Citation: | LIN CHANGYOU, LIU XIAOLING, JANG MEI, Wu YUXIAcom sh . 1988: ON THE CONDUCTIVE LAYERS IN SOME REGIONS OF NORTHWESTERN CHINA AND THE DEEP ELECTRICAL INDEXES FOR SEISMOLOGICAL ZONING. Acta Seismologica Sinica, 10(1): 66-76. |
[1] 林长佑、张云琳,河西走廊地区下部地壳异常低阻层的发现,西北地震学报,1982,4,1,141——142,
[2] 林长佑、张云琳、粱恕信、司玉兰、蒋梅、江钊,内蒙、甘、宁某些地区地球上部电导率分布的横向变化特征,西北地震学报,1983,5,1,31——42, [3] 国家地震局兰州地震大队大地电磁测深组,中国南北地震带北段地壳和上地慢的电性特征,地球物理学报,1976,19,28——34, [4] 林长佑、张云琳、司玉兰、蒋梅、李柱国,河西走廊东部地区的大地电磁测深研究,地球物理学报,1984,27,131——143, [5] E. P.波波夫,固体力学引论,王士耕、韩二丽译,165——188,1985,人民邮电出版社. [6] 秦保燕、郭增建,由地震时震中区的显著下沉讨论震源的底部条件,西北地震学报,1979,1,1,8——15, [7] 国家地震局兰州地震研究所大地电磁测深组,与大地震有关的地壳深部的电性变化,大地电磁测深,8 0——8 8 ,1981,地震出版社. [8] 林长佑,大震孕震物理过程的初步探讨,西北地震学报,1979,1,3,42——48, [9] 姚振兴、李白基、梁尚鸿、朱培定、张立敏、卢善声,青藏高原地区瑞利波群速度和地壳构造,地球物理学报,1981,24,287——295, [10] Kurd., R. D., Magnetotelluric interpretation of crust al and mantle structure in the Grenvilleprovince, Geophys. J. R. Astr. Soc., 1982, 70, 373——397, [11] Kern, H., Elestic——wave velocity in crust al and mantle rocks at high pressure and temperature:the role of the high——low quartz transition and of dehydration reaction, Phyr. Earth Planet. In t.,1982, 29, 12——23, [12] 张少泉、武利均、郭建明等,中国西部地区门源——平凉——渭南地震测深剖面资料的分析解释,地球物理学报,1985,28,460——472. [13] Lin Changyou, Phase transition dehydration—A possible way of interior source of the water in the focal region,西北地震学报,1964,6,1,64——92, [14] Word, D. R., H. W. Smith, and F. X. Jr, Bostic, Crustal investigations Uy the magnetotelluric tensor impeuance method, The structure and physical properties of the earth's crust, Geophysical Monograph 14, 145——167, 1971 American geophysical Union, Washington, D. C. [15] 林长佑,第八章地壳上地慢条件下岩石的导电性,大地电磁测深研究,301——341地震出版社,1985, [16] 荣代潞,像力及其在震源过程中的作用,西北地震学报,1952,4,1,7——23, [17] ELsasser, W. M., Sea——floor spreading as thermal convection, ,l. Grophys. Res., 1971, 76, 1101——1111, [18] Stacey, F. D., Chapter 7, Physics of the Earth, John wiley a,:,l Sons, lnc., 1969,
[1] 林长佑、张云琳,河西走廊地区下部地壳异常低阻层的发现,西北地震学报,1982,4,1,141——142,
[2] 林长佑、张云琳、粱恕信、司玉兰、蒋梅、江钊,内蒙、甘、宁某些地区地球上部电导率分布的横向变化特征,西北地震学报,1983,5,1,31——42, [3] 国家地震局兰州地震大队大地电磁测深组,中国南北地震带北段地壳和上地慢的电性特征,地球物理学报,1976,19,28——34, [4] 林长佑、张云琳、司玉兰、蒋梅、李柱国,河西走廊东部地区的大地电磁测深研究,地球物理学报,1984,27,131——143, [5] E. P.波波夫,固体力学引论,王士耕、韩二丽译,165——188,1985,人民邮电出版社. [6] 秦保燕、郭增建,由地震时震中区的显著下沉讨论震源的底部条件,西北地震学报,1979,1,1,8——15, [7] 国家地震局兰州地震研究所大地电磁测深组,与大地震有关的地壳深部的电性变化,大地电磁测深,8 0——8 8 ,1981,地震出版社. [8] 林长佑,大震孕震物理过程的初步探讨,西北地震学报,1979,1,3,42——48, [9] 姚振兴、李白基、梁尚鸿、朱培定、张立敏、卢善声,青藏高原地区瑞利波群速度和地壳构造,地球物理学报,1981,24,287——295, [10] Kurd., R. D., Magnetotelluric interpretation of crust al and mantle structure in the Grenvilleprovince, Geophys. J. R. Astr. Soc., 1982, 70, 373——397, [11] Kern, H., Elestic——wave velocity in crust al and mantle rocks at high pressure and temperature:the role of the high——low quartz transition and of dehydration reaction, Phyr. Earth Planet. In t.,1982, 29, 12——23, [12] 张少泉、武利均、郭建明等,中国西部地区门源——平凉——渭南地震测深剖面资料的分析解释,地球物理学报,1985,28,460——472. [13] Lin Changyou, Phase transition dehydration—A possible way of interior source of the water in the focal region,西北地震学报,1964,6,1,64——92, [14] Word, D. R., H. W. Smith, and F. X. Jr, Bostic, Crustal investigations Uy the magnetotelluric tensor impeuance method, The structure and physical properties of the earth's crust, Geophysical Monograph 14, 145——167, 1971 American geophysical Union, Washington, D. C. [15] 林长佑,第八章地壳上地慢条件下岩石的导电性,大地电磁测深研究,301——341地震出版社,1985, [16] 荣代潞,像力及其在震源过程中的作用,西北地震学报,1952,4,1,7——23, [17] ELsasser, W. M., Sea——floor spreading as thermal convection, ,l. Grophys. Res., 1971, 76, 1101——1111, [18] Stacey, F. D., Chapter 7, Physics of the Earth, John wiley a,:,l Sons, lnc., 1969, |
Guo Huili, Ding Zhifeng. 2018: Crustal velocity structure beneath the northern North-South Seismic Zone from local seismic tomography and its tectonic implications. Acta Seismologica Sinica, 40(5): 547-562. DOI: 10.11939/jass.20180006 | |
2018: 《纪念汶川大地震十周年》专辑前言. Acta Seismologica Sinica, 40(3): 1-1. | |
Mei Xiupingup, Shao Zhigangup Zhang Langpingup Feng Jiangangup, Dai Weiup,://caref=http. 2012: Study on potential earthquake risk of unbroken active faults in the northern segment of the North-South seismic zone. Acta Seismologica Sinica, 34(4): 509-525. | |
2004: 华东地区地电阻率各向异性度的地震前兆异常特征初步研究. Acta Seismologica Sinica, 26(2): 223-227. | |
Xinling Qinup, L. B. Pedersonup2, Yulin Zhaoup, Ping Zhangup2, Fuye Qianup, Wei Qianup2, Zhengnan Liup, Jingxian Duuptitletyle(415px,auto,a. 1991: CONDUCTIVITY STRUCTURE OF CRUST IN THE TANGSHAN SEISMIC AREA AND THE POSSIBILITY OF EXPLORING POTENTIAL SEISMIC SOURCES BY MAGNETOTELLURIC METHOD. Acta Seismologica Sinica, 13(3): 354-363. | |
LIANG GUIPEI, LI WEIJUAN h. 1990: THE CHARACTERISTICS OF DEEP STRUCTURE OF THE NORTH SEGMENT OF THE NORTH-SOUTH SEISMIC BELT. Acta Seismologica Sinica, 12(2): 176-185. | |
LIN CHANGYOU, Liu XIAOLING, Wu YUXIAcom sh advance. 1990: THE FURTHER APPLICATION OF MAGNETOTELLURIC SOUNDING IN THE PROBE OF EARTHQUAKE PRECURSORS. Acta Seismologica Sinica, 12(2): 166-175. | |
GU JINPIPNG, YU XUEJUN, SIIENG GUOTINGcom sh advance. 1986: RECKONING EARTHQUAKE MAGNITUDE AND OCCURRENCE TIME FOR THE NORTHERN PORTION OF THE NORTH-SOUTH EARTHQUAKE BELT OF CHINA. Acta Seismologica Sinica, 8(1): 21-27. |