Simpson RW (1997) Quantifying Anderson’s fault types. Scholz CH (2002) The mechanics of earthquakes and faulting. In: Lee WHK, Kanamori H, Jennings PC, Kisslinger C (eds) International handbook of earthquake and engineering seismology. Ruff LJ (2002) State of stress within the earth. Michael AJ (1987) Use of focal mechanisms to determine stress: a control study. Michael AJ (1984) Determination of stress from slip data: faults and folds. Tools for seismic analysis in porous media. Mavko G, Mukerji T, Dvorkin J (2009) The rock physics handbook. Maury J, Cornet FH, Dorbath L (2013) A review of methods for determining stress fields from earthquake focal mechanisms: application to the Sierentz 1980 seismic crisis (Upper Rhine graben). Martínez-Garzón P, Bohnhoff M, Kwiatek G, Dresen G (2013) Stress tensor changes related to fluid injection at The Geysers geothermal field, California. Lund B, Slunga R (1999) Stress tensor inversion using detailed microearthquake information and stability constraints: application to Ölfus in southwest Iceland. Lay T, Wallace TC (1995) Modern global seismology. Julian BR, Miller AD, Foulger GR (1998) Non-double-couple earthquakes. Jaeger JC, Cook NGW, Zimmerman RW (2007) Fundamentals of rock mechanics, 4th edn. Ickrath M, Bohnhoff M, Bulut F, Dresen G (2014) Stress rotation and recovery in conjunction with the 1999 Izmit Mw 7.4 earthquake. Heidbach O, Tingay M, Barth A, Reinecker J, Kurfeß D, Müller B (2008) The world stress map database release 2008. Hardebeck JL, Michael AJ (2006) Damped regional-scale stress inversions: methodology and examples for southern California and the Coalinga aftershock sequence. Hardebeck JL (2006) Homogeneity of small-scale earthquakes faulting, stress, and fault strength. Gephart JW, Forsyth DW (1984) An improved method for determining the regional stress tensor using earthquake focal mechanism data: application to the San Fernando earthquake sequence. Pure Appl Geophys 116:615–626įischer T, Guest A (2011) Shear and tensile earthquakes caused by fluid injection. Geophys J Int 150:588–609īott MHP (1959) The mechanics of oblique slip faulting. Oliver & Boyd, EdinburghĪngelier J (2002) Inversion of earthquake focal mechanisms to obtain the seismotectonic stress IV – a new method free of choice among nodal lines. * Although dust and splash resistant structure allows the lens to be used in light rain, it is not the same as being waterproof.Anderson EM (1951) The dynamics of faulting. * This product is developed, manufactured and sold based on the specifications of E-mount which was disclosed by Sony Corporation under the license agreement with Sony Corporation. * L-Mount is a registered trademark of Leica Camera AG. The degree to which light is refracted by glass depends on the light's waveleng… The super multi-layer coating is combined with SIGMA’s unique coating technolog… The polygonal shape of a conventional iris dia phragm causes out-of-focus light… The zoom lock switch fixes the zoom ring at the widest end, preventing it from … The AFL button can be assigned with various functions widens the range of opera… Incorporates a water and oil-repellent coating that allows water to be wiped aw… The brass mount combines high precision with rugged construction. High-precision, rugged brass bayonet mount.Matching the optical characteristics of the lens, this function performs in-cam… Compatible with Lens Aberration Correction.This lens features a highly effective dust and splash resistant structure with … A focus movement method of interchangeable lenses for mirrorless cameras (DN le…
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