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Brueckner, Hannes K. (1977) A crustal origin for eclogites and a mantle origin for garnet peridotites: Strontium isotopic evidence from clinopyroxenes. Contributions to Mineralogy and Petrology, 60 (1) 1-15 doi:10.1007/bf00372847

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Reference TypeJournal (article/letter/editorial)
TitleA crustal origin for eclogites and a mantle origin for garnet peridotites: Strontium isotopic evidence from clinopyroxenes
JournalContributions to Mineralogy and Petrology
AuthorsBrueckner, Hannes K.Author
Year1977Volume60
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00372847Search in ResearchGate
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Mindat Ref. ID74441Long-form Identifiermindat:1:5:74441:8
GUID0
Full ReferenceBrueckner, Hannes K. (1977) A crustal origin for eclogites and a mantle origin for garnet peridotites: Strontium isotopic evidence from clinopyroxenes. Contributions to Mineralogy and Petrology, 60 (1) 1-15 doi:10.1007/bf00372847
Plain TextBrueckner, Hannes K. (1977) A crustal origin for eclogites and a mantle origin for garnet peridotites: Strontium isotopic evidence from clinopyroxenes. Contributions to Mineralogy and Petrology, 60 (1) 1-15 doi:10.1007/bf00372847
In(1977) Contributions to Mineralogy and Petrology Vol. 60 (1) Springer Science and Business Media LLC

See Also

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Brueckner, Hannes K. (1975) Contact and fracture ultramafic assemblages from Norway: Rb-Sr evidence for crustal contamination. Contributions to Mineralogy and Petrology, 49 (1) 39-48 doi:10.1007/bf00371077
Brueckner, Hannes K. (1974) “Mantle” Rb/Sr and 87Sr/86Sr ratios for clinopyroxenes from Norwegian garnet peridotites and pyroxenites. Earth and Planetary Science Letters, 24 (1) 26-32 doi:10.1016/0012-821x(74)90004-1
Simakov, S. K. (2006) Redox state of eclogites and peridotites from sub-cratonic upper mantle and a connection with diamond genesis. Contributions to Mineralogy and Petrology, 151 (3) 282-296 doi:10.1007/s00410-005-0058-z
Loomis, Timothy P., Gottschalk, Richard R. (1981) Hydrothermal origin of mafic layers in alpine-type peridotites: Evidence from the seiad ultramafic complex, California, USA. Contributions to Mineralogy and Petrology, 76 (1) 1-11 doi:10.1007/bf00373677
Beyer, C., Frost, D. J., Miyajima, N. (2015) Experimental calibration of a garnet–clinopyroxene geobarometer for mantle eclogites. Contributions to Mineralogy and Petrology, 169 (2) doi:10.1007/s00410-015-1113-z
Nimis, P. (1995) Clinopyroxenes from plagioclase peridotites (Zabargad Island, Red Sea) and comparison between high- and low-pressure mantle clinopyroxenes. Mineralogy and Petrology, 53 (1) 49-61 doi:10.1007/bf01171946
Cortini, Massimo, Hermes, O. Don (1981) Sr isotopic evidence for a multi-source origin of the potassic magmas in the neapolitan area (S. Italy) Contributions to Mineralogy and Petrology, 77 (1) 47-55 doi:10.1007/bf01161501
Zipfel, J., W�rner, G. (1992) Four- and five-phase peridotites from a continental rift system: evidence for upper mantle uplift and cooling at the Ross Sea margin (Antarctica) Contributions to Mineralogy and Petrology, 111 (1) 24-36 doi:10.1007/bf00296575
Vollmer, Ronald (1977) Isotopic evidence for genetic relations between acid and alkaline rocks in Italy. Contributions to Mineralogy and Petrology, 60 (2) 109-118 doi:10.1007/bf00372277
McLelland, James M., Whitney, Philip R. (1977) The origin of garnet in the anorthosite-charnockite suite of the Adirondacks. Contributions to Mineralogy and Petrology, 60 (2) 161-181 doi:10.1007/bf00372280
Čopjaková, Renata, Kotková, Jana (2018) Composition of barian mica in multiphase solid inclusions from orogenic garnet peridotites as evidence of mantle metasomatism in a subduction zone setting. Contributions to Mineralogy and Petrology, 173 (12) doi:10.1007/s00410-018-1534-6
 
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