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Message

Found 2 translations.

NameCurrent message text
 h English (en)(fortsch) An irregular seismic discontinuity sometimes seen at 8–11 km in continental crust, usually attributed to a change from granitic to dioritic composition.
 h Spanish (es)Una discontinuidad sísmica irregular que a veces se observa a 8–11 km en la corteza continental, generalmente atribuida a un cambio de la composición granítica a la composición diorítica.