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![Post facto analysis of Zumpango del Río earthquake of 11 December 2011 (Mw 6.5) (centroid moment tensor catalog), comparing an earthquake early warning system using the tP+3 algorithm with the 2(tS−tP) and (tS−tP) algorithms. The horizontal axis corresponds to GMT beginning at the origin time of the earthquake. The red dot on the map shows the location of the Zumpango earthquake.]()
![AmaxHF versus Amax at CU for earthquakes listed in Table 1. For clarity, only some of the events are identified. Note that the 7 earthquakes with the largest AmaxHF values during the period 1964–2011 are all intraslab earthquakes. AmaxHF of Michoacan and Zumpango earthquakes are 5.4 and 17.0 gal, respectively. None of these events caused damage in the hill zone.]()
![(a), (b) NS accelerograms of the earthquakes of 1985 Michoacan (Mw8.0) and 2011 Zumpango (Mw6.4) recorded at CU. (c), (d) Band-pass filtered (2.5–8.5 Hz) accelerograms of the records shown in (a) and (b). (e) Fourier acceleration spectra at CU of the two earthquakes. (f) Sa, 5% damping, at CU of the two earthquakes.]()
![Post facto analysis of the 11 December 2011 Mw 6.5 Zumpango earthquake with a focal depth of 65 km. The (tS−tP) and the 2(tS−tP) algorithm would have issued an alert in Mexico City ∼27 and 16 s before the arrival of the S waves.]()
![Same as Figure 4 but for the lake-bed zone site SCT. In this case, the AmaxHF values as well as Fourier spectra at high frequencies of the two earthquakes are similar. (a), (b) NS accel-erograms of the earthquakes of 1985 Michoacan (Mw8.0) and 2011 Zumpango (Mw6.4) recorded at the lake-bed zone site SCT. (c), (d) Band-pass filtered (2.5–8.5 Hz) accelerograms of the records shown in (a) and (b). (e) Fourier acceleration spectra at SCT of the two earthquakes. (f) Sa, 5% damping, at SCT of the two earthquakes.]()
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Zumpango earthquake 2011
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Post facto analysis of Zumpango del Río earthquake of 11 December 2011 ( ... Available to Purchase
in A Fast Earthquake Early Warning Algorithm Based on the First 3 s of the P ‐Wave Coda
> Bulletin of the Seismological Society of America
Published: 10 July 2018
Figure 10. Post facto analysis of Zumpango del Río earthquake of 11 December 2011 ( M w 6.5) (centroid moment tensor catalog), comparing an earthquake early warning system using the t P + 3 algorithm with the 2 ( t S − t P ) and ( t S − t P
Image
A max HF versus A max at CU for earthquakes listed in Table 1 . For ... Available to Purchase
in Intraslab versus Interplate Earthquakes as Recorded in Mexico City: Implications for Seismic Hazard
> Earthquake Spectra
Published: 01 May 2015
Figure 6. A max HF versus A max at CU for earthquakes listed in Table 1 . For clarity, only some of the events are identified. Note that the 7 earthquakes with the largest A max HF values during the period 1964–2011 are all intraslab earthquakes. A max HF of Michoacan and Zumpango
Image
(a), (b) NS accelerograms of the earthquakes of 1985 Michoacan ( M w 8.0) ... Available to Purchase
in Intraslab versus Interplate Earthquakes as Recorded in Mexico City: Implications for Seismic Hazard
> Earthquake Spectra
Published: 01 May 2015
Figure 4. (a), (b) NS accelerograms of the earthquakes of 1985 Michoacan ( M w 8.0) and 2011 Zumpango ( M w 6.4) recorded at CU. (c), (d) Band-pass filtered (2.5–8.5 Hz) accelerograms of the records shown in (a) and (b). (e) Fourier acceleration spectra at CU of the two earthquakes. (f) Sa , 5
Image
Post facto analysis of the 11 December 2011 M w 6.5 Zumpango eart... Available to Purchase
in A Fast Earthquake Early Warning Algorithm Based on the First 3 s of the P ‐Wave Coda
> Bulletin of the Seismological Society of America
Published: 10 July 2018
Figure 1. Post facto analysis of the 11 December 2011 M w 6.5 Zumpango earthquake with a focal depth of 65 km. The ( t S − t P ) and the 2 ( t S − t P ) algorithm would have issued an alert in Mexico City ∼ 27 and 16 s before the arrival of the S
Image
Same as Figure 4 but for the lake-bed zone site SCT. In this case, the A... Available to Purchase
in Intraslab versus Interplate Earthquakes as Recorded in Mexico City: Implications for Seismic Hazard
> Earthquake Spectra
Published: 01 May 2015
Figure 7. Same as Figure 4 but for the lake-bed zone site SCT. In this case, the A max HF values as well as Fourier spectra at high frequencies of the two earthquakes are similar. (a), (b) NS accel-erograms of the earthquakes of 1985 Michoacan ( M w 8.0) and 2011 Zumpango ( M w 6.4
Journal Article
Intraslab versus Interplate Earthquakes as Recorded in Mexico City: Implications for Seismic Hazard Available to Purchase
Journal: Earthquake Spectra
Publisher: Earthquake Engineering Research Institute
Published: 01 May 2015
Earthquake Spectra (2015) 31 (2): 795–812.
...Figure 6. A max HF versus A max at CU for earthquakes listed in Table 1 . For clarity, only some of the events are identified. Note that the 7 earthquakes with the largest A max HF values during the period 1964–2011 are all intraslab earthquakes. A max HF of Michoacan and Zumpango...
FIGURES
Journal Article
A Fast Earthquake Early Warning Algorithm Based on the First 3 s of the P ‐Wave Coda Available to Purchase
Publisher: Seismological Society of America
Published: 10 July 2018
Bulletin of the Seismological Society of America (2018) 108 (4): 2068–2079.
...Figure 10. Post facto analysis of Zumpango del Río earthquake of 11 December 2011 ( M w 6.5) (centroid moment tensor catalog), comparing an earthquake early warning system using the t P + 3 algorithm with the 2 ( t S − t P ) and ( t S − t P...
FIGURES
Includes: Supplemental Content
Journal Article
Intraslab Earthquake of 16 June 2013 ( M w 5.9), One of the Closest Such Events to Mexico City Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 01 March 2014
Seismological Research Letters (2014) 85 (2): 268–277.
... 6.1; (d) 22 May 2009, M w 5.7; and (e) 11 December 2011, M w 6.5. With the exception of the 2011 earthquake, the stress drop of other events is about the same. © 2014 by the Seismological Society of America Along the Guerrero segment of the Mexican subduction zone, the region...
FIGURES
Journal Article
Deadly Intraslab Mexico Earthquake of 19 September 2017 ( M w 7.1): Ground Motion and Damage Pattern in Mexico City Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 10 October 2018
Seismological Research Letters (2018) 89 (6): 2193–2203.
... . Dynamic source inversion of the M 6.5 intraslab Zumpango earthquake in central Mexico: A parallel genetic algorithm , J. Geophys. Res. 119 , 7768 – 7785 . Ferrari L. Orozco‐Esquivel T. Manea V. , and Manea M. 2012 . The dynamic history of the Trans‐Mexican volcanic belt...
FIGURES
Includes: Supplemental Content
Journal Article
BIEM_CH: An Efficient Algorithm for Dynamic Rupture Simulation of Complex Fault Systems with Unstructured Meshes and Half‐Space Green’s Function Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 18 December 2024
Seismological Research Letters (2025) 96 (3): 1886–1900.
... . Dynamic source inversion of the M 6.5 intermediate‐depth Zumpango earthquake in central Mexico: A parallel genetic algorithm , J. Geophys. Res. 119 , no. 10 , 7768 – 7785 . Dieterich J. 1979 . Modeling of rock friction: 1. experimental results and constitutive equations , J. Geophys...
FIGURES
Book Chapter
Engineering geology approach to the effects of land subsidence in Mexico City Available to Purchase
Series: GSA Field Guide
Publisher: Geological Society of America
Published: 01 January 2012
DOI: 10.1130/2012.0025(06)
EISBN: 9780813756257
... and fractures mapped. Figure 2. Vertical mean subsidence map (cm/yr) superimposed on amplitude SAR image. Black contours show the limits between the main geotechnical units ( Orden Jurídico Nacional, 2011 ). Sites of interest: 1—Chalco, 2—San Sebastian Tecoloxtitla, 3—Catedral Metropolitana, 4— Nabor...
