Miguel Angel Rodríguez-Pascua
Biographic Data
| ID | 2001010 |
|---|---|
| NAME | Miguel Angel Rodríguez-Pascua |
| GIVEN NAMES | Miguel Angel |
| FAMILY NAME | Rodríguez-Pascua |
| SIGNATURE | RODRÍGUEZ-PASCUA M A |
| AFFILIATIONS | Instituto Geológico y Minero de España |
| ORCID | 0000-0001-5174-119X |
| VERIFIED | Yes |
| TOTAL WORKS | 11 |
| TOTAL CITATIONS | 2 |
| AUTHOR COUNT | 11 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2010 |
| 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)”
Prehistoric Evidence of Crustal Earthquakes and Debris Flow in Archaeological Site of Pikillaqta in Cusco: Archaeological Implications
In the Cusco Valley, seismic activity resulted from reactivations of the Qoricocha, Tambomachay, and Pachatusan faults in 1986, 1950, and 1650 during the Inca and Wari cultures' settlement. However, the pre‐1650 seismic record is scant, with few chroniclers mentioning Inca‐era earthquakes lacking precise information. Filling this void, our study centers on paleoseismological and archaeoseismological research in the Cusco Valley, emphasizing the P…
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…
Análisis arqueosísmico del monumento de Pozo Moro: Lo derrumbó un terremoto
Análisis arqueosísmico del monumento de Pozo Moro, situado en Chinchilla de Montearagón, Albacete, actualmente conservado en el Museo Arqueológico Nacional. Los resultados obtenidos indican que este monumento turriforme de casi 10 m de altura, construido con sillares hacia el 500 a.C., fue destruido pocos años después por un terremoto, según parecía indicar cierta deformación del terreno y la posición de caída de los sillares hallados en la excav…
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…
Miocene to present-day tectonic control on the relief of the Duero and Ebro basins confluence (North Iberia)
This article presents a morpho-structural map at 1:50,000 scale of the confluence area between three regional units: (1) the Burgalesa Platform (Mesozoic; Cantabrian Mountains), (2) the Duero Basin and (3) the Ebro Basin (Cenozoic foreland basins). The map covers an area of 527 km2 in north Iberia. Additionally, structural lineaments such as joints are well preserved and documented in the Upper Cretaceous sediments of the Burgalesa Platform, repr…
Natural disasters written in historical woods: Floods, a thunderbolt fire and an earthquake
Estimation of the epicentral area of the 1912 Acambay earthquake (M 6.9, Mexico) determined from the earthquake archaeological effects (EAE) and the ESI07 macroseismic scale
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…
Palaeoenvironmental significance of diatom and vertebrate fossils from Late Cenozoic tectonic basins in west-central México: A review
Natural disasters written in historical woods: Floods, a thunderbolt fire and an earthquake
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…
Palaeoenvironmental significance of diatom and vertebrate fossils from Late Cenozoic tectonic basins in west-central México: A review
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…
Estimation of the epicentral area of the 1912 Acambay earthquake (M 6.9, Mexico) determined from the earthquake archaeological effects (EAE) and the ESI07 macroseismic scale
Natural disasters written in historical woods: Floods, a thunderbolt fire and an earthquake
Miocene to present-day tectonic control on the relief of the Duero and Ebro basins confluence (North Iberia)
This article presents a morpho-structural map at 1:50,000 scale of the confluence area between three regional units: (1) the Burgalesa Platform (Mesozoic; Cantabrian Mountains), (2) the Duero Basin and (3) the Ebro Basin (Cenozoic foreland basins). The map covers an area of 527 km2 in north Iberia. Additionally, structural lineaments such as joints are well preserved and documented in the Upper Cretaceous sediments of the Burgalesa Platform, repr…
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…
Análisis arqueosísmico del monumento de Pozo Moro: Lo derrumbó un terremoto
Análisis arqueosísmico del monumento de Pozo Moro, situado en Chinchilla de Montearagón, Albacete, actualmente conservado en el Museo Arqueológico Nacional. Los resultados obtenidos indican que este monumento turriforme de casi 10 m de altura, construido con sillares hacia el 500 a.C., fue destruido pocos años después por un terremoto, según parecía indicar cierta deformación del terreno y la posición de caída de los sillares hallados en la excav…
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)”
Prehistoric Evidence of Crustal Earthquakes and Debris Flow in Archaeological Site of Pikillaqta in Cusco: Archaeological Implications
In the Cusco Valley, seismic activity resulted from reactivations of the Qoricocha, Tambomachay, and Pachatusan faults in 1986, 1950, and 1650 during the Inca and Wari cultures' settlement. However, the pre‐1650 seismic record is scant, with few chroniclers mentioning Inca‐era earthquakes lacking precise information. Filling this void, our study centers on paleoseismological and archaeoseismological research in the Cusco Valley, emphasizing the P…
Geology (9 works) · earthquake and tectonic studies (5 works) · Seismology (5 works) · Archaeology (4 works) · Geography (4 works) · Geological and Geophysical Studies Worldwide (4 works) · Art (3 works) · Geology and Paleoclimatology Research (3 works) · Geomorphology (3 works) · Paleontology (3 works)