| 单词 | Mohorovicic discontinuity |
| 释义 | Mohorovicic discontinuity [´mō·hō`rō·vǝ´chich dis´känt·ǝn`ü·ǝd·ē] GEOPHYSICS A seismic discontinuity that separates the earth's crust from the subjacent mantle, inferred from travel time curves indicating that seismic waves undergo a sudden increase in velocity. Also known as Moho. |
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