ExLibris header image
SFX Logo
Title: Seismogenic faulting of the sedimentary sequence and laterally variable material properties in the Zagros Mountains (Iran) revealed by the August 2014 Murmuri (E. Dehloran) earthquake sequence
Source:

Geophysical Journal International [0956-540X] Copley, A yr:2015


Collapse list of basic services Basic
Sorry, no full text available...
Please use the document delivery service (see below)  
Holding information
Holdings in library search engine ALBERT GO
Document delivery
Request document via Library/Bibliothek GO
Users interested in this article also expressed an interest in the following:
1. Barnhart, William D. "Phantom earthquakes and triggered aseismic creep: Vertical partitioning of strain during earthquake sequences in Iran." Geophysical research letters 40.5 (2013): 819-823. Link to Full Text for this item Link to SFX for this item
2. Barnhart, William D. "Active accommodation of plate convergence in Southern Iran: Earthquake locations, triggered aseismic slip, and regional strain rates." Journal of Geophysical Research: Solid Earth 118.10 (2013): 5699-5711. Link to Full Text for this item Link to SFX for this item
3. Delahaye, E.J., E.J. J. "Microseismicity but no tremor accompanying slow slip in the Hikurangi subduction zone, New Zealand." Earth and planetary science letters 277.1/2 (2009): 21-28. Link to SFX for this item
4. Castagna, J. P. P. "Relationships between compressional-wave and shear-wave velocities in clastic silicate rocks." The leading edge 50.4 (1985): 571-581. Link to Full Text for this item Link to SFX for this item
5. Ballato, P. "Accommodation of transpressional strain in the Arabia‐Eurasia collision zone: new constraints from (U‐Th)/He thermochronology in the Alborz mountains, north Iran." Tectonics 32.1 (2012): 1-18. Link to Full Text for this item Link to SFX for this item
6. Walker, Richard T. "Geomorphic evidence for ancestral drainage patterns in the Zagros Simple Folded Zone and growth of the Iranian plateau." Geological magazine 148.5-6 (2011): 901-910. Link to Full Text for this item Link to SFX for this item
7. Wallace, Laura M. "Characterizing the seismogenic zone of a major plate boundary subduction thrust: Hikurangi Margin, New Zealand." Geochemistry, geophysics, geosystems 10.10 (2009). Link to Full Text for this item Link to SFX for this item
8. Greve, S.M. M. "Strong variations in seismic anisotropy across the Hikurangi subduction zone, North Island, New Zealand." Tectonophysics 462.1-4 (2008): 7-21. Link to SFX for this item
9. Prasad. "Velocity to porosity transform in marine sediments." Petrophysics 42.5 (2001): 429-437. Link to Full Text for this item Link to SFX for this item
10. Roland, E. "Earthquake swarms on transform faults." Geophysical journal international 178.3 (2009): 1677-1690. Link to SFX for this item
11. GERCEK, H. "Poisson's ratio values for rocks." International journal of rock mechanics and mining sciences & geomechanics abstracts 44.1 (2007): 1-13. Link to SFX for this item
12. Gassmann, F. "Elastic waves through a packing of spheres." The leading edge 16.4 (1951): 673-685. Link to SFX for this item
13. Fagereng, A.. "On factors controlling the depth of interseismic coupling on the Hikurangi subduction interface, New Zealand." Earth and planetary science letters 278.1-2 (2009): 120-130. Link to SFX for this item
14. Backus, GE E. "Long-Wave Elastic Anisotropy Produced by Horizontal Layering." Journal of geophysical research 67.11 (1962): 4427-4440. Link to Full Text for this item Link to SFX for this item
15. Ito, Y. "Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events." Science 315.5811 (2006): 503-506. Link to SFX for this item
16. Gardner, GHF F. "FORMATION VELOCITY AND DENSITY—THE DIAGNOSTIC BASICS FOR STRATIGRAPHIC TRAPS." The leading edge 39.6 (1974): 770-780. Link to SFX for this item
View More...
View Less...
Select All Clear All

Expand list of advanced services Advanced
A service provided by the Library of the Wissenschaftspark Albert Einstein, Potsdam, Germany.
© 2005 SFX by Ex Libris Inc.