Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland
Title: Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland, Author: Michael T. Franklyn, Location: Thode The pillow lavas of the lower Crabb Creek area or the Bay of Islands Ophiolite complex exhibit geochemical and petrographic characteristics similar to meta...
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1985
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ftmcmaster:oai:macsphere.mcmaster.ca:11375/19846 2023-05-15T17:20:22+02:00 Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland Franklyn, Michael T. McNutt, R.H. Geology 1985-04 http://hdl.handle.net/11375/19846 en eng http://hdl.handle.net/11375/19846 Thesis 1985 ftmcmaster 2022-03-22T21:13:48Z Title: Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland, Author: Michael T. Franklyn, Location: Thode The pillow lavas of the lower Crabb Creek area or the Bay of Islands Ophiolite complex exhibit geochemical and petrographic characteristics similar to metamorphosed mid-ocean ridge basalts. Depletions of Ca and Mg and the enrichment or K, P, Na, Si and H2O are the result of hydrothermal alteration and the metasomatic influence seawater on fresh basalts. All samples exhibit typical low grade, greenschist Facies metamorphic mineral assemblages. 'Fresh', moderately altered and severely altered suites can be recognized by the degree or degradation of the phenocryst and matrix phases. Immobile trace elements show these metabasalts to originally be ocean-floor tholeiites . Thesis Bachelor of Science (BSc) Thesis Newfoundland MacSphere (McMaster University) |
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Open Polar |
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MacSphere (McMaster University) |
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ftmcmaster |
language |
English |
description |
Title: Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland, Author: Michael T. Franklyn, Location: Thode The pillow lavas of the lower Crabb Creek area or the Bay of Islands Ophiolite complex exhibit geochemical and petrographic characteristics similar to metamorphosed mid-ocean ridge basalts. Depletions of Ca and Mg and the enrichment or K, P, Na, Si and H2O are the result of hydrothermal alteration and the metasomatic influence seawater on fresh basalts. All samples exhibit typical low grade, greenschist Facies metamorphic mineral assemblages. 'Fresh', moderately altered and severely altered suites can be recognized by the degree or degradation of the phenocryst and matrix phases. Immobile trace elements show these metabasalts to originally be ocean-floor tholeiites . Thesis Bachelor of Science (BSc) |
author2 |
McNutt, R.H. Geology |
format |
Thesis |
author |
Franklyn, Michael T. |
spellingShingle |
Franklyn, Michael T. Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland |
author_facet |
Franklyn, Michael T. |
author_sort |
Franklyn, Michael T. |
title |
Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland |
title_short |
Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland |
title_full |
Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland |
title_fullStr |
Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland |
title_full_unstemmed |
Seawater Alteration of Pillow Lavas, Bay of Islands Ophiolite Complex, Western Newfoundland |
title_sort |
seawater alteration of pillow lavas, bay of islands ophiolite complex, western newfoundland |
publishDate |
1985 |
url |
http://hdl.handle.net/11375/19846 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
http://hdl.handle.net/11375/19846 |
_version_ |
1766099235216818176 |