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Tate, Marcus C., Clarke, D. Barrie, Heaman, Larry M. (1997) Progressive hybridisation between Late Devonian mafic-intermediate and felsic magmas in the Meguma Zone of Nova Scotia, Canada. Contributions to Mineralogy and Petrology, 126 (4) 401-415 doi:10.1007/s004100050259

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Reference TypeJournal (article/letter/editorial)
TitleProgressive hybridisation between Late Devonian mafic-intermediate and felsic magmas in the Meguma Zone of Nova Scotia, Canada
JournalContributions to Mineralogy and Petrology
AuthorsTate, Marcus C.Author
Clarke, D. BarrieAuthor
Heaman, Larry M.Author
Year1997 (February)Volume126
Page(s)401-415Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050259Search in ResearchGate
Mindat Ref. ID77483Long-form Identifiermindat:1:5:77483:5
GUID641c43f5-b79a-42c1-8dca-b889ecf62c95
Full ReferenceTate, Marcus C., Clarke, D. Barrie, Heaman, Larry M. (1997) Progressive hybridisation between Late Devonian mafic-intermediate and felsic magmas in the Meguma Zone of Nova Scotia, Canada. Contributions to Mineralogy and Petrology, 126 (4) 401-415 doi:10.1007/s004100050259
Plain TextTate, Marcus C., Clarke, D. Barrie, Heaman, Larry M. (1997) Progressive hybridisation between Late Devonian mafic-intermediate and felsic magmas in the Meguma Zone of Nova Scotia, Canada. Contributions to Mineralogy and Petrology, 126 (4) 401-415 doi:10.1007/s004100050259
In(1997, February) Contributions to Mineralogy and Petrology Vol. 126 (4) Springer Science and Business Media LLC

See Also

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Tate, Marcus C., Clarke, D. Barrie (1995) Petrogenesis and regional tectonic significance of Late Devonian mafic intrusions in the Meguma Zone, Nova Scotia. Canadian Journal of Earth Sciences, 32 (11) 1883-1898 doi:10.1139/e95-145
Tate, M.C. (1995) The relationship between Late Devonian mafic intrusions and peraluminous granitoid generation in the Meguma lithotectonic zone, Nova Scotia, Canada. Ph.D. Thesis, Deptartment of Earth Sciences, Dalhousie University, Halifax, Nova Scotia, 528 p.
Tate, M (1997) Compositional diversity among Late Devonian peraluminous granitoid intrusions in the Meguma Zone of Nova Scotia, Canada. Lithos, 39 (3) 179-194 doi:10.1016/s0024-4937(97)00002-9
Clarke, D Barrie, Fallon, Raymond, Heaman, Larry M (2002) Interaction among Upper Crustal, Lower Crustal, and Mantle Materials in the Port Mouton Pluton, Meguma Zone, Southwest Nova Scotia: Erratum. Canadian Journal of Earth Sciences, 39 (4) 560 doi:10.1139/e02-902
Tate, M. C., Clarke, D. B. (1993) Origin of the Late Devonian Weekend lamprophyre dykes, Meguma Zone, Nova Scotia. Canadian Journal of Earth Sciences, 30 (12) 2295-2304 doi:10.1139/e93-199
Clarke, D Barrie, Fallon, Raymond, Heaman, Larry M (2000) Interaction among upper crustal, lower crustal, and mantle materials in the Port Mouton pluton, Meguma Lithotectonic Zone, southwest Nova Scotia. Canadian Journal of Earth Sciences, 37 (4) 579-600 doi:10.1139/e99-124
Maillet, Lynne A., Barrie Clarke, D. (1985) Cordierite in the peraluminous granites of the Meguma Zone, Nova Scotia, Canada. Mineralogical Magazine, 49 (354) 695-702 doi:10.1180/minmag.1985.049.354.08
Di Vincenzo, Gianfranco, Rocchi, Sergio (1999) Origin and interaction of mafic and felsic magmas in an evolving late orogenic setting: the Early Paleozoic Terra Nova Intrusive Complex, Antarctica. Contributions to Mineralogy and Petrology, 137 (1) 15-35 doi:10.1007/s004100050579
Eberz, G. W., Clarke, D. B., Chatterjee, A. K., Giles, P. S. (1991) Chemical and isotopic composition of the lower crust beneath the Meguma Lithotectonic Zone, Nova Scotia: evidence from granulite facies xenoliths. Contributions to Mineralogy and Petrology, 109 (1) 69-88 doi:10.1007/bf00687201
Tate, Marcus C. (1994) The nature and origin of enclaves in four peraluminous granitoid intrusions from the Meguma Zone, Nova Scotia. Atlantic Geology, 30 (3) doi:10.4138/2130
Pistone, Mattia, , , Blundy, Jonathan D., Brooker, Richard A. (2016) Textural and chemical consequences of interaction between hydrous mafic and felsic magmas: an experimental study. Contributions to Mineralogy and Petrology, 171 (1) doi:10.1007/s00410-015-1218-4
 
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