. Geochemistry International, 50(3), 272-288.
Kumar, G R Ravindra (1986) The petrology and geochemistry of massif anorthosites and gabbros of the Bavali fault zone, North Kerala. Journal of Earth System Science, 95 (1). 117-130 doi:10.1007/bf03029176
DEMPSTER, T. J., PRESTON, R. J., BELL, B. R. (1999) The origin of Proterozoic massif-type anorthosites: evidence from interactions between crustal xenoliths and basaltic magma. Journal of the Geological Society, 156 (1) 41-46 doi:10.1144/gsjgs.156.1.0041
 
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