Koppers, A. A. P. ; Sano, T.; Natland, J. H.; Widdowson, M.; Almeev, R.; Greene, A. R.; Murphy, D. T.; Delacour, A.; Miyoshi, M.; Shimizu, K.; Li, S.; Hirano, N. and Geldmacher, J.
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|DOI (Digital Object Identifier) Link:||http://doi.org/10.2204/iodp.proc.324.109.2010|
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Drilling during Ocean Drilling Program Leg 198 at Site 1213 recovered three massive basalt units (8–15 m thick) from the southern flank of Tamu Massif at Shatsky Rise. Originally, these igneous units were interpreted to represent three diabase sills. During Integrated Ocean Drilling Program Expedition 324, this core was redescribed leading to the new conclusion that these diabase units represent three submarine massive basalt flows. These massive submarine flows were probably emplaced as inflated compound sheet flows during eruptions similar to those in large oceanic plateaus and continental flood basalts.
|Item Type:||Book Chapter|
|Copyright Holders:||2010 Integrated Ocean Drilling Program Management International, Inc.|
|Extra Information:||ISSN 1930-1014
|Academic Unit/Department:||Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Mike Widdowson|
|Date Deposited:||09 Dec 2010 09:55|
|Last Modified:||04 Oct 2016 12:08|
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