SEISMIC IMAGING OF SEA-BED SEDIMENTS USING VERTICAL-CABLE METHOD

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.

BABAEI L.; SIAHKOUHI H.R.

Educational Videos and Scientific Workshops

Scientific Information Database

ISSN: 2588-4824

Journal Paper

Paper Information

Journal: Journal of the Earth and Space Physics Year:2006 | Volume:32 | Issue:2 Page(s): 57-69

Download Full-Text

Persian Verion

View:

763

Download:

Cites:

Information Journal Paper

Title

SEISMIC IMAGING OF SEA-BED SEDIMENTS USING VERTICAL-CABLE METHOD

Author(s)

BABAEI L. | SIAHKOUHI H.R. | Issue Writer Certificate

Keywords

ANISOTROPYQ3

MARINE SEISMICQ3

SEA-BED SEDIMENTQ3

VERTICAL-CABLE METHODQ3

Abstract

In MARINE SEISMIC surveys amplitudes, frequency contents and travel times of seismic waves are influenced significantly by elastic and physical properties of .sea-bed sediments. Therefore, investigation of elastic properties of propagation medium at the bottom of the sea floor is worth while in MARINE SEISMIC studies.In this paper refraction arrival times are analyzed to estimate the velocity structure and anisotropic parameters of SEA-BED SEDIMENTs using a vertical-cable (VC) configuration. Two sets of synthetic seismic data from two distinct earth models were used to evaluate the influence of dip and ANISOTROPY of layers on propagation of seismic waves. In the first set of data, for a constant value of ANISOTROPY, the values of 00, 50 and 100 were assigned to dip in order to evaluate the influences of dip. However, in the second set of models, we kept the dip constant and varied the P-wave ANISOTROPY strength of the medium to examine the sensitivity of ray-slowness to ANISOTROPY. All above mentioned analyses were done on synthetic P-wave VC seismic records, which were obtained by solving of eikonal equation using finite-difference method. Our result indicated the usefulness of the VC acquisition method for determination of real dip (b), dip azimuth jd azimuth of symmetry axis with respect to the X-axis ja and anisotropic parameters (v P0, e) of the saturated SEA-BED SEDIMENTs.

Cites

No record.

References

No record.

Cite

APA: Copy

BABAEI, L., & SIAHKOUHI, H.R.. (2006). SEISMIC IMAGING OF SEA-BED SEDIMENTS USING VERTICAL-CABLE METHOD. JOURNAL OF THE EARTH AND SPACE PHYSICS, 32(2), 57-69. SID. https://sid.ir/paper/80344/en

Vancouver: Copy

BABAEI L., SIAHKOUHI H.R.. SEISMIC IMAGING OF SEA-BED SEDIMENTS USING VERTICAL-CABLE METHOD. JOURNAL OF THE EARTH AND SPACE PHYSICS[Internet]. 2006;32(2):57-69. Available from: https://sid.ir/paper/80344/en

IEEE: Copy

L. BABAEI, and H.R. SIAHKOUHI, “SEISMIC IMAGING OF SEA-BED SEDIMENTS USING VERTICAL-CABLE METHOD,” JOURNAL OF THE EARTH AND SPACE PHYSICS, vol. 32, no. 2, pp. 57–69, 2006, [Online]. Available: https://sid.ir/paper/80344/en

Related Journal Papers

Related Seminar Papers

No record.

Related Plans

No record.

Recommended Workshops

File Not Exists.

Move to top

وبگردی