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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Accurate XANES determination of microscale Fe redox state in clinopyroxene: a multivariate approach with polarization-dependent Fe K -edge XAFS Available to Purchase
Paired Metamorphism of SW Japan and Implications for Tectonics of Convergent Margins Available to Purchase
Thermal Modeling of the Sanbagawa and Ryoke Belts Available to Purchase
Geochronology of the Sanbagawa Belt: Younger and Faster than Before Available to Purchase
Identifying plutons associated with long-lived volcanism by thermal modeling of contact metamorphic aureoles Available to Purchase
Recognition of Detrital Carbonaceous Material in the Ryoke Metamorphic Belt by Using Raman Thermometry: Implications for Thermal Structure and Detrital Origin Open Access
Crystallographic preferred orientation of talc determined by an improved EBSD procedure for sheet silicates: Implications for anisotropy at the slab–mantle interface due to Si-metasomatism Available to Purchase
Tsunamis: geology, hazards and risks – introduction Open Access
Geological studies in tsunami research since the 2011 Tohoku earthquake Available to Purchase
Abstract The 2011 Tohoku earthquake, tsunami and resulting damage is often referred to as 3.11 after the date on which it took place. Leading to almost 20 000 people dead or missing, a major nuclear disaster and severe economic damage, 3.11 represents the biggest challenge faced by Japan since the end of World War II. Before 3.11, the possibility of a Mw 9 earthquake in this area was not generally recognized, highlighting the need to reassess seismic risk in NE Japan. The large amount of new quantitative data covering a range of disciplines and from onshore and offshore studies makes 3.11 an important case study that can contribute to improving our understanding of tsunamis, including their formation, their effects on coastal regions and the effectiveness of defensive measures old and new. Geological studies have a key role to play in this new phase of tsunami studies and this is the only method available for determining recurrence intervals over timescales of thousands of years. Data from 3.11 have improved our ability to identify sedimentary records of tsunami events and to estimate tsunami size from geological data. More complete databases will provide invaluable information for long-term planning of coastal regions in convergent plate margins.