Results 191 to 200 of about 7,697 (265)
Abstract Constraining peak temperature during seismic slip is essential for quantifying earthquake energy budgets and fault weakening. Rock magnetic methods provide a sensitive means of estimating shear‐induced coseismic temperature rise; however, the role of fluids in friction‐induced magnetic alterations remains poorly constrained.
Qiang Fu +6 more
wiley +1 more source
Tilt measurements in the underground laboratory Lohja 2, Finland, in 1977-1987
Ruotsalainen, Hannu +1 more
core
Abstract The Tangra Yumco Rift (TYR) in central Tibet is a key window for crust–mantle interactions during extension. We performed high‐resolution crust‐mantle imaging using receiver function analysis, 1‐D nonlinear S‐wave velocity inversion, and tomoDD tomography, revealing a vertical Crust–Mantle Degassing System (CMDS) bounded by the Zhala (ZF) and ...
Zongxu Li +8 more
wiley +1 more source
Measurements of Gravity Tides along the ''Blue Road Geotraverse'' in Fennoscandia
Asch, G. +4 more
core
Abstract The observed inter‐annual variability of Global Dust Events (GDE) occurrence on Mars remains challenging to understand and therefore to predict. Several hypotheses have been investigated so far, but a central aspect seems to be missing: How the heterogeneity of the surface dust cover and regolith particle size distributions relate to regional ...
Demetrius Ramette +3 more
wiley +1 more source
Observation results. Angle measurements in 1964-65, 1971, 1984 and 1986-87
Konttinen, Raimo
core
Abstract As the climate warms, associated changes in ocean dynamics will redistribute sea‐water mass within the ocean, contributing to relative sea‐level change. This mass redistribution will cause additional sea‐level changes due to gravitational self‐attraction, deformation of the solid Earth, and shifts in the Earth's rotation axis (GRD), which are ...
Grace Ertel +3 more
wiley +1 more source
High precision measurements for studying the secular variation in gravity in Finland
Kiviniemi, Aimo
core
Sulfur Exposure for Airplane Passengers From Stratospheric Aerosol Injection
Abstract Injection of sulfur dioxide to create a stratospheric sulfate aerosol cloud is the most studied method of climate intervention. It has been suggested that airplanes be used at high latitudes to create such a cloud at lower altitudes. Commercial airplanes routinely fly at altitudes of 11 km in the Arctic, and therefore passengers could be ...
Alan Robock +3 more
wiley +1 more source
Geodetic measurements at the Pasmajärvi and Nuottavaara faults
Ruotsalainen, Hannu +4 more
core

