  {"id":149581,"date":"2021-10-13T08:00:16","date_gmt":"2021-10-13T18:00:16","guid":{"rendered":"https:\/\/www.hawaii.edu\/news\/?p=149581"},"modified":"2022-06-17T12:48:52","modified_gmt":"2022-06-17T22:48:52","slug":"tectonic-motion-saturn-moon","status":"publish","type":"post","link":"https:\/\/www.hawaii.edu\/news\/2021\/10\/13\/tectonic-motion-saturn-moon\/","title":{"rendered":"San Andreas Fault-like tectonics discovered on Saturn moon Titan"},"content":{"rendered":"<span class=\"span-reading-time rt-reading-time\" style=\"display: block;\"><span class=\"rt-label rt-prefix\">Reading time: <\/span> <span class=\"rt-time\"> 2<\/span> <span class=\"rt-label rt-postfix\">minutes<\/span><\/span><figure id=\"attachment_149587\" aria-describedby=\"caption-attachment-149587\" style=\"width: 676px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram.jpg\" alt=\"diagram of saturn and titan\" width=\"676\" height=\"381\" class=\"size-full wp-image-149587\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram.jpg 676w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram-130x73.jpg 130w\" sizes=\"auto, (max-width: 676px) 100vw, 676px\" \/><figcaption id=\"caption-attachment-149587\" class=\"wp-caption-text\">Titan\u2019s eccentric orbit causes variations in gravitational tidal forces. (Photo credit: Burkhard,et al 2021)<\/figcaption><\/figure>\n<p>Strike-slip faulting, the type of motion common to California\u2019s well-known San Andreas Fault, was reported recently to possibly occur on Titan, Saturn\u2019s largest moon. New <a href=\"https:\/\/www.google.com\/url?q=https:\/\/authors.elsevier.com\/a\/1dno44L-YbLWd&#038;sa=D&#038;source=docs&#038;ust=1634077686221000&#038;usg=AOvVaw0eXP_EXbQqF1F7loJTioEL\">research<\/a>, led by planetary scientists from the University of <span aria-label=\"Hawaii\">Âé¶¹´«Ã½<\/span> at M&#257;noa <a href=\"https:\/\/www.soest.hawaii.edu\/soestwp\/\">School of Ocean and Earth Science and Technology<\/a> (<abbr>SOEST<\/abbr>), suggests this tectonic motion may be active on Titan, deforming the icy surface.<\/p>\n<p>On multiple ocean worlds, for example Jupiter\u2019s Europa and Saturn\u2019s Enceladus, expressions of strike-slip faulting are well documented. Researchers believe the motion along these faults is driven by variations in diurnal tidal stresses\u2014the push and pull caused by the relative motion of a moon and its planet.<\/p>\n<figure id=\"attachment_149588\" aria-describedby=\"caption-attachment-149588\" style=\"width: 300px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram-2-300x169.jpg\" alt=\"tectonics diagram\" width=\"300\" height=\"169\" class=\"size-medium wp-image-149588\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram-2-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram-2-130x73.jpg 130w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/10\/manoa-soest-saturn-titan-diagram-2.jpg 676w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><figcaption id=\"caption-attachment-149588\" class=\"wp-caption-text\">Possible slip directions on (a) Titan and (b) San Andreas Fault. (Photo credit: Burkhard et al. 2021)<\/figcaption><\/figure>\n<h2>Lakes and seas on the surface<\/h2>\n<p>Titan has a thick crust made of rock-hard water ice. And Titan is the only place besides Earth known to have liquids in the form of lakes and seas on its surface. However, Titan\u2019s liquids are hydrocarbons, such as methane and ethane.<\/p>\n<p>With limited observational data available, <strong>Liliane Burkhard<\/strong>, doctoral candidate and graduate student researcher in the <a href=\"http:\/\/www.soest.hawaii.edu\/gg\/\">Department of Earth Sciences<\/a> at <abbr>SOEST<\/abbr>, and co-authors examined the possibility for strike-slip tectonics using physics-based faulting models. The model calculations take into account the tidal stress on Titan, the orientations of candidate faults, crustal properties (including pore fluid pressure), and the stress needed to cause the surface material to fail or crack.<\/p>\n<p>&ldquo;Titan is unique because it is the only known satellite to have stable liquids on the surface,&rdquo; said Burkhard. &ldquo;We, therefore, were able to make an argument for integrating pore fluid pressures in our calculations, which can reduce the shear strength of the icy crust and may play a key role in the tectonic evolution of Titan.&rdquo;<\/p>\n<p>In this novel study, the scientists found that a combination of diurnal tidal stresses and pore fluid pressures promotes shear failure for shallow faults on Titan. Further, faults near the equator that strike near east-west are optimally oriented for potential failure.<\/p>\n<p>&ldquo;This is an exciting revelation,&rdquo; said Burkhard. &ldquo;Our results suggest that under these conditions, shear failure is not only possible, but may be an active deformation mechanism on the surface and in the subsurface of Titan, and could potentially serve as a pathway for subsurface liquids to rise to the surface. This can potentially facilitate material transport that could affect habitability.&rdquo;<\/p>\n<h2>Future missions<\/h2>\n<p>In the future, Burkhard hopes to conduct more research on the deformation of not only Titan but also other icy moons to uncover their tectonic history and astrobiological implications. Several remote sensing missions are scheduled to launch within the next few years to investigate Ganymede (ESA JUICE, 2022), Europa (NASA Clipper, 2024) and Titan (NASA Dragonfly, 2027).<\/p>\n<p>&ldquo;Combining new observations with our modeling techniques will strengthen our understanding of the icy crust and pinpoint the best location for exploration with a future lander mission and possibly access to the interior ocean,&rdquo; she added.<\/p>\n<p>This research is an example of <abbr title=\"University of Hawaii\">UH<\/abbr> M&#257;noa\u2019s goal of <a href=\"https:\/\/manoa.hawaii.edu\/wp\/wp-content\/uploads\/2020\/12\/manoa-2025-strategic-plan.pdf#page=25\">Excellence in Research: Advancing the Research and Creative Work Enterprise<\/a> (<span class=\"small-text\"><abbr title=\"Portable Document Format\">PDF<\/abbr><\/span>), one of four goals identified in the <a href=\"https:\/\/manoa.hawaii.edu\/wp\/wp-content\/uploads\/2020\/12\/manoa-2025-strategic-plan.pdf\">2015&#8211;25 Âé¶¹´«Ã½<\/a> (<span class=\"small-text\"><abbr title=\"Portable Document Format\">PDF<\/abbr><\/span>), updated in December 2020.<\/p>\n<p><a href=\"https:\/\/www.soest.hawaii.edu\/soestwp\/announce\/news\/strike-slip-faulting-may-be-active-on-saturns-largest-moon-titan\/\">For more information, see <abbr>SOEST<\/abbr>\u2019s website<\/a>.<\/p>\n<p><em>&#8211;By Marcie Grabowski<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"<p><abbr>UH<\/abbr> research suggests strike-slip faulting may be active on Titan, deforming the icy surface.<\/p>\n","protected":false},"author":16,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[30],"tags":[1187,1467,1363,92,174,9],"class_list":["post-149581","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research","tag-earth-science","tag-manoa-excellence-in-research","tag-manoa-research","tag-school-of-ocean-and-earth-science-and-technology","tag-space","tag-uh-manoa","entry","has-media"],"aioseo_notices":[],"jetpack_featured_media_url":"","_links":{"self":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/149581","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/users\/16"}],"replies":[{"embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/comments?post=149581"}],"version-history":[{"count":7,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/149581\/revisions"}],"predecessor-version":[{"id":160866,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/149581\/revisions\/160866"}],"wp:attachment":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/media?parent=149581"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/categories?post=149581"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/tags?post=149581"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}