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Makran Subduction Zone crustal structure

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NIAID Data Ecosystem2026-03-13 收录
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Two complementary data sets are inverted to obtain the on-shore Makran Subduction Zone crustal structure. The first (JB022942.prfdata.tgz) consist of P-wave receiver function. The receiver functions files are in SAC format. Information on the individual waveforms are contained in the header of the SAC files. The second (JB022942.rwgvdata.tgz) consists of pseudo-dispersion curves for each of the site formatted for input to the SURF96 code of Herrmann [2013]. References Ahmadzadeh-Irandoust, M., K. Priestley, and F. Sobouti (2022), Crustal structure of the Iranian Plateau, to be submitted to Geochemistry, Geophysics, Geosystems, in preparation. Herrmann, R. B. (2013), Computer programs in seismology: An evolving tool for instruction and research, Seismological Research Letters, 84(6), 1081–1088. Ligorria, J. P., and C. J. Ammon (1999), Iterative Deconvolution and Receiver-Function Estimation, October, 89(5), 1395–1400.
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2021-11-29
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