Japan Geoscience Union Meeting 2018

Presentation information

[EE] Evening Poster

S (Solid Earth Sciences) » S-IT Science of the Earth's Interior & Tectonophysics

[S-IT24] Probing the Earth's interior with geophysical observation on seafloor

Tue. May 22, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Daisuke Suetsugu(Department of Deep Earth Structure and Dynamics Research, Japan Agency for Marine-Earth Science and Technology), Guilhem BARRUOL(CNRS, Institut de Physique du Globe de Paris, France), Hitoshi Kawakatsu(東京大学地震研究所, 共同), Douglas Wiens(Washington University in St Louis)

[SIT24-P07] Toward complete tomography of the Earth’s interior with floating robotic acoustic sensors in the oceans: the EarthScope-Oceans

*Masayuki Obayashi1, Hiroko Sugioka2, Hajime Shiobara3 (1.D-EARTH, Japan Agency for Marine-Earth Science and Technology, 2.Department of Planetology, Kobe University, 3.Eartquake Research Institute, University of Tokyo)

Keywords:tomography, floating seismometer

The tomography techniques of imaging the earth’s interior have been improved significantly over the past three decades. The resolution of the earth’s interior images, however, has been severely limited by the lack of seismic stations in the oceans that cover the 2/3 of the earth’s surface. The classical approach to improve resolution in oceanic regions is covering the ocean floor with ocean-bottom seismometers, however these observations are of short duration (limited by battery life) and depend on available ship, can only cover a restricted surface at any given time and are very costly. Here we introduce a project ‘EarthScope-Oceans’ to measure seismic signals by deploying floating robotic acoustic sensors (MERMAIDs) that is driven by France, USA, China, UK, Korea and Japan. In the previous Mermaid experiment, these ‘Mermaids’ have recorded teleseismic waves that are crucial to provide resolution for tomographic images of the deep mantle beneath oceanic areas, as well as swarms of earthquakes that are too small to be observed on land, indicative of tectonic motions on oceanic ridges. The data transmission is in quasi-real time by satellites (Iridium). A new version of the Mermaid, of much larger capacity, with a lifetime of five to six years is available for deployment.

We plan to launch more than 30 Mermaids in the Southern Pacific, where contains both complex subduction zones and mantle plumes, in 2018 and 2019. Unique and very precious data from previously un-sampled regions of the South Pacific Ocean that will provide crucial constraints at mid-mantle depths and improve the tomographic images further analogue and numerical geodynamic modeling of mantle plumes based on the robust features of the tomographic images.