Abstract is: In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according to . In some earthquakes the main rupture happens in two or more steps, resulting in multiple main shocks. These are known as doublet earthquakes, and in general can be distinguished from aftershocks in having similar magnitudes and nearly identical seismic waveforms.
P1417 | Encyclopædia Britannica Online ID | science/aftershock-geology |
P646 | Freebase ID | /m/01hyrq |
P11514 | Great Russian Encyclopedia portal ID | aftershok-b80b0f |
P8408 | KBpedia ID | Aftershock |
P6366 | Microsoft Academic ID | 156801008 |
P4297 | MIL-STD-2525 Symbol Identification Code | 10014000001701010000 |
P10283 | OpenAlex ID | C156801008 |
P461 | opposite of | foreshock | Q950713 |
P1687 | Wikidata property | aftershocks | P2320 |
uri / http://www.wikidata.org/entity/L43869-S1 | L43869-S1 |
uri / http://www.wikidata.org/entity/L683606-S1 | L683606-S1 |
Q11521044 | mainshock | followed by | P156 |
P2320 | aftershocks | Wikidata item of this property | P1629 |
Q950713 | foreshock | opposite of | P461 |
Q114041309 | earthquake sequence | has part(s) | P527 |
Q3258284 | Omori's law | main subject | P921 |
Arabic (ar / Q13955) | هزة ارتدادية | wikipedia |
az | Afterşok | wikipedia |
Catalan (ca / Q7026) | Rèplica (sismologia) | wikipedia |
Dotřes | wikipedia | |
Efterskælv | wikipedia | |
Aftershock | wikipedia | |
en-simple | Aftershock | wikipedia |
Esperanto (eo / Q143) | Posttertremo | wikipedia |
Réplica (sismología) | wikipedia | |
Persian (fa / Q9168) | پسلرزه | wikipedia |
Jälkijäristys | wikipedia | |
Réplique (sismologie) | wikipedia | |
gl | Réplica (sismoloxía) | wikipedia |
רעידה עוקבת | wikipedia | |
Replik | wikipedia | |
Utórengés | wikipedia | |
Gempa susulan | wikipedia | |
Eftirskjálfti | wikipedia | |
余震 | wikipedia | |
Форшоктар | wikipedia | |
여진 (지진) | wikipedia | |
ku | Hejeka peyhate | wikipedia |
Pēcgrūdiens | wikipedia | |
Gegar penghujung | wikipedia | |
nan | Û-chìn | wikipedia |
nb | Etterskjelv | wikipedia |
Naschok | wikipedia | |
Wstrząs wtórny | wikipedia | |
Réplica (sismologia) | wikipedia | |
Replică (seismologie) | wikipedia | |
Афтершок | wikipedia | |
แผ่นดินไหวตาม | wikipedia | |
Artçı deprem | wikipedia | |
Афтершок | wikipedia | |
Urdu (ur / Q1617) | پس زلزلہ | wikipedia |
uz | Aftershok | wikipedia |
Dư chấn | wikipedia | |
yue | 餘震 | wikipedia |
餘震 | wikipedia |
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