Large-scale aseismic creep in the areas of the strong earthquakes revealed from the GRACE data on the time variations of the Earth’s gravity field

• Published in: Izvestiya. Physics of the solid earth Vol. 52; no. 5; pp. 692 - 703
• Main Authors: Mikhailov, V. O., Diament, M., Lyubushin, A. A., Timoshkina, E. P., Khairetdinov, S. A.
• Format: Journal Article
• Language: English
• Published: Moscow Pleiades Publishing 01.09.2016; Springer Nature B.V
• Subjects: Average velocity; Creep (materials); Disasters; Earth and Environmental Science; Earth Sciences; Earthquakes; Fault lines; Geophysics/Geodesy; Global positioning systems; GPS; GRACE (experiment); Gravitation; Gravitational fields; Gravity; Gravity anomalies; Islands; Marine; Seismic activity; Seismology; Subduction (geology); INW, Japan, Hokkaido; ISW, Indian Ocean; ISW, East Indian Ocean, Wharton Basin; ISE, Chile; ISE, Pacific, Samoa; INW, Japan, Honshu, Miyagi Prefect., Tohoku
• ISSN: 1069-3513; 1555-6506
• DOI: 10.1134/S1069351316040054

The refinement of the accuracy and resolution of the monthly global gravity field models from the GRACE satellite mission, together with the accumulation of more than a decade-long series of these models, enabled us to reveal the processes that occur in the regions of large ( M w ≥8) earthquakes that have not been studied previously. The previous research into the time variations of the gravity field in the regions of the giant earthquakes, such as the seismic catastrophes in Sumatra (2004) and Chile (2010), and the Tohoku mega earthquake in Japan (2011), covered the coseismic gravity jump followed by the long postseismic changes reaching almost the same amplitude. The coseismic gravity jumps resulting from the lower-magnitude events are almost unnoticeable. However, we have established a long steady growth of gravity anomalies after a number of such earthquakes. For instance, in the regions of the subduction earthquakes, the growth of the positive gravity anomaly above the oceanic trench was revealed after two events with magnitudes M w =8.5 in the Sumatra region (the Nias earthquake of March 2005 and the Bengkulu event of September 2007 near the southern termination of Sumatra Island), after the earthquake with M w =8.5 on Hokkaido in September 2007, a doublet Simushir earthquake with the magnitudes M w = 8.3 and 8.1 in the Kuriles in November 2006 and January 2007, and after the earthquake off the Samoa Island in September 2009 ( M w =8.1). The steady changes in the gravity field have also been recorded after the earthquake in the Sichuan region (May 2008, M w = 8.0) and after the doublet event with magnitudes 8.6 and 8.2, which occurred in the Wharton Basin of the Indian Ocean on April 11, 2012. The detailed analysis of the growth of the positive anomaly in gravity after the Simushir earthquake of November 2006 is presented. The growth started a few months after the event synchronously with the seismic activation on the downdip extension of the coseismically ruptured fault plane zone. The data demonstrating the increasing depth of the aftershocks since March 2007 and the approximately simultaneous change in the direction and average velocity of the horizontal surface displacements at the sites of the regional GPS network indicate that this earthquake induced postseismic displacements in a huge area extending to depths below 100 km. The total displacement since the beginning of the growth of the gravity anomaly up to July 2012 is estimated at 3.0 m in the upper part of the plate’s contact and 1.5 m in the lower part up to a depth of 100 km. With allowance for the size of the region captured by the deformations, the released total energy is equivalent to the earthquake with the magnitude M w = 8.5. In our opinion, the growth of the gravity anomaly in these regions indicates a large-scale aseismic creep over the areas much more extensive than the source zone of the earthquake. These processes have not been previously revealed by the ground-based techniques. Hence, the time series of the GRACE gravity models are an important source of the new data about the locations and evolution of the locked segments of the subduction zones and their seismic potential.