Citation: | Chao Zhang, Lianwang Chen . 1991: COMPREHENSIVE STUDY ON STABILITY OF DEEP CRUST AND UNSTABLE BEHAVIOR OF EARTHQUAKE SOURCE BY BOTH FAILURE MECHANISM AND FRICTIONAL SLIDING MECHANISM. Acta Seismologica Sinica, 13(4): 462-470. |
[1] Anderson. E. M——1951. The dynamics of fracture. 2nd ed——Oliver +nd Bovd. Edinburgh,206
[2] P rice. N. J——1966—— h'ault urul joint rlevolopnrent in br——itlle and,senribrittle rock. Pergamon. London.Sibson. R. H.、1977. Fault rocks and fault mechanics. J. Geolophy,133,191——233 [3] Jaeger. J. C. and Cook. N. G. W,1976. Fundanntals onck Mrolrunics. 2nd ed. Chapman and Hall.London. 585PP. [4] Hubbet. M. and Rubey. W. W,1959. Role of fluid pressure in mechanics of overthrust faulting. Bull. Geol.Anur.,70. 115——205. [5] Sibson. R. H.,1974. Frictional constrains on thrust. wmench and nornml taults. Nature. Po.s. Sci,249,542——544. [6] Sibson. R. H.,1982. Fault zone models. heat flow. and depth distribution of earthduakes in the continental crust of the United States. Bull. Seism. Soe. Anr.,72. 151——163. [7] Haimson. B. C.,1978. The hydrofracturing stress mcasuing method and recent field results. Int. J. Rock Mec. Sci and Geonrech—— Abstr.,15. 167——178 [8] Haimson. B. C. and Rutnmel. F——1982. Hydrofracturing stress measurements in RDP drillhole at Reydre rdur. lceland.J. Geophys. Res., 87, B8. 6631——6649. [9] Brown. E. T. and Hoek. E——1978. Trends in relationships between measured in——situ stress and depth. Itrt. J.Rock Meeh——Sei.and Geonreoh——Ahstr.,15. 211——215. [10] 陈家庚、曹新玲、李自强,1982.水力压裂法测定华北地下深部应力.地震学报,4, 35,360. [11] 丁建民、梁国平. 1985.唐山天津和沧州地区的油井水压致裂应力测量.地震学报,7. 363——373. [12] 马宗晋、傅征祥、张郧珍,汪成民、张国民、刘德富,1982.中国九大地震.地震出版社,北京.216 pp. [13] 国家地震局《深部物探成果》编写组,1986.中国地壳上地慢地球物理探测成果.地震出版社.北京,407pp. [14] iriggs. D. T., Turner. F. J. and Heard, H. C:,1960. Deformation of rock at 500°C to 800°C. Gcul. Ant. Menruir. 79. 39——104. [15] Tullis. J. and Yund. R. A.,1977 Experimental deformation of dry westerly granite. J. Gerplirs. Res——82,5705——57 I 8. [16] Edmond. J. M. and Patterson, M. S, 1972. Volume changes during the deformation of rocks at high pres——sure. InI. J. Rock Mcch. Mining Sci.,9, 161——182 [17] Stcsky, R. M——Brace. W. F——Riley, D. K. and Robin, P. Y. F——1974. Fraction in faulted rock at high temperalure and pressure.Tecluttuphy.sic.s, 23, 177——203 [18] 王绳祖、张流,1982.地壳温压条件卜周口店花岗闪长岩的变形破坏.地震地质,4, 4, 68. [19] 高建理、丁建民、梁国平、郭启良,1987.华北地区盆地内地壳应力随深度的变化.中国地震,3, 4. 82——89. [20] 杨绪充,1985.济阳坳陷沙河街组区域应力及水动力特征探讨.石油勘探与开发,12, 13——20 [21] Evans. C. R.,Mclvor, D. K. and Magara, K.,1975. Organic matter, compection history and hydrocabon oc currence—— Meckenzie Delta. Imperial oil limited. Calgary, Albeita. Canada. Proceedings o the 9th World Petroleum Congress, 2. 149——157. [22] Byerlee, J——1978. Friction of rocks. Pure and Appl. Geophys., 116. 615——626. [23] 梁国平、丁建民,1987.测定水压破裂面方向的地面电测法原理及其在华北地区的测量结果.地壳构造与地壳 [24] 应力文集,1: 88——95,地震出版社,北京. [25] 张汝惠、解政文、武冀新、谢毅真、刘明,1982.唐山及其邻区热流值的分布.地震地质,4, 4, 57——67. [26] 汪良谋、张裕明、董瑞树,1982.华北平原及渤海地区新生代地堑的深部扩张及其与强震活动的关系.第二届全国构造地质学术会议论文选集、38——52,地质出版社.北京. [27] Patterson. M. S——1978 Experirmntal Rock Defomxrtion——The Brittle Field. SpingerVerlag, Berlin Heidelberg. New York, 354PP
[1] Anderson. E. M——1951. The dynamics of fracture. 2nd ed——Oliver +nd Bovd. Edinburgh,206
[2] P rice. N. J——1966—— h'ault urul joint rlevolopnrent in br——itlle and,senribrittle rock. Pergamon. London.Sibson. R. H.、1977. Fault rocks and fault mechanics. J. Geolophy,133,191——233 [3] Jaeger. J. C. and Cook. N. G. W,1976. Fundanntals onck Mrolrunics. 2nd ed. Chapman and Hall.London. 585PP. [4] Hubbet. M. and Rubey. W. W,1959. Role of fluid pressure in mechanics of overthrust faulting. Bull. Geol.Anur.,70. 115——205. [5] Sibson. R. H.,1974. Frictional constrains on thrust. wmench and nornml taults. Nature. Po.s. Sci,249,542——544. [6] Sibson. R. H.,1982. Fault zone models. heat flow. and depth distribution of earthduakes in the continental crust of the United States. Bull. Seism. Soe. Anr.,72. 151——163. [7] Haimson. B. C.,1978. The hydrofracturing stress mcasuing method and recent field results. Int. J. Rock Mec. Sci and Geonrech—— Abstr.,15. 167——178 [8] Haimson. B. C. and Rutnmel. F——1982. Hydrofracturing stress measurements in RDP drillhole at Reydre rdur. lceland.J. Geophys. Res., 87, B8. 6631——6649. [9] Brown. E. T. and Hoek. E——1978. Trends in relationships between measured in——situ stress and depth. Itrt. J.Rock Meeh——Sei.and Geonreoh——Ahstr.,15. 211——215. [10] 陈家庚、曹新玲、李自强,1982.水力压裂法测定华北地下深部应力.地震学报,4, 35,360. [11] 丁建民、梁国平. 1985.唐山天津和沧州地区的油井水压致裂应力测量.地震学报,7. 363——373. [12] 马宗晋、傅征祥、张郧珍,汪成民、张国民、刘德富,1982.中国九大地震.地震出版社,北京.216 pp. [13] 国家地震局《深部物探成果》编写组,1986.中国地壳上地慢地球物理探测成果.地震出版社.北京,407pp. [14] iriggs. D. T., Turner. F. J. and Heard, H. C:,1960. Deformation of rock at 500°C to 800°C. Gcul. Ant. Menruir. 79. 39——104. [15] Tullis. J. and Yund. R. A.,1977 Experimental deformation of dry westerly granite. J. Gerplirs. Res——82,5705——57 I 8. [16] Edmond. J. M. and Patterson, M. S, 1972. Volume changes during the deformation of rocks at high pres——sure. InI. J. Rock Mcch. Mining Sci.,9, 161——182 [17] Stcsky, R. M——Brace. W. F——Riley, D. K. and Robin, P. Y. F——1974. Fraction in faulted rock at high temperalure and pressure.Tecluttuphy.sic.s, 23, 177——203 [18] 王绳祖、张流,1982.地壳温压条件卜周口店花岗闪长岩的变形破坏.地震地质,4, 4, 68. [19] 高建理、丁建民、梁国平、郭启良,1987.华北地区盆地内地壳应力随深度的变化.中国地震,3, 4. 82——89. [20] 杨绪充,1985.济阳坳陷沙河街组区域应力及水动力特征探讨.石油勘探与开发,12, 13——20 [21] Evans. C. R.,Mclvor, D. K. and Magara, K.,1975. Organic matter, compection history and hydrocabon oc currence—— Meckenzie Delta. Imperial oil limited. Calgary, Albeita. Canada. Proceedings o the 9th World Petroleum Congress, 2. 149——157. [22] Byerlee, J——1978. Friction of rocks. Pure and Appl. Geophys., 116. 615——626. [23] 梁国平、丁建民,1987.测定水压破裂面方向的地面电测法原理及其在华北地区的测量结果.地壳构造与地壳 [24] 应力文集,1: 88——95,地震出版社,北京. [25] 张汝惠、解政文、武冀新、谢毅真、刘明,1982.唐山及其邻区热流值的分布.地震地质,4, 4, 57——67. [26] 汪良谋、张裕明、董瑞树,1982.华北平原及渤海地区新生代地堑的深部扩张及其与强震活动的关系.第二届全国构造地质学术会议论文选集、38——52,地质出版社.北京. [27] Patterson. M. S——1978 Experirmntal Rock Defomxrtion——The Brittle Field. SpingerVerlag, Berlin Heidelberg. New York, 354PP |
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