FOUR EARTHQUAKES OF THE SUMATRAN FAULT ZONE (MW 6.0-6.4): SOURCE PARAMETERS AND IDENTIFICATION OF THE ACTIVATED FAULT PLANES

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

MADLAZIM -; SANTOSA B.J.

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: Journal of Seismology and Earthquake Engineering Year:2010 | Volume:11 | Issue:4 Page(s): 159-169

Download Full-Text

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

View:

758

Download:

159

Cites:

Information Journal Paper

Title

FOUR EARTHQUAKES OF THE SUMATRAN FAULT ZONE (MW 6.0-6.4): SOURCE PARAMETERS AND IDENTIFICATION OF THE ACTIVATED FAULT PLANES

Author(s)

MADLAZIM - | SANTOSA B.J. | Issue Writer Certificate

Keywords

SUMATRAN FAULT ZONEQ4

3-COMPONENT LOCAL WAVEFORM INVERSIONQ4

SOURCE PARAMETERS AND FAULT PLANEQ4

Abstract

Four earthquakes (Mw 6.0-6.4) which occurred at 3 major segments of SUMATRAN FAULT ZONE (SFZ) were analyzed to identify their fault planes. The events were relocated to assess physical insight into the hypocenter uncertainty. The earthquake source parameters were determined from three-component local waveforms recorded by IRIS-DMC and Geofon broadband IA networks. The epicentral distances of all stations were less than 10o. Moment tensor solutions of the events was performed, simultaneously with the determination of the centroid position. Joint analysis of the hypocenter position, centroid position and nodal planes of the events indicated the Sumatra fault planes. The hypocenters of all four events clearly prefer that strikes parallel to Sumatra Island to be the fault plane in all cases. Regional moment tensor solutions of this paper along with the focal mechanisms, which represent the only double couple of moment tensor, is plotted. The MT solutions consist of all events have strike slip one fault type. The preferable seismotectonic interpretation is that the events activated Sumatra fault zone at a depth of about 14-18 km, corresponding to the interplate of Sumatra fault boundary.

Cites

No record.

References

No record.

Cite

APA: Copy

MADLAZIM, -, & SANTOSA, B.J.. (2010). FOUR EARTHQUAKES OF THE SUMATRAN FAULT ZONE (MW 6.0-6.4): SOURCE PARAMETERS AND IDENTIFICATION OF THE ACTIVATED FAULT PLANES. JOURNAL OF SEISMOLOGY AND EARTHQUAKE ENGINEERING, 11(4), 159-169. SID. https://sid.ir/paper/112350/en

Vancouver: Copy

MADLAZIM -, SANTOSA B.J.. FOUR EARTHQUAKES OF THE SUMATRAN FAULT ZONE (MW 6.0-6.4): SOURCE PARAMETERS AND IDENTIFICATION OF THE ACTIVATED FAULT PLANES. JOURNAL OF SEISMOLOGY AND EARTHQUAKE ENGINEERING[Internet]. 2010;11(4):159-169. Available from: https://sid.ir/paper/112350/en

IEEE: Copy

- MADLAZIM, and B.J. SANTOSA, “FOUR EARTHQUAKES OF THE SUMATRAN FAULT ZONE (MW 6.0-6.4): SOURCE PARAMETERS AND IDENTIFICATION OF THE ACTIVATED FAULT PLANES,” JOURNAL OF SEISMOLOGY AND EARTHQUAKE ENGINEERING, vol. 11, no. 4, pp. 159–169, 2010, [Online]. Available: https://sid.ir/paper/112350/en

Related Journal Papers