Oceanic volcanoes formed by mantle plumes, such as those of Hawaii and Iceland, strongly influence our views about the deep Earth (Morgan, 1971; Sleep, 2006). These volcanoes are the principal geochemical probe into the deep

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http://www.iodp.org/iodp_journals/1_Deep_Drilling_into_Mantle_SD7.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.605.3349 2023-05-15T16:46:16+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.605.3349 http://www.iodp.org/iodp_journals/1_Deep_Drilling_into_Mantle_SD7.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.605.3349 http://www.iodp.org/iodp_journals/1_Deep_Drilling_into_Mantle_SD7.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.iodp.org/iodp_journals/1_Deep_Drilling_into_Mantle_SD7.pdf text ftciteseerx 2016-01-08T14:13:28Z Oceanic volcanoes formed by mantle plumes, such as those of Hawaii and Iceland, strongly influence our views about the deep Earth (Morgan, 1971; Sleep, 2006). These volcanoes are the principal geochemical probe into the deep Text Iceland Unknown
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description Oceanic volcanoes formed by mantle plumes, such as those of Hawaii and Iceland, strongly influence our views about the deep Earth (Morgan, 1971; Sleep, 2006). These volcanoes are the principal geochemical probe into the deep
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