In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 47, No. 3 ( 2020-02-16)
Kurzfassung:
Behavior of directly monitored high‐pressure pulses indicates nonlinear diffusion induced by fracture dilation High fracture fluid pressure signals change direction during stimulation and are associated with seismic and aseismic deformation Seismohydromechanical monitoring indicates a combination of Mode I and II/III deformation during high‐pressure fluid injections
Materialart:
Online-Ressource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2019GL086135
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2020
ZDB Id:
2021599-X
ZDB Id:
7403-2
SSG:
16,13