Near-surface folding along an active fault: seismic or aseismic?
- 1 July 1998
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 292 (3-4) , 279-291
- https://doi.org/10.1016/s0040-1951(98)00074-2
Abstract
No abstract availableThis publication has 23 references indexed in Scilit:
- SOIL-PORE AND PARTICLE ORIENTATIONS CAUSED BY ACTIVE FAULTING: A MICROMORPHOLOGICAL PERSPECTIVESoil Science, 1998
- How did the Meers fault scarp form? Paleoearthquake or aseismic creep?Engineering Geology, 1997
- Style and timing of Holocene surface faulting on the Meers fault, southwestern OklahomaGSA Bulletin, 1990
- COCORP profiling across the Southern Oklahoma aulacogen: Overthrusting of the Wichita Mountains and compression within the Anadarko BasinGeology, 1983
- Steady-State Flow in Marble at 500° to 800°CGSA Bulletin, 1972
- Hydrolytic Weakening of Quartz and Other Silicates*Geophysical Journal of the Royal Astronomical Society, 1967
- Effect of Large Changes in Strain Rate in the Experimental Deformation of Yule MarbleThe Journal of Geology, 1963
- Chapter 4: Deformation of Rocks at 500° to 800° C.Published by Geological Society of America ,1960
- Chapter 13: Observations on Fracture and a Hypothesis of EarthquakesPublished by Geological Society of America ,1960
- Chapter 7: Transition from Brittle Fracture to Ductile Flow in Solenhofen Limestone as a Function of Temperature, Confining Pressure, and Interstitial Fluid PressurePublished by Geological Society of America ,1960