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・ 2012 Ibero-American Championships in Athletics
・ 2012 Ibero-American Championships in Athletics – Results
・ 2012 ICC Africa Twenty20 Division Three
・ 2012 ICC Africa Twenty20 Division Two
・ 2012 ICC Awards
・ 2012 ICC European T20 Championship Division Three
・ 2012 Guam national football team results
・ 2012 Guangdong–Hong Kong Cup
・ 2012 Guangxi cadmium spill
・ 2012 Guangzhou Evergrande F.C. season
・ 2012 Guangzhou International Women's Open
・ 2012 Guangzhou International Women's Open – Doubles
・ 2012 Guangzhou International Women's Open – Singles
・ 2012 Guangzhou R&F F.C. season
・ 2012 Guatemala earthquake
2012 Guerrero–Oaxaca earthquake
・ 2012 Guia Race of Macau
・ 2012 Guinea-Bissau coup d'état
・ 2012 Guizhou Renhe F.C. season
・ 2012 Gulf Ice Hockey Championship
・ 2012 Guwahati molestation case
・ 2012 Guzzini Challenger
・ 2012 Guzzini Challenger – Doubles
・ 2012 Guzzini Challenger – Singles
・ 2012 Gwangju FC season
・ 2012 GX17
・ 2012 Gyeongnam FC season
・ 2012 Gymnastics Olympic Test Event
・ 2012 H.E. Mahinda Rajapaksa Under-23 International Football Trophy
・ 2012 H.E. Mahinda Rajapaksa Under-23 International Football Trophy Final


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2012 Guerrero–Oaxaca earthquake : ウィキペディア英語版
2012 Guerrero–Oaxaca earthquake

The 2012 Guerrero–Oaxaca earthquake struck southern Mexico with a moment magnitude of 7.4 at on Tuesday, 20 March. Its epicenter was near Ometepec, in the border between the states of Guerrero and Oaxaca. With a shallow focus of 15 to 20 km, the earthquake caused strong shaking over a large area along the Oaxaca–Guerrero border and the adjacent Pacific coastline. Significant tremors were felt in areas up to several hundred kilometers away, including Mexico City and also in Guatemala. Two people were killed and over 30,000 houses were damaged or destroyed.
==Tectonic setting==
The states of Guerrero and Oaxaca lie above the convergent boundary where the Cocos Plate is being subducted below the North American Plate at a rate of 6.4 cm/yr (2.5 in/yr). The dip of the subducting slab is about 15° as defined by focal mechanisms and hypocenters of previous earthquakes. Seismicity in this area is characterized by regular megathrust earthquakes along the plate interface. In addition, there have been a series of historic normal fault events within the subducting slab.

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