CRUSTAL VELOCITY STRUCTURE OF NORTH-EAST OF CENTRAL IRAN AND BINALUD ZONE, USING TELESEISMIC RECEIVER FUNCTIONS

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JAVAN DOULOUEI GH.; NOUROUZI GH.R.; GHAFOURI ASHTIANI M.

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Journal: Journal of the Earth and Space Physics Year:2007 | Volume:33 | Issue:1 Page(s): 119-134

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Title

CRUSTAL VELOCITY STRUCTURE OF NORTH-EAST OF CENTRAL IRAN AND BINALUD ZONE, USING TELESEISMIC RECEIVER FUNCTIONS

Author(s)

JAVAN DOULOUEI GH. | NOUROUZI GH.R. | GHAFOURI ASHTIANI M. | Issue Writer Certificate

Keywords

EAST OF IRANQ3

SABZAVARQ3

NORTHQ3

TAKNAR ZONEQ4

BINALUD ZONEQ3

CRUSTAL VELOCITY STRUCTUREQ3

RECEIVER FUNCTIONSQ3

Abstract

The crustal structure beneath 9 seismic stations, deployed in NORTH-EAST OF IRAN is determined using RECEIVER FUNCTIONS analysis. In this study, 4 stations in the SABZAVAR-Taknar zone and 5 stations in the BINALUD ZONE with more than 40 teleseismic earthquakes are used to calculate RECEIVER FUNCTIONS. A crustal structure is suggested for the SABZAVAR-Taknar zone with a Moho depth of 46-48km, results present the three main layers: The upper crust has a S wave velocity between 1.9-3.1 km/s and a 11 km thickness. The middle crust has S wave velocity between 3.0-3.5 km/s and an 18 km thickness. The lower crust has S wave velocity between 3.6-4.6 km/s and an 18 km thickness. The crustal structure that is suggested for the Binalud, is a Moho depth of 48-50 km and three main layers for crust: The upper crust has a S wave velocity between 2.4-3.3 km/s and a 10 km thickness. The middle crust has S wave velocity between 3.0-3.5 km/s and a 22 km thickness. The lower crust has S wave velocity between 3.6-4.6 km/s and a 17 km thickness.

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APA: Copy

JAVAN DOULOUEI, GH., NOUROUZI, GH.R., & GHAFOURI ASHTIANI, M.. (2007). CRUSTAL VELOCITY STRUCTURE OF NORTH-EAST OF CENTRAL IRAN AND BINALUD ZONE, USING TELESEISMIC RECEIVER FUNCTIONS. JOURNAL OF THE EARTH AND SPACE PHYSICS, 33(1), 119-134. SID. https://sid.ir/paper/80480/en

Vancouver: Copy

JAVAN DOULOUEI GH., NOUROUZI GH.R., GHAFOURI ASHTIANI M.. CRUSTAL VELOCITY STRUCTURE OF NORTH-EAST OF CENTRAL IRAN AND BINALUD ZONE, USING TELESEISMIC RECEIVER FUNCTIONS. JOURNAL OF THE EARTH AND SPACE PHYSICS[Internet]. 2007;33(1):119-134. Available from: https://sid.ir/paper/80480/en

IEEE: Copy

GH. JAVAN DOULOUEI, GH.R. NOUROUZI, and M. GHAFOURI ASHTIANI, “CRUSTAL VELOCITY STRUCTURE OF NORTH-EAST OF CENTRAL IRAN AND BINALUD ZONE, USING TELESEISMIC RECEIVER FUNCTIONS,” JOURNAL OF THE EARTH AND SPACE PHYSICS, vol. 33, no. 1, pp. 119–134, 2007, [Online]. Available: https://sid.ir/paper/80480/en

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