Decoding the state of stress and fluid pathways along the Andean Southern Volcanic Zone
N Pérez-Estay, J Ruz-Ginouves… - … Earth & Environment, 2023 - nature.com
Decoding means decrypting a hidden message. Here, the encrypted messages are the state
of stress, fluid pathways, and volcano tectonic processes occurring in volcanoes of the …
of stress, fluid pathways, and volcano tectonic processes occurring in volcanoes of the …
The geodynamic setting and geological context of Merapi volcano in Central Java, Indonesia
Abstract Mount (Mt.) Merapi is a Quaternary stratovolcano situated on the active volcanic
front in Central Java. It is a part of the active volcanic arc chain of Java Island formed by the …
front in Central Java. It is a part of the active volcanic arc chain of Java Island formed by the …
Geomorphological classification of monogenetic volcanoes and its implication to tectonic stress orientation in the Middle Atlas Volcanic Field (Morocco)
M Benamrane, K Németh, M Jadid, EH Talbi - Land, 2022 - mdpi.com
The Middle Atlas Volcanic Field (MAVF) covers an area of 1500 km2, with a total erupted
volume of solid products (eg, Dense Rock Equivalent or DRE) estimated to be more than 80 …
volume of solid products (eg, Dense Rock Equivalent or DRE) estimated to be more than 80 …
Sensitivity assessment of morphometric parameters of monogenetic volcanic landforms with global free DEMs
Improvements in the resolution of Digital Elevation Model (DEM) have greatly facilitated the
research of small to moderate landforms such as dunes, landslides/rockfalls …
research of small to moderate landforms such as dunes, landslides/rockfalls …
Seismic imaging of lithospheric structure beneath Central-East Java region, Indonesia: relation to recent earthquakes
The Central and East Java region, which is part of the Sunda Arc, has an important role in
producing destructive earthquakes and volcanic complexes in Indonesia as a result of the …
producing destructive earthquakes and volcanic complexes in Indonesia as a result of the …
Geostatistical multitemporal InSAR method and elastic deformation model for detailed characterizations of topographic change and magma reservoirs: Application to …
This study proposes the entire detection of the surface deformation of a volcanic area using
interferometric synthetic aperture radar (InSAR) with geostatistics to specify the locations …
interferometric synthetic aperture radar (InSAR) with geostatistics to specify the locations …
[HTML][HTML] Rift obliquity in the Northern Volcanic Zone in Iceland using UAV-based structural data
Rift obliquity is known to be very frequent at divergent plate boundaries and shear
components in the opening of fissures have been detected through seismicity in the …
components in the opening of fissures have been detected through seismicity in the …
[HTML][HTML] Morphological analysis of volcanic cones and its implication to Quaternary tectonics of the Jeju Island (South Korea)
The morphological characteristics and distribution of volcanic cones of Jeju Island in Korea
could be controlled by several factors, including stress field in the substrate and subsurface …
could be controlled by several factors, including stress field in the substrate and subsurface …
Tectonic controls on geomorphology and spatial distribution of monogenetic volcanoes in the Central Southern Volcanic Zone of the Andes (Argentina)
Monogenetic volcanoes are among the most common volcanic landforms on Earth. The
morphology and distribution of small volcanoes can provide important information about …
morphology and distribution of small volcanoes can provide important information about …
The growth of polygenetic volcanoes in the laboratory: Control of eruptive volume and magma viscosity on edifice development and morphology
H Andikagumi, CB de Maisonneuve, B Taisne - Geomorphology, 2023 - Elsevier
Morphometric parameters have been used to describe and classify the shape of volcanic
edifices, but the processes that control these parameters are not fully understood. Here we …
edifices, but the processes that control these parameters are not fully understood. Here we …