scholarly article | Q13442814 |
P819 | ADS bibcode | 2005GeoRL..3210311A |
P356 | DOI | 10.1029/2004GL022256 |
P2093 | author name string | Andrea Antonioli | |
P2860 | cites work | Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents | Q56997724 |
Aftershocks driven by a high-pressure CO2 source at depth | Q57123913 | ||
Aftershocks caused by pore fluid flow? | Q57140418 | ||
Static stress changes and fault interaction during the 1997 Umbria-Marche earthquake sequence | Q57858794 | ||
Complex Normal Faulting in the Apennines Thrust-and-Fold Belt: The 1997 Seismic Sequence in Central Italy | Q58457850 | ||
Aftershocks and pore fluid diffusion following the 1992 Landers earthquake | Q99215827 | ||
P433 | issue | 10 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | fluid flow | Q12142910 |
Italy | Q38 | ||
P577 | publication date | 2005-01-01 | |
P1433 | published in | Geophysical Research Letters | Q5535576 |
P1476 | title | Fluid flow and seismicity pattern: Evidence from the 1997 Umbria-Marche (central Italy) seismic sequence | |
P478 | volume | 32 |
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Q64067857 | Clock advance and magnitude limitation through fault interaction: the case of the 2016 central Italy earthquake sequence |
Q60706741 | First observations of non-volcanic, long-period seismicity in the central Apennines, Italy |
Q59761797 | Modeling seismicity rate changes during the 1997 Umbria-Marche sequence (central Italy) through a rate- and state-dependent model |
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