Mauna Loa's submarine western flank: Evidence for deep volcanic spreading and hydrothermal alteration

dc.contributor.advisorMorgan, Julia K.en_US
dc.creatorBorchers, Deanna Carolineen_US
dc.date.accessioned2009-06-04T08:48:11Zen_US
dc.date.available2009-06-04T08:48:11Zen_US
dc.date.issued2005en_US
dc.description.abstractObservations of submersible dives across Mauna Loa's submarine western flank suggest the flank has been influenced by a number of interacting processes, including large-scale sector collapses, deep volcanic spreading, and hydrothermal alteration. Subaerially derived pillow lavas observed draping the upper flank are in strong contrast to the volcaniclastic debris discovered at the toe of the flank. The distribution of rock types, deformation structures, and alteration phases within the volcaniclastic rocks suggest the mid-slope bench is constructed of a series of thrust sheets formed by seaward sliding of the western flank. Volcaniclastic sediments within the bench have been locally altered by circulation of hot hydrothermal fluids along the faults. The remnant landslide scar, from which much of the clastic debris within the bench derived, has largely been concealed by a flood of new lava flows, many of which crossed the shoreline and were deposited on the upper flank as pillow basalts.en_US
dc.format.extent131 p.en_US
dc.format.mimetypeapplication/pdfen_US
dc.identifier.callnoTHESIS GEOL. 2005 BORCHERSen_US
dc.identifier.citationBorchers, Deanna Caroline. "Mauna Loa's submarine western flank: Evidence for deep volcanic spreading and hydrothermal alteration." (2005) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/17758">https://hdl.handle.net/1911/17758</a>.en_US
dc.identifier.urihttps://hdl.handle.net/1911/17758en_US
dc.language.isoengen_US
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.en_US
dc.subjectGeologyen_US
dc.titleMauna Loa's submarine western flank: Evidence for deep volcanic spreading and hydrothermal alterationen_US
dc.typeThesisen_US
dc.type.materialTexten_US
thesis.degree.departmentEarth Scienceen_US
thesis.degree.disciplineNatural Sciencesen_US
thesis.degree.grantorRice Universityen_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Scienceen_US
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