中国东部海域活动构造定量研究若干问题探讨

陈晓辉; 李日辉

doi:10.16562/j.cnki.0256-1492.2017.03.010

中国东部海域活动构造定量研究若干问题探讨

陈晓辉^1,2,,
李日辉^1,2

1.
国土资源部海洋油气资源与环境地质重点实验室, 青岛 266071

2.
中国地质调查局青岛海洋地质研究所, 青岛 266071

基金项目:
国家自然科学基金项目(41406077);国土资源大调查项目(1212011220113, GZH201500203, GZH201400205, 121201005000150019)

详细信息

作者简介: 陈晓辉(1981—), 男, 助理研究员, 主要从事晚第四纪地层与环境地质研究, E-mail:hongzi1982@163.com

中图分类号: P736.1

蔡秋蓉编辑

收稿日期: 2016-03-11

修回日期: 2016-08-18

刊出日期: 2017-06-28

A REVIEW ON QUANTITATIVE STUDIES OF ACTIVE TECTONICS IN EASTERN CHINA SEAS

CHEN Xiaohui^1,2,,
LI Rihui^1,2

1.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071

2.
Qingdao Institute of Marine Geology, Qingdao 266071

Received Date: 11 March 2016

Revised Date: 18 August 2016

Publish Date: 28 June 2017

摘要

摘要:
晚更新世以来的活动构造与现代地质灾害密切相关，目前针对陆域活动构造的定量研究成果卓著，而在海域方面研究薄弱。本文综述了国内外有关海域活动构造的研究进展，提出了目前国内海域活动构造定量研究存在的主要问题。在研究实践的基础上，阐述了海域活动构造的主要研究方法、其定量研究的关键问题及解决方案，重点总结了海域活动构造区地震危险性定量评价的研究方案，并进一步探讨了海域活动构造自身因素的危险性定量评价的研究思路。
- 晚更新世 /
- 活动构造 /
- 定量研究 /
- 东部海域
Abstract:
Many kinds of modern geo-hazards are closely related to the active tectonic movement since Pleistocene.Many quantitative researches have been devoted to the active tectonics on land, but seldom in the sea. This paper presents a review on progresses of the research on marine active tectonics in China and some other countries, in which, we made a review of the main problems encountered recently in quantitative studies of active tectonics in the sea area of China, and discussed the main methods for study of marine active tectonics, as well as the key issues for quantitative research and solutions based on the practice in recent years. Emphasis is put on the research schemes for the quantitative risk assessment on potential earthquake in the tectonically active region. Further, the paper discussed the way of thinking for quantitative risk assessment of marine active tectonics from self-factors of China seas.
- Pleistocene /
- active tectonics /
- quantitative research /
- eastern China seas

HTML全文

图 1 中国东部海域及周边主要断裂^[26]及地震震中

Figure 1.

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图 2 渤海海域活动断层典型浅地层剖面^[45]

Figure 2.

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图 3 渤海海域活动断层典型单道地震剖面^[45]

Figure 3.

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图 4 渤海BH08孔上部50 m段综合地层划分^[46]

Figure 4.

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表 1 海域活动构造自身因素危险性定量评价的主要评价指标

Table 1. The main indicators of quantitative risk assessment for marine active tectonics from self-factors in China seas area

评价指标	赋值原则
最新活动时间	由新至老，由大到小的原则
断距	由大至小，由大到小的原则
活动速率	由大至小，由大到小的原则
距活动构造的距离	由近至远，由大到小的原则，借鉴国外陆域活动构造避让距离的研究成果^[57]，赋值时不但需要分析海域活动构造的自身影响范围，而且需充分考虑海域已经存在的管线、光缆及其他工程设施的分布，对各网格单元科学合理的进行赋值。
......	......

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参考文献(58)

[1]	邓起东, 陈立春, 冉勇康.活动构造定量研究与应用[J].地学前缘, 2004, 11(4): 383-392. doi: 10.3321/j.issn:1005-2321.2004.04.005 DENG Qidong, CHEN Lichun, RAN Yongkang. Quantitative studies and applications of active tectonics[J]. Earth Science Frontiers, 2004, 11(4): 383-392. doi: 10.3321/j.issn:1005-2321.2004.04.005
[2]	Momma H, Kawaguchi K, Iwase R, et al. Seabeam and deep tow surveys off Hatsushima Island after 1997 earthquake swarm east of Izu Peninsula[J]. Journal of Deep-Sea Research, 1997, 13: 375-393.
[3]	Nanayama F, Ikeda M, Otsuka K, et al. Regional imaging and segmentation of the MTL active fault system in the Iyo-nada sea-off saganoseki area[J]. Annual Report on Active Fault and Paleoearthquake Researches, 2002, 2: 141-152.
[4]	Itoh Y, Tsutsumi H, Yamamoto N, et al. Active right-lateral strike-slip fault zone along the southern margin of the Japan Sea[J]. Tectonophysics, 2002, 351(4): 301-314. doi: 10.1016/S0040-1951(02)00164-6
[5]	Okamura Y, Satake K, Ikehara K, et al. Paleoseismology of deep-sea faults based on marine surveys of northern Okushiri ridge in the Japan Sea[J]. Journal of Geophysical Research, 2005, 110(B5): B09105, doi: 10.1029/2004JB003135.
[6]	Ishiyama T, Sato H, Abe S, et al. High-resolution 3D seismic reflection imaging across active faults and its impact on seismic hazard estimation in the Tokyo metropolitan area[J]. Tectonophysics, 2016, 689: 79-88, doi: 10.1016/j.tecto.2016.01.042.
[7]	Ambraseys N N, Finkel C F. Long-term seismicity of Istanbul and of the Marmara Sea region[J]. Terra Nova, 1991, 3(5): 527-539. doi: 10.1111/j.1365-3121.1991.tb00188.x
[8]	Okay A I, KaŞlIlar-Özcan A, ĺmren C, et al. Active faults and evolving strike-slip basins in the Marmara Sea, northwest Turkey: A multichannel seismic reflection study[J]. Tectonophysics, 2000, 312(2): 189-218. doi: 10.1016/S0040-1951(00)00046-9
[9]	Kuşçuİ, Okamura M, Matsuoka H, et al. Active faults in the Gulf of zmit on the North Anatolian Fault, NW Turkey: a high-resolution shallow seismic study[J]. Marine Geology, 2002, 190(1-2): 421-443. doi: 10.1016/S0025-3227(02)00357-2
[10]	Le Pichon X, Chamot-Rooke N, Rangin C, et al. The North Anatolian fault in the Sea of Marmara[J]. Journal of Geophysical Research, 2003, 108(B4): 2179, doi: 10.1029/2002JB001862.
[11]	Flerit F, Armijo R, King G C P, et al. Slip partitioning in the Sea of Marmara Pull-Apart determined from GPS velocity vectors[J]. Geophysical Journal International, 2003, 154(1): 1-7. doi: 10.1046/j.1365-246X.2003.01899.x
[12]	Armijo R, Pondard N, Meyer B, et al. Submarine fault scarps in the Sea of Marmara pull-apart (North Anatolian Fault): implications for seismic hazard in Istanbul[J]. Geochemistry, Geophysics, Geosystems, 2005, 6(6): Q06009, doi: 10.1029/2004GC000896.
[13]	Muller J R, Aydin A. Using mechanical modeling to constrain fault geometries proposed for the northern Marmara Sea[J]. Journal of Geophysical Research, 2005, 110(B3): B03407, doi: 10.1029/2004JB003226.
[14]	Mchugh C M G, Braudy N, Caǧatay M N, et al. Seafloor fault ruptures along the North Anatolia Fault in the Marmara Sea, Turkey: Link with the adjacent basin turbidite record[J]. Marine Geology, 2014, 353: 65-83. doi: 10.1016/j.margeo.2014.03.005
[15]	Alvarez-Marrón J. Pliocene to Holocene structure of the eastern Alboran Sea (Western Mediterranean)[M]//Zahn R, Comas M C. Klaus A. Proceedings of the Ocean Drilling Program, Scientific Results. College Station, TX: ODP, 1999, 161: 145-156.
[16]	Haughton P. Contained turbidites used to track sea bed deformation and basin migration, Sorbas Basin, south-east Spain[J]. Basin Research, 2001, 13(2): 117-139. doi: 10.1046/j.1365-2117.2001.00143.x
[17]	Nalbant S S, Hubert A, King G C P. Stress coupling between earthquakes in northwest Turkey and the North Aegean Sea[J]. Journal of Geophysical Research, 1998, 103(B10): 24469-24486. doi: 10.1029/98JB01491
[18]	Saatcilar R, Ergintav S, Demirba? E, et al. Character of active faulting in the North Aegean Sea[J]. Marine Geology, 1999, 160(3-4): 339-353. doi: 10.1016/S0025-3227(99)00025-0
[19]	Kurt H, Demirbaǧ E, Kuscu. Active submarine tectonism and formation of the Gulf of Saros, Northeast Aegean Sea, inferred from multi-channel seismic reflection data[J]. Marine Geology, 2000, 165(1-4): 13-26. doi: 10.1016/S0025-3227(00)00005-0
[20]	Piper D J W, Perissoratis C. Quaternary neotectonics of the South Aegean arc[J]. Marine Geology, 2003, 198(3-4): 259-288. doi: 10.1016/S0025-3227(03)00118-X
[21]	Déverchère J, Yelles K, Domzig A, et al. Active thrust faulting offshore Boumerdes, Algeria, and its relations to the 2003 Mw 6.9 earthquake[J]. Geophysical Research Letters, 2005, 32: L04311.
[22]	廖其林, 王振明, 王屏路, 等.福州-泉州-汕头地区地壳结构的爆炸地震研究[J].地球物理学报, 1988, 31(3): 270-280. doi: 10.3321/j.issn:0001-5733.1988.03.004 LIAO Qilin, WANG Zhenming, WANG Pinglu, et al. Explosion seismic study of the crustal structure in Fuzhou-Quanzhou-Shantou region[J]. Acta Geophysica Sinica, 1988, 31(3): 270-280. doi: 10.3321/j.issn:0001-5733.1988.03.004
[23]	姚伯初, 曾维军, 陈艺中, 等.南海北部陆缘东部的地壳结构[J].地球物理学报, 1994, 37(1): 27-35. doi: 10.3321/j.issn:0001-5733.1994.01.004 YAO Bochu, ZENG Weijun, CHEN Yizhong, et al. The crustal structure in the eastern part of the northern margin of the South China Sea[J]. Acta Geophysica Sinica, 1994, 37(1): 27-35. doi: 10.3321/j.issn:0001-5733.1994.01.004
[24]	Yan P, Zhou D, Liu Z S. A crustal structure profile across the northern continental margin of the south China sea[J]. Tectonophysics, 2001, 338(1): 1-21. doi: 10.1016/S0040-1951(01)00062-2
[25]	赵明辉, 丘学林, 叶春明, 等.南海东北部海陆深地震联测与滨海断裂带两侧地壳结构分析[J].地球物理学报, 2004, 47(5): 845-852. doi: 10.3321/j.issn:0001-5733.2004.05.016 ZHAO Minghui, QIU Xuelin, YE Chunming, et al. Analysis on deep crustal structure along the onshore-offshore seismic profile across the Binhai (Littoral) Fault Zone in northeastern South China Sea[J]. Chinese Journal of Geophysics, 2004, 47(5): 845-852. doi: 10.3321/j.issn:0001-5733.2004.05.016
[26]	李培英, 杜军, 刘乐军, 等.中国海岸带灾害地质特征及评价[M].北京:海洋出版社, 2007. LI Peiying, DU Jun, LIU Lejun, et al. Characteristics and Evaluation of Hazard Geology in Coastal Zone of China[M]. Beijing: China Ocean Press, 2007.
[27]	胡政, 丁东.渤海地震震中附近地区浅层地质构造特征[J].地震学刊, 1990(3): 26-32. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000378673 HU Zheng, DING Dong. The characteristics of the shallow geololgical structure in the adjacent region of the epicenter of the Bohai Sea earthquake[J]. Journal of Seismology, 1990(3): 26-32. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000378673
[28]	赵根模, 赵国敏, 杨港生, 等.声波探测显示的渤海湾西部全新世断层活动[J].中国地震, 2005, 21(2): 139-146. doi: 10.3969/j.issn.1001-4683.2005.02.001 ZHAO Genmo, ZHAO Guomin, YANG Gangsheng, et al. The Holocene active fault in the western part of Bohai Gulf showed by acoustic sounding[J]. Earthquake Research in China, 2005, 21(2): 139-146. doi: 10.3969/j.issn.1001-4683.2005.02.001
[29]	郑彦鹏, 王勇, 陈宇坤, 等.天津塘沽地区海河断裂的浅部构造特征[J].海洋科学进展, 2006, 24(3): 307-313. doi: 10.3969/j.issn.1671-6647.2006.03.006 ZHENG Yanpeng, WANG Yong, CHEN Yukun, et al. Shallow tectonic characteristics of the Haihe Fault in Tanggu Area, Tianjin municipality[J]. Advances in Marine Science, 2006, 24(3): 307-313. doi: 10.3969/j.issn.1671-6647.2006.03.006
[30]	王志才, 邓起东, 杜宪宋, 等.莱州湾海域郯庐断裂带活断层探测[J].地震学报, 2006, 28(5): 493-503. doi: 10.3321/j.issn:0253-3782.2006.05.006 WANG Zhicai, DENG Qidong, DU Xiansong, et al. Active fault survey on the Tanlu fault zone in Laizhou Bay[J]. Acta Seismologica Sinica, 2006, 28(5): 493-503. doi: 10.3321/j.issn:0253-3782.2006.05.006
[31]	李西双, 裴彦良, 刘保华, 等. 1969年渤海M_S 7.4地震发震断层的声学探测[J].地球物理学报, 2009, 52(9): 2291-2301. doi: 10.3969/j.issn.0001-5733.2009.09.013 LI Xishuang, PEI Yanliang, LIU Baohua, et al. Acoustic detection of the causative fault of 1969 M_S7.4 earthquake in Bohai Sea[J]. Chinese Journal of Geophysics, 2009, 52(9): 2291-2301. doi: 10.3969/j.issn.0001-5733.2009.09.013
[32]	李西双, 刘保华, 华清峰, 等.张家口-蓬莱断裂带渤海段晚第四纪活动特征[J].海洋科学进展, 2009, 27(3): 332-341. doi: 10.3969/j.issn.1671-6647.2009.03.006 LI Xishuang, LIU Baohua, HUA Qingfeng, et al. Characters of the Zhangjiakou-Penglai Fault Zone activity in the Bohai Sea since Late Quaternary[J]. Advances in Marine Science, 2009, 27(3): 332-341. doi: 10.3969/j.issn.1671-6647.2009.03.006
[33]	李西双, 赵月霞, 刘保华, 等.郯庐断裂带渤海段晚更新世以来的浅层构造变形和活动性[J].科学通报, 2010, 55(8): 684-692. doi: 10.1360/csb2010-55-8-684 LI Xishuang, ZHAO Yuexia, LIU Baohua, et al. Structural deformation and fault activity of the Tan-Lu fault zone in the Bohai Sea since the late Pleistocene[J]. Chinese Science Bulletin, 2010, 55(18): 1908-1916. doi: 10.1360/csb2010-55-8-684
[34]	李西双, 刘保华, 赵月霞, 等.渤海海域晚更新世-全新世的活动构造[J].海洋学报, 2010, 32(5): 52-59. http://d.old.wanfangdata.com.cn/Periodical/hyxb201005007 LI Xishuang, LIU Baohua, ZHAO Yuexia, et al. Late Pleistocene-Holocene submarine active structures in the Bohai Sea[J]. Acta Oceanologica Sinica, 2010, 32(5): 52-59. http://d.old.wanfangdata.com.cn/Periodical/hyxb201005007
[35]	王洪聚, 刘保华, 李西双.晚更新世以来渤海南部海域断裂活动性[J].地球科学进展, 2011, 26(5): 556-564. doi: 10.11867/j.issn.1001-8166.2011.05.0556 WANG Hongju, LIU Baohua, LI Xishuang. Activity of the faults in the southern part of Bohai Sea since the Late Pleistocene[J]. Advances in Earth Science, 2011, 26(5): 556-564. doi: 10.11867/j.issn.1001-8166.2011.05.0556
[36]	Zhu G, Hu W, Song L H, et al. Quaternary activity along the Tan-Lu fault zone in the Bohai Bay, East China: Evidence from seismic profiles[J]. Journal of Asian Earth Sciences, 2015, 114: 5-17. doi: 10.1016/j.jseaes.2015.03.030
[37]	王志才, 邓起东, 晁洪太, 等.山东半岛北部近海海域北西向蓬莱-威海断裂带的声波探测[J].地球物理学报, 2006, 49(4): 1092-1101. doi: 10.3321/j.issn:0001-5733.2006.04.022 WANG Zhicai, DENG Qidong, CHAO Hongtai, et al. Shallow-depth sonic reflection profiling studies on the active Penglai-Weihai fault zone offshore of the northern Shandong Peninsula[J]. Chinese Journal of Geophysics, 2006, 49(4): 1092-1101. doi: 10.3321/j.issn:0001-5733.2006.04.022
[38]	王志才, 晁洪太, 杜宪宋, 等.南黄海北部千里岩断裂活动性初探[J].地震地质, 2008, 30(1): 176-186. doi: 10.3969/j.issn.0253-4967.2008.01.012 WANG Zhicai, CHAO Hongtai, DU Xiansong, et al. Preliminary survey on the Quaternary activities of the Qianliyan Fault in the northern part of the South Yellow Sea[J]. Seismology and Geology, 2008, 30(1): 176-186. doi: 10.3969/j.issn.0253-4967.2008.01.012
[39]	马胜中.浅层地球物理方法在广西钦州湾-北海海域断层探测的应用[J].海洋技术, 2010, 29(2): 20-24. doi: 10.3969/j.issn.1003-2029.2010.02.005 MA Shengzhong. Application of shallow geophysical method to detect active fault in nearshore of Qingzhou Bay-Beihai[J]. Ocean Technology, 2010, 29(2): 20-24. doi: 10.3969/j.issn.1003-2029.2010.02.005
[40]	Demirbaǧ E, Rangin C, Le Pichon X, et al. Investigation of the tectonics of the Main Marmara Fault by means of deep-towed seismic data[J]. Tectonophysics, 2003, 361(1-2): 1-19. doi: 10.1016/S0040-1951(02)00535-8
[41]	李西双, 刘保华, 赵月霞, 等.海底活动断裂研究方法及我国近海活动断裂研究[J].海洋地质动态, 2008, 24(3): 8-13. doi: 10.3969/j.issn.1009-2722.2008.03.002 LI Xishuang, LIU Baohua, ZHAO Yuexia, et al. Methodology for research of seabed activity fracture and research on paralic activity fracture in China[J]. Marine Geology Letters, 2008, 24(3): 8-13. doi: 10.3969/j.issn.1009-2722.2008.03.002
[42]	mren C, Le Pichon X, Rangin C, et al. The North Anatolian fault within the Sea of Marmara: a new interpretation based on multi-channel seismic and multi-beam bathymetry data[J]. Earth and Planetary Science Letters, 2001, 186(2): 143-158. doi: 10.1016/s0012-821x(01)00241-2
[43]	Gazioǧlu C, Gökasan E, Algan O, et al. Morphologic features of the Marmara Sea from multi-beam data[J]. Marine Geology, 2002, 190(1-2): 397-420. doi: 10.1016/S0025-3227(02)00356-0
[44]	Yaltirak C, Alpar B. Evolution of the middle strand of north Anatolian Fault and shallow seismic investigation of the southeastern Marmara Sea (Gemlik bay)[J]. Marine Geology, 2002, 190(1-2): 307-327. doi: 10.1016/S0025-3227(02)00352-3
[45]	青岛海洋地质研究所. 1: 100万天津幅海洋区域地质调查报告[R]. 2015. Qingdao Institute of Marine Geology. 1: 1000000 Tianjin Marine Geological Survey Report[R]. 2015.
[46]	李小艳, 赵泉鸿, 姚政权, 等.渤海百万年以来的海侵记录: BH08孔有孔虫和介形类证据[J].海洋地质与第四纪地质, 2015, 35(6): 93-108. LI Xiaoyan, ZHAO Quanhong, YAO Zhengquan, et al. Transgressive records of last million years in the Bohai Sea, China: evidence from Foraminifera and Ostracoda of core BH08[J]. Marine Geology and Quaternary Geology, 2015, 35(6): 93-108.
[47]	邓起东, 闻学泽.活动构造研究—历史、进展与建议[J].地震地质, 2008, 30(1): 1-30. doi: 10.3969/j.issn.0253-4967.2008.01.002 DENG Qidong, WEN Xueze. A review on the research of active tectonics—history, progress and suggestions[J]. Seismology and Geology, 2008, 30(1): 1-30. doi: 10.3969/j.issn.0253-4967.2008.01.002
[48]	邓起东.城市活动断裂探测和地震危险性评价问题[J].地震地质, 2002, 24(4): 601-605. doi: 10.3969/j.issn.0253-4967.2002.04.015 DENG Qidong. Exploration and seismic hazard assessment of active faults in urban areas[J]. Seismology and Geology, 2002, 24(4): 601-605. doi: 10.3969/j.issn.0253-4967.2002.04.015
[49]	闻学泽, 徐锡伟, 龙锋, 等.中国大陆东部中—弱活动断层潜在地震最大震级评估的震级—频度关系模型[J].地震地质, 2007, 29(2): 236-253. doi: 10.3969/j.issn.0253-4967.2007.02.004 WEN Xueze, XU Xiwei, LONG Feng, et al. Frequency-magnitude relationship models for assessment of maximum magnitudes of potential earthquakes on moderately and weakly active faults in eastern China mainland[J]. Seismology and Geology, 2007, 29(2): 236-253. doi: 10.3969/j.issn.0253-4967.2007.02.004
[50]	陈宇坤, 刘芳, 袁盾, 等.天津地区隐伏断裂地震危险性定量评价[J].地震地质, 2010, 32(1): 138-149. doi: 10.3969/j.issn.0253-4967.2010.01.014 CHEN Yukun, LIU Fang, YUAN Dun, et al. Seismic risk quantitative evaluation on blind faults in Tianjin area[J]. Seismology and Geology, 2010, 32(1): 138-149. doi: 10.3969/j.issn.0253-4967.2010.01.014
[51]	刘红艳, 陈宇坤, 闫成国, 等.天津近海海域隐伏断裂地震危险性评价[J].震灾防御技术, 2013, 8(2): 146-155. doi: 10.3969/j.issn.1673-5722.2013.02.004 LIU Hongyan, CHEN Yukun, YAN Chengguo, et al. Seismic risk evaluation on blind faults in Tianjin offshore areas[J]. Technology for Earthquake Disaster Prevention, 2013, 8(2): 146-155. doi: 10.3969/j.issn.1673-5722.2013.02.004
[52]	Gutenberg B, Richter C F. Magnitude and energy of earthquakes[J]. Annali di Geofisica, 1956, 9: 1-15. doi: 10.1126/science.83.2147.183
[53]	Mogi K. Magnitude-frequency relation for elastic shocks accompanying fractures of various materials and some related problems in earthquakes[J]. Bulletin of the Earthquake Research Institute, University of Tokyo, 1962, 40(4): 831-853.
[54]	Cornell C A. Engineering seismic risk analysis[J]. Bulletin of the Seismological Society of America, 1968, 58(5): 1583-1606. doi: 10.1161/CIRCULATIONAHA.111.084483
[55]	Wyss M, Wiemer S. Change in the probability for earthquakes in southern California due to the landers magnitude 7.3 earthquake[J]. Science, 2000, 290(5495): 1334-1338. doi: 10.1126/science.290.5495.1334
[56]	青岛海洋地质研究所. 1: 100万大连幅海洋区域地质调查报告[R]. 2013. Qingdao Institute of Marine Geology. 1: 1000000 Dalian Marine Geological Survey Report[R]. 2013.
[57]	张建毅, 薄景山, 袁一凡, 等.活动断层及其避让距离研究综述[J].自然灾害学报, 2012, 21(2): 9-18. http://zrzh.iemzzs.com/oa/search.aspx?q=%BB%EE%B6%AF%B6%CF%B2%E3%BC%B0%C6%E4%B1%DC%C8%C3%BE%E0%C0%EB%D1%D0%BE%BF%D7%DB%CA%F6 ZHANG Jianyi, BO Jingshan, YUAN Yifan, et al. Review of research on active fault and its setback[J]. Journal of Natural Disasters, 2012, 21(2): 9-18. http://zrzh.iemzzs.com/oa/search.aspx?q=%BB%EE%B6%AF%B6%CF%B2%E3%BC%B0%C6%E4%B1%DC%C8%C3%BE%E0%C0%EB%D1%D0%BE%BF%D7%DB%CA%F6
[58]	陆雍森.环境评价[M].上海:同济大学出版社, 1990. LU Yongsen. Environment Assessment[M]. Shanghai: Tongji University Press, 1990.