| Citation: |
CHEN PEISHANup, HU RUIHUAup2, ZHOU KUNGENup3, LI WENXIANGuploans.com sh advancelucashadv. 1984: HOMOGENEOUS MAGNITUDE SYSTEM OF THE MAINLAND CHINA. Acta Seismologica Sinica, 6(4): 369-394.
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[1] Nuttli, O. W., G. A. Bollinger, and D. W. Griffiths, on the relation between modified Mercalli intensity and body——wave magnitude, Bull. Seism. Soc. Am., 69, 893——909, 1979.
[2] Christoskov, L, N. V. Kondorskaya, and J. Vanek, Homogeneous magnitude system of the Eura——sian Continent, Tectonophysics, 49, 131——138, 1978. [3] Christoskov, I. I. V. Fedorova, N. V. Kondorskaya, and J. Vanek, on a homogeneous system of selected Eurasian stations for magnitude determinations, Pure Appl. Geoplays. 112. 619——626, 1974. [4] Christoskov, L., N. V. Kondorskaya, J. Vanek, Homogeneous magnitude system of the Eurasian Continent, World Data Center A for Solid Earth Geophysics, Report 1979. [5] Kanamori, H. and G. Stewart, Mode of the strain release along the Gibbs fracture zone, Mid——Atlantic tidge, Phys. Earth Planet. Inter., 11, 312——332, 1976. [6] Gupta, H. K., and B. K. Kastogi, Earthquake u, h }——, 1!W relation and source multiplicity, Geophys.J. R. astr. Soc., 28, 65——89, 1972. [7] Duda, S. J., Physical significance of the earthquake magnitude——the present state of interpretation of the concept, Tectonophysics, 49, 3/4, 119——130, 1978. [8] Kanamori, H., and D. L. Anderson, Theoretical base of some empirical relations in seismology,Bull.. Seis. Soc. Am., 65, 5, 1073——1095, 1975. [9] 陈培善,分析地震波估算地壳内的应力值,地震学报,3, 3, 251——263, 1981, [10] 金严、陈培善,地震仪的暂态响应及其对地震波形的影响,地球物理学报,25,增刊,622——631,1982. [11] 维尔莫,p, L.地震观测业务手册,国家地震局地球物理研究所译,1979.
[1] Nuttli, O. W., G. A. Bollinger, and D. W. Griffiths, on the relation between modified Mercalli intensity and body——wave magnitude, Bull. Seism. Soc. Am., 69, 893——909, 1979.
[2] Christoskov, L, N. V. Kondorskaya, and J. Vanek, Homogeneous magnitude system of the Eura——sian Continent, Tectonophysics, 49, 131——138, 1978. [3] Christoskov, I. I. V. Fedorova, N. V. Kondorskaya, and J. Vanek, on a homogeneous system of selected Eurasian stations for magnitude determinations, Pure Appl. Geoplays. 112. 619——626, 1974. [4] Christoskov, L., N. V. Kondorskaya, J. Vanek, Homogeneous magnitude system of the Eurasian Continent, World Data Center A for Solid Earth Geophysics, Report 1979. [5] Kanamori, H. and G. Stewart, Mode of the strain release along the Gibbs fracture zone, Mid——Atlantic tidge, Phys. Earth Planet. Inter., 11, 312——332, 1976. [6] Gupta, H. K., and B. K. Kastogi, Earthquake u, h }——, 1!W relation and source multiplicity, Geophys.J. R. astr. Soc., 28, 65——89, 1972. [7] Duda, S. J., Physical significance of the earthquake magnitude——the present state of interpretation of the concept, Tectonophysics, 49, 3/4, 119——130, 1978. [8] Kanamori, H., and D. L. Anderson, Theoretical base of some empirical relations in seismology,Bull.. Seis. Soc. Am., 65, 5, 1073——1095, 1975. [9] 陈培善,分析地震波估算地壳内的应力值,地震学报,3, 3, 251——263, 1981, [10] 金严、陈培善,地震仪的暂态响应及其对地震波形的影响,地球物理学报,25,增刊,622——631,1982. [11] 维尔莫,p, L.地震观测业务手册,国家地震局地球物理研究所译,1979. |
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