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Earth and Space Sciences · 术语表

什么是 Wadati–Benioff zone？

又称： Wadati--Benioff zone

Definition 15.2 High School Earth and Space Sciences · 第 15 章 — Subduction Zones

A Wadati–Benioff zone is the inclined band of earthquakes that starts at a trench and goes deeper and deeper beneath the overriding plate, down to as much as about $700\,\mathrm{km}$ .

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Definition 14.3 University Earth and Space Sciences — Year 1 · 第 14 章 — Active Margins

A Wadati–Benioff zone is the inclined zone of earthquakes that starts near a trench and deepens beneath the overriding plate, down to as much as about $700\,\mathrm{km}$ : it outlines the subducting slab.

The Kuril subduction zone: earthquakes of magnitude 5 or more, 1976–2025, coloured by depth, and the volcanoes active in the last ten thousand years. The trench (teeth on the overriding plate) and the band of the section shown in the next figure (dashed, 150\, km on each side of the section line). Data: USGS earthquake catalogue; Smithsonian Global Volcanism Program; trench from Bird (2003); coast from Natural Earth. — The Kuril subduction zone: earthquakes of magnitude 5 or more, 1976–2025, coloured by depth, and the volcanoes active in the last ten thousand years. The trench (teeth on the overriding plate) and the band of the section shown in the next figure (dashed, $150\,\mathrm{km}$ on each side of the section line). Data: USGS earthquake catalogue; Smithsonian Global Volcanism Program; trench from Bird (2003); coast from Natural Earth.

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