Rapid dike emplacement leads to eruptions and hydrothermal plume release during seafloor spreading events

• DOI: 10.1130/g23476a.1
• Publication Date: 2007-06-28T19:47:40Z
• Authors: R.P. Dziak; D.R Bohnenstiehl; J.P. Cowen; E.T. Baker; K.H. Rubin; J.H. Haxel; M.J. Fowler
• Keywords: Seafloor Spreading; Marine geology; Dike; Seamount

Research Article| July 01, 2007 Rapid dike emplacement leads to eruptions and hydrothermal plume release during seafloor spreading events R.P. Dziak; Dziak 1Cooperative Institute for Marine Resource Studies, Oregon State University, Pacific Environmental Laboratory, National Oceanic Atmospheric Administration (NOAA), Hatfield Science Center, Newport, 97365, USA Search other works by this author on: GSW Google Scholar D.R Bohnenstiehl; Bohnenstiehl 2Department of Marine, Earth Sciences, North Carolina Rayleigh, 27695, J.P. Cowen; Cowen 3Department Oceanography, University Hawaii, Honolulu, Hawaii 96817, E.T. Baker; Baker 4Pacific Seattle, Washington 98115, K.H. Rubin; Rubin 5Department Geology Geophysics, School Ocean Technology, J.H. Haxel; Haxel 6Cooperative M.J. Fowler Author Article Information Publisher: Geological Society America Received: 30 Oct 2006 Revision 01 Feb Accepted: 07 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print 0091-7613 (2007) 35 (7): 579–582. https://doi.org/10.1130/G23476A.1 history Cite View This Citation Add Manager Share Icon Facebook Twitter LinkedIn MailTo Tools Get Permissions Site Dziak, Bohnenstiehl, Cowen, Baker, Rubin, Haxel, Fowler; events. 2007;; doi: Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Dropdown Menu input auto suggest filter your All ContentBy SocietyGeology Advanced Abstract The creation ocean crust rapid injection magma at mid-ocean ridges can lead lava onto the "event plumes," which are huge volumes anomalously warm water enriched in reduced chemicals that rise up 1 km above seafloor. Here, we use seismic data show event plumes correspond diking episodes with high velocities onset within rift zone. These attributes result from excess pressure source, likely due a new influx melt mantle. dynamic magmatic conditions be detected remotely may predict likelihood future You do not have access content, please speak institutional administrator if you feel should access.