Pablo Gabriel Silva Barroso
Biographic Data
| ID | 4791003 |
|---|---|
| NAME | Pablo Gabriel Silva Barroso |
| GIVEN NAMES | Pablo Gabriel Silva |
| FAMILY NAME | Barroso |
| SIGNATURE | BARROSO P G S |
| AFFILIATIONS | Catholic University of Ávila |
| ORCID | 0000-0003-1470-292X |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 1 |
| AUTHOR COUNT | 5 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2015 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 1 |
Reply to comment by Suárez et al., did Teotihuacán collapse due to a major earthquake? On “Teotihuacan ancient culture affected by megathrust earthquakes during the early Epiclassic period (Mexico)”
Teotihuacan ancient culture affected by megathrust earthquakes during the early Epiclassic Period (Mexico)
Teotihuacan was one of the thriving cultures in the Mesoamerica pre-Hispanic times, located in the Central Valley of Mexico. The city-state was a dominant centre point during the Classic period and its influence affected other contemporaneous cultures. Around the year 550 CE, a continuous decrease in urban population and selective building destruction was noted, accompanied by widespread fire. The layout of the city is identified by an avenue tha…
The AD 1755 Lisbon Earthquake-Tsunami: Seismic source modelling from the analysis of ESI-07 environmental data
This work presents a macroseismic analysis of the AD 1755 Lisbon Earthquake-Tsunami event by means of the combination of intensity data derived from the EMS-98 scale and the ESI-07 scale (Environmental damage). About 600 records of secondary earthquake environmental effects (EEEs) for the whole Spain have been used to define intensities, focused on the SW portion of the Iberian Peninsula. The Spanish data have been complemented with 308 EEEs reco…
Polygenetic sand volcanoes: On the features of liquefaction processes generated by a single event (2012 Emilia Romagna 5.9 Mw earthquake, Italy)
Archaeoseismological Analysis of a Late Bronze Age Site on the Alhama de Murcia Fault, SE Spain
An archaeoseismological study of Tira del Lienzo (Totana, Spain) was undertaken. The site belongs to the Argar archaeological group (2200–1550 cal. B.C.; Bronze Age). It is located on the trace of the reverse left‐lateral Alhama de Murcia fault (AMF) that was responsible for the 5.1 Mw 2011 Lorca earthquake. The constructive typology of the site consists of mortar‐free irregular natural boulders (dry‐set masonry) and differs from earlier archaeos…
Archaeoseismological Analysis of a Late Bronze Age Site on the Alhama de Murcia Fault, SE Spain
An archaeoseismological study of Tira del Lienzo (Totana, Spain) was undertaken. The site belongs to the Argar archaeological group (2200–1550 cal. B.C.; Bronze Age). It is located on the trace of the reverse left‐lateral Alhama de Murcia fault (AMF) that was responsible for the 5.1 Mw 2011 Lorca earthquake. The constructive typology of the site consists of mortar‐free irregular natural boulders (dry‐set masonry) and differs from earlier archaeos…
Polygenetic sand volcanoes: On the features of liquefaction processes generated by a single event (2012 Emilia Romagna 5.9 Mw earthquake, Italy)
Archaeoseismological Analysis of a Late Bronze Age Site on the Alhama de Murcia Fault, SE Spain
An archaeoseismological study of Tira del Lienzo (Totana, Spain) was undertaken. The site belongs to the Argar archaeological group (2200–1550 cal. B.C.; Bronze Age). It is located on the trace of the reverse left‐lateral Alhama de Murcia fault (AMF) that was responsible for the 5.1 Mw 2011 Lorca earthquake. The constructive typology of the site consists of mortar‐free irregular natural boulders (dry‐set masonry) and differs from earlier archaeos…
The AD 1755 Lisbon Earthquake-Tsunami: Seismic source modelling from the analysis of ESI-07 environmental data
This work presents a macroseismic analysis of the AD 1755 Lisbon Earthquake-Tsunami event by means of the combination of intensity data derived from the EMS-98 scale and the ESI-07 scale (Environmental damage). About 600 records of secondary earthquake environmental effects (EEEs) for the whole Spain have been used to define intensities, focused on the SW portion of the Iberian Peninsula. The Spanish data have been complemented with 308 EEEs reco…
Teotihuacan ancient culture affected by megathrust earthquakes during the early Epiclassic Period (Mexico)
Teotihuacan was one of the thriving cultures in the Mesoamerica pre-Hispanic times, located in the Central Valley of Mexico. The city-state was a dominant centre point during the Classic period and its influence affected other contemporaneous cultures. Around the year 550 CE, a continuous decrease in urban population and selective building destruction was noted, accompanied by widespread fire. The layout of the city is identified by an avenue tha…
Reply to comment by Suárez et al., did Teotihuacán collapse due to a major earthquake? On “Teotihuacan ancient culture affected by megathrust earthquakes during the early Epiclassic period (Mexico)”
earthquake and tectonic studies (4 works) · Geology (4 works) · Seismology (4 works) · Archaeology (3 works) · Geography (3 works) · Fault (geology (2 works) · Geological and Geochemical Analysis (2 works) · Geological and Geophysical Studies Worldwide (2 works) · Geomorphology (2 works) · Geotechnical engineering (2 works)