{"id":13,"date":"2017-06-06T16:32:27","date_gmt":"2017-06-06T20:32:27","guid":{"rendered":"https:\/\/www2.whoi.edu\/staff\/template-blue-prepop\/?page_id=13"},"modified":"2020-10-26T14:16:47","modified_gmt":"2020-10-26T18:16:47","slug":"projects","status":"publish","type":"page","link":"https:\/\/www2.whoi.edu\/staff\/jcanales\/projects\/","title":{"rendered":"Projects"},"content":{"rendered":"\n\t

Projects<\/strong><\/h1>\n

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Cascadia Ocean Bottom Sensors Deployment<\/strong><\/a><\/h3>\n

The goal of this project is to acquire an open-access, marine wide-angle seismic reflection\/refraction dataset across the Cascadia accretionary wedge. This survey will consist of the deployment and recovery of short-period multicomponent ocean bottom seismometers \u00a0and large-N arrays of ocean bottom nodes. The sensors will record the controlled-source acoustic signals of a seismic reflection survey off the Cascadia margin planned for summer 2020.<\/p>\n\t

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Juan De Fuca Plate: From Ridge to Trench<\/strong><\/a><\/h3>\n

In June-July 2012 we conducted a two-ship active source seismic experiment aiming to characterize crustal and shallow mantle velocities and distribution of faulting along two ridge-perpendicular transects spanning the full width of the JdF plate, and a trench-parallel line to characterize along-trench variations in the architecture and velocity structure of the down-going plate across distinct structural regimes of the Cascadia subduction zone.<\/p>\n\t

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Rifting in the Okavango<\/strong><\/a><\/h3>\n

SEISORZ is the active-source seismic component of the PRIDE project.\u00a0 The PRIDE project aims to understand the processes of continental rift initiation and evolution by analyzing along-axis trends in the southern portion of the East Africa rift system, from Botswana through Zambia and Malawi.<\/p>\n\t

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MARINER Rainbow<\/strong><\/a><\/h3>\n

This project consists of a three-part seismic study of the physical architecture of the crustal and upper mantle at Rainbow to address the following fundamental question: What is the relationship between magmatism, faulting, substrate lithology, and hydrothermal circulation at the Rainbow hydrothermal field?<\/p>\n\t

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Image from Escartin and Canales (2011)<\/p><\/div>\n

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Chapman Conference on Oceanic Detachments<\/strong><\/a><\/h3>\n

Detachments in Oceanic Lithosphere: Deformation, Magmatism, Fluid Flow and Ecosystems.<\/p>\n\t

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Seismic Investigations of Oceanic Core Complexes<\/strong><\/a><\/h3>\n

Oceanic core complexes (OCCs) are deep sections of the oceanic lithosphere exhumed tothe seafloor by long-lived detachment faults.<\/p>\n

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The Juan de Fuca Ridge and its Flanks<\/strong><\/a><\/h3>\n

In 2002, a team from the Lamont-Doherty EarthObservatory, Woods Hole Oceanographic Institution, and Scripps Institution of Oceanography conducted an extensive MCS investigation of the Juan de Fuca Ridge (JdFR) and its flanks.<\/p>\n\t

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3D Multichannel Seismic Survey of the Magmatic-Hydrothermal System of the East Pacific Rise 9o<\/sup>50’N<\/strong><\/a><\/h3>\n

The East Pacific Rise (EPR) at 9\u00b050\u2019N, one of the fastest spreading centers on Earth, is a highly dynamic magmatic, hydrothermal, and biological system that presents an ideal opportunity to observe and measure changes in and linkages between surface and sub-surface mid-ocean ridge processes on decadal time-scales.<\/p>\n","protected":false},"excerpt":{"rendered":"

Projects Cascadia Ocean Bottom Sensors Deployment The goal of this project is to acquire an open-access, marine wide-angle seismic reflection\/refraction dataset across the Cascadia accretionary wedge. This survey will consist of the deployment and recovery of short-period multicomponent ocean bottom seismometers \u00a0and large-N arrays of ocean bottom nodes. The sensors will record the controlled-source acoustic…<\/p>\n","protected":false},"author":73,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/pages\/13"}],"collection":[{"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/users\/73"}],"replies":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/comments?post=13"}],"version-history":[{"count":3,"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/pages\/13\/revisions"}],"predecessor-version":[{"id":387,"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/pages\/13\/revisions\/387"}],"wp:attachment":[{"href":"https:\/\/www2.whoi.edu\/staff\/jcanales\/wp-json\/wp\/v2\/media?parent=13"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}