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Florence, F. P., Darling, R. S., Orrell, S. E. (1995) Moderate pressure metamorphism and anatexis due to anorthosite intrusion, western Adirondack Highlands, New York. Contributions to Mineralogy and Petrology, 121 (4) 424-436 doi:10.1007/s004100050107

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Reference TypeJournal (article/letter/editorial)
TitleModerate pressure metamorphism and anatexis due to anorthosite intrusion, western Adirondack Highlands, New York
JournalContributions to Mineralogy and Petrology
AuthorsFlorence, F. P.Author
Darling, R. S.Author
Orrell, S. E.Author
Year1995 (October 17)Volume121
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050107Search in ResearchGate
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Mindat Ref. ID77310Long-form Identifiermindat:1:5:77310:0
GUID0
Full ReferenceFlorence, F. P., Darling, R. S., Orrell, S. E. (1995) Moderate pressure metamorphism and anatexis due to anorthosite intrusion, western Adirondack Highlands, New York. Contributions to Mineralogy and Petrology, 121 (4) 424-436 doi:10.1007/s004100050107
Plain TextFlorence, F. P., Darling, R. S., Orrell, S. E. (1995) Moderate pressure metamorphism and anatexis due to anorthosite intrusion, western Adirondack Highlands, New York. Contributions to Mineralogy and Petrology, 121 (4) 424-436 doi:10.1007/s004100050107
In(1995, October) Contributions to Mineralogy and Petrology Vol. 121 (4) Springer Science and Business Media LLC

See Also

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Alcock, J., Muller, Peter (2000) Anatexis at 700 to 1000 MPa in the aureole of the Marcy anorthosite, Adirondack Highlands, New York. Contributions to Mineralogy and Petrology, 139 (6) 643-654 doi:10.1007/s004100000165
Darling, Robert S., Florence, Frank P. (1995) Apatite light rare earth element chemistry of the Port Leyden nelsonite, Adirondack Highlands, New York; implications for the origin of nelsonite in anorthosite suite rocks. Economic Geology, 90 (4) 964-968 doi:10.2113/gsecongeo.90.4.964
Bohlen, S. R., Essene, E. J. (1977) Feldspar and oxide thermometry of granulites in the Adirondack Highlands. Contributions to Mineralogy and Petrology, 62 (2) 153-169 doi:10.1007/bf00372874
Darling, R.S., and Florence, F.P., 1995, Apatite light rare-earth element chemistry of the Port Leyden nelsonite, Adirondack Highlands, New York: Implications for the origin of nelsonite in anorthosite-suite rocks: Economic Geology, v. 90, p. 964-968.
Whitney, Philip R., Olmsted, James F. (1988) Geochemistry and origin of albite gneisses, northeastern Adirondack Mountains, New York. Contributions to Mineralogy and Petrology, 99 (4) 476-484 doi:10.1007/bf00371938
Bohlen, S. R., Essene, E. J. (1978) Igneous pyroxenes from metamorphosed anorthosite massifs. Contributions to Mineralogy and Petrology, 65 (4) 433-442 doi:10.1007/bf00372290
Alcock, J, Muller, P (2001) Very high temperature, moderate pressure metamorphism in the New Russia gneiss complex, northeastern Adirondack Highlands, metamorphic aureole to the Marcy anorthosite: Reply. Canadian Journal of Earth Sciences, 38 (3) 471-475 doi:10.1139/e00-119
Arnaud, N. O., Kelley, S. P. (1995) Evidence for excess argon during high pressure metamorphism in the dora maira massif (Western Alps, Italy), using an ultra-violet laser ablation microprobe 40Ar-39Ar technique. Contributions to Mineralogy and Petrology, 121 (1) 1-11 doi:10.1007/s004100050086
Alcock, J., Muller, P. (2001) Very high temperature, moderate pressure metamorphism in the New Russia gneiss comple×, northeastern Adirondack Highlands, metamorphic aureole to the Marcy anorthosite: Reply. Canadian Journal of Earth Sciences, 38 (3) 471-475 doi:10.1139/cjes-38-3-471
Alcock, J, Muller, Peter (1999) Very high temperature, moderate pressure metamorphism in the New Russia gneiss complex, northeastern Adirondack Highlands, metamorphic aureole to the Marcy anorthosite. Canadian Journal of Earth Sciences, 36 (1) 1-13 doi:10.1139/e98-072
McLelland, J M, Valley, J W, Essene, E J (2001) Very high temperature, moderate pressure metamorphism in the New Russia gneiss complex, northeastern Adirondack Highlands, metamorphic aureole to the Marcy anorthosite: Discussion. Canadian Journal of Earth Sciences, 38 (3) 465-470 doi:10.1139/e00-026
 
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