Anisotropic thermal conductivity of antigorite along slab subduction impacts seismicity of intermediate-depth earthquakes
Yu-Hsiang Chien,
Enrico Marzotto,
Yi-Chi Tsao
et al.
Abstract:Double seismic zones (DSZs) are a feature of some subducting slabs, where intermediate-depth earthquakes (~70–300 km) align along two separate planes. The upper seismic plane is generally attributed to dehydration embrittlement, whereas mechanisms forming the lower seismic plane are still debated. Thermal conductivity of slab minerals is expected to control the temperature evolution of subducting slabs, and therefore their seismicity. However, effects of the potential anisotropic thermal conductivity of layere… Show more
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