APPLICATION PROGRESS OF RECRYSTALLIZED CARBONATE IN THE STUDY OF FAULT AND LANDSLIDE ACTIVITY IN CARBONATE BEDROCK AREA

doi:10.3969/j.issn.0253-4967.2024.01.005

Abstract

Abstract:

The research on the activity history of seismogenic faults is the basis for the research and prevention of natural disasters such as earthquakes and landslides. Dating has always been the focus and difficulty of the research on the activity history of fault. However, it is difficult to carry out geochronological surveys for faults and landslides evolution in the carbonated areas due to the lack of suitable dating materials, such as the region of south-eastern Tibet where the main lithology is carbonate bedrock. The exposure dating of cosmogenic nuclides is the main method to determine the activity history of fault. But the cosmic nuclides 36Cl and ¹⁴C dating methods still have some limitations, such as the complex generation mode of 36Cl being caused by fission under the action of cosmic rays, neutron capture and meson action, the yield of 36Cl being changed with chemical composition change of dating mineral(the range of 2-171atom/g·a), and so on. More importantly, the rapid rock weathering in the carbonate bedrock area is a big problem. Once exposed, the bedrock will start rapid weathering and erosion and dissolution. Therefore, it is necessary to find new dating materials or dating methods in carbonate bedrock areas, especially in areas with little or no quaternary sediments. When a large landslide moves on the sliding surface of carbonate bedrock, heat is often generated due to high-speed friction, and then the dynamic metamorphism can occur easily on the sliding surface to form recrystallized carbonate, which can be used to determine the active time of faults.

Carbonate is one of the main materials for ESR dating. As early as the 1970s, Ikeya made the first electron spin resonance(ESR)dating study of carbonates using stalactite calcite. After that, many researches on the ESR signal characteristics of carbonate(such as coral, shell, aragonite, stalagmite and etc)were carried out, and the carbonate ESR dating then became one of the main methods in Quaternary chronology and had been widely used. The recrystallized carbonate on the fault friction surface and the sliding surface of the landslide is a newly discovered dating material. Although its main component is calcium carbonate, its origin is different from the carbonate materials commonly used in ESR dating(such as stalagmite, stalactite, etc.), so it is necessary to study its characteristics of ESR dating.

The characteristics of recrystallized carbonate collected from the fault friction surface of Jianchuan section on Lijiang-Xiaojinhe Fault(Yin et al., 2021)and the sliding surface of Qiaojia landslide which is located at the intersection of Xiaojiang Fault and Zemuhe Fault(Liu et al., 2023)have been studied, including microstructure, thermal annealing characteristics, sunlight bleaching characteristics, and compared with the previous dating results of AMS ¹⁴C and OSL on sediments. Yin et al.(2021)and Liu et al.(2023)analyzed and demonstrated the feasibility and reliability of the recrystallized carbonate ESR dating method used in the analysis of bedrock fault and landslide activity in the carbonate bedrock area, and established the recrystallized carbonate ESR dating technology.

Therefore, the ESR dating of recrystallized carbonate is an effective dating technology and can be used widely for the studying of activity history of faults and landslides in carbonate bedrock areas. This paper introduced the latest research progress of recrystallized carbonate ESR dating in the Carbonate rock area of southwest China by Yin et al.(2021)and Liu et al.(2023). In this paper, the requirements for sample collection and the range of dating were proposed which provide technical support for dating of key geological samples for research on fault and landslide activity history, engineering exploration, active structure, and seismic risk assessment in Carbonate rock bedrock area.

Key words: ESR dating, carbonate rock, bedrock fault, landslide, recrystallization

摘要：

开展发震断层活动历史研究是地震、滑坡等自然灾害研究和防治的基础, 年代测定一直是断层活动历史研究的热点和难点。在缺乏第四纪沉积物的碳酸盐岩基岩区, 宇生核素暴露测年是确定断层活动历史的主要手段, 但测年结果受曝露面表面风化、侵蚀和溶蚀作用影响较大。碳酸盐是ESR年代学研究的主要测年矿物之一, 可以测量碳酸盐的结晶年龄。在碳酸盐岩基岩区的大型断层面和滑坡滑动面上, 因高速摩擦生热可形成重结晶碳酸盐, 为ESR测年提供了可靠的测年计时零点, 有望通过ESR测年法获得重结晶碳酸盐的结晶年龄, 即断层和滑坡最近一次的活动时代。以往用于ESR测年的碳酸盐都是自生碳酸盐, 如珊瑚、石笋、文石等, 尚未对断层和滑坡滑动面上的重结晶碳酸盐开展过相关研究。因此, 文中介绍了重结晶碳酸盐ESR测年的最新研究, 以丽江-小金河断裂剑川剖面的断层面和小江断裂与则木河断裂交会处的巧家滑坡后缘滑动面上的重结晶碳酸盐为研究对象, 通过微观结构观察、热退火实验、光晒退实验及与前人的沉积物¹⁴C和光释光测年结果进行比对等, 对将重结晶碳酸盐ESR测年法用于碳酸盐岩基岩区断层和滑坡活动性分析的可行性和可靠性进行分析和论证, 并建立了重结晶碳酸盐ESR测年技术, 该技术可广泛地用于碳酸盐岩基岩区的断层和滑坡活动历史研究。

关键词: ESR测年, 碳酸盐岩, 基岩断层, 滑坡, 重结晶

LIU Chun-ru, YUAN Ren-mao, YIN Gong-ming, JI Hao, WEI Chuan-yi, TIAN Ying-ying, MA Xi, DANG Jia-xiang. APPLICATION PROGRESS OF RECRYSTALLIZED CARBONATE IN THE STUDY OF FAULT AND LANDSLIDE ACTIVITY IN CARBONATE BEDROCK AREA[J]. SEISMOLOGY AND GEOLOGY, 2024, 46(1): 63-80.

刘春茹, 袁仁茂, 尹功明, 姬昊, 魏传义, 田颖颖, 马玺, 党嘉祥. 重结晶碳酸盐ESR年代学在碳酸盐岩基岩区断层和滑坡活动性研究中的应用进展[J]. 地震地质, 2024, 46(1): 63-80.

Figures/Tables 9

Fig. 1 Location of Jianchuan Section of Lijiang-Xiaojinhe Fault and Qiaojia Landslide.

Fig. 2 Carbonate bedrock fault planes and recrystallized carbonate samples in the Jianchuan section of the Lijiang-Xiaojinhe Fault.

Fig. 3 Fault planes and recrystallized carbonate samples of the carbonate bedrock in the Qiaojia landslide.

Fig. 4 Micrograph image of recrystallized carbonate samples on the backsliding surface of the Qiaojia landslide.

Fig. 5 Characteristics of ESR signals of carbonate on the sliding surface of the Jianchuan section, Lijiang-Xiaojinhe Fault.

Fig. 6 Isochronous annealing curve of g=2.000 6 signal in recrystallized carbonate sample S1 on the sliding surface of the rear edge of the Qiaojia landslide(Cited from Liu et al., 2023).

Fig. 7 Instantaneous annealing curve of g=2.000 6 ESR signal of recrystallized carbonate rock on the sliding surface of Funing-Napo Fault(heating time is 5s).

Fig. 8 The bleaching characteristics of recrystallized carbonate sample S1 on the sliding surface of the rear edge of Qiaojia landslide(Cited from Liu et al., 2023).

Fig. 9 Recrystallized carbonates on the Lijiang-Xiaojinhe fault plane in Yunnan in different periods.

References 68

[1]	安芷生, 符淙斌. 2001. 全球变化科学的进展[J]. 地球科学进展, 16(5): 671—680.
	AN Zhi-sheng, FU Cong-bin. 2001. The progress in global change science[J]. Advance in Earth Sciences, 16(5): 671—680 (in Chinese).
[2]	白世彪, 崔鹏, 葛永刚, 等. 2021. 古滑坡测年方法与定年精度的提高途径[J]. 地学前缘, 28(2): 19—34. DOI
	BAI Shi-biao, CUI Peng, GE Yong-gang, et al. 2021. Analysis of geochronology of fossil landslide and improvement ways of dating accuracy[J]. Earth Science Frontiers, 28(2): 19—34 (in Chinese).
[3]	陈以健, 卢景芬, 蔡同茂, 等. 1987. 洞穴次生碳酸盐的ESR年龄测定[J]. 地质评论, 33(4): 339—345.
	CHEN Yi-jian, LU Jing-fen, CAI Tong-mao, et al. 1987. ESR dating of cave secondary carbonates[J]. Geological Review, 33(4): 339—345 (in Chinese).
[4]	丁锐, 任俊杰, 张世民, 等, 2018. 丽江-小金河断裂中段晚第四纪古地震历史[J]. 地震地质, 40(3): 622—640.
	DING Rui, REN Jun-jie, ZHANG Shi-min, et al. 2018. Late Quaternary paleoearthquakes on the middle segment of the Lijiang-Xiaojinhe Fault, southeastern Tibet[J]. Seismology and Geology, 40(3): 622—640 (in Chinese). DOI
[5]	冯振, 吴中海, 曹佳文, 等. 2019. 小江断裂带巧家段巨型古滑坡及其工程地质特征[J/OL]. 地球学报, 40(4): 629—636. http://kns.cnki.net/kcms/detail/11.3474.P.20190124.1354.002.html.
	FENG Zhen, WU Zhong-hai, CAO Jia-wen, et al. 2019. Engineering geological characteristics of gigantic pre-historic landslide along Qiaojia section of the Xiaojiang fault[J/OL]. Acta Geoscientica Sinica, 40(4): 629—636 http://kns.cnki.net/kcms/detail/11.3474.P.20190124.1354.002.html. (in Chinese).
[6]	韩非, 尹功明, 刘春茹, 等. 2012. 中国早更新世考古遗址电子自旋共振-铀系联合法牙齿化石测年问题研究[J]. 第四纪研究, 32(3): 492—498.
	HAN Fei, YIN Gong-ming, LIU Chun-ru, et al. 2012. The combined ESR/U-series dating of fossil tooth from early Pleistocene archaeological sites in China[J]. Quaternary Sciences, 32(3): 492—498 (in Chinese).
[7]	何宏林, 魏占玉, 毕丽思, 等. 2015. 利用基岩断层面形貌定量特征识别古地震: 以霍山山前断裂为例[J]. 地震地质, 37(2): 400—412. DOI
	HE Hong-lin, WEI Zhan-yu, BI Li-si, et al. 2015. Identify paleo-earthquakes using quantitative morphology of bedrock fault surface: A case study on the Houshan piedmont fault[J]. Seismology and Geology, 37(2): 400—412 (in Chinese). DOI
[8]	李建平, 刁少波, 刘春茹, 等. 2015. ESR测年法在海洋碳酸盐岩测年中的应用[J]. 海洋地质前沿, 31(10): 65—70.
	LI Jian-ping, DIAO Shao-bo, LIU Chun-ru, et al. 2015. The application of ESR dating to marine carbonate[J]. Marine Geology Frontiers, 31(10): 65—70 (in Chinese).
[9]	刘星. 1998. 云南石林地区钙华的ESR测年及其地质意义[J]. 中国岩溶, 17(1): 9—14.
	LIU Xing. 1998. ESR dating and its geological significance of travertine in the stone forest, Yunnan Province[J]. Carsologica Sinica, 17(1): 9—14 (in Chinese).
[10]	罗明, 陈杰, 刘进峰. 2017. 岩石暴露与埋藏面释光测年进展及其应用[J]. 地震地质, 39(1): 183—192.
	LUO Ming, CHEN Jie, LIU Jin-feng. 2017. Research progress on luminescence dating of rock surfaces and its application[J]. Seismology and Geology, 39(1): 183—192 (in Chinese). DOI
[11]	冉勇康, 邓起东. 1999. 古地震学研究的历史、现状和发展趋势[J]. 科学通报, 44(1): 12—20.
	RAN Yong-kang, DENG Qi-dong. 1999. History, current situation and development trend of paleoseismology[J]. Chinese Science Bulletin, 44(1): 12—20 (in Chinese).
[12]	任美锷, 刘振中. 1983. 岩溶学概论[M]. 北京: 商务印书馆:1—331.
	REN Mei-e, LIU Zhen-zhong. 1983. Introduction to Karst Science[M]. Commercial Press, Beijing:1—331 (in Chinese).
[13]	王盈. 2019. 金沙江巧家—东川段堰塞湖沉积及滑坡灾害[D]. 北京: 中国地震局地质研究所:44—45.
	WANG ying. 2019. Landslide-dammed lake deposits and landslide hazards in the Qiaojia-Dongchuan section of Jinsha River[D]. Institute of Geology, China Earthquake Administration, Beijing: 44—45 (in Chinese).
[14]	王治华. 1996. 特大规模滑坡遥感调查: 巧家县城滑坡[J]. 环境遥感, 14(4): 280—284.
	WANG Zhi-hua. 1996. Remote sensing investigation for a huge landslide: Qiaojia county landslide[J]. Remote Sensing of Environment, 14(4): 280—284 (in Chinese).
[15]	向宏发, 徐锡伟, 虢顺民, 等. 2002. 丽江-小金河断裂第四纪以来的左旋逆推运动及其构造地质意义: 陆内活动地块横向构造的屏蔽作用[J]. 地震地质, 24(2): 188—198.
	XIANG Hong-fa, XU Xi-wei, GUO Shun-min, et al. 2002. Sinistral thrusting along the Lijiang-Xiaojinhe Fault since Quaternary and its geologic-tectonic significance: Shielding effect of transverse structure of intracontinental active block[J]. Seismology and Geology, 24(2): 188—198 (in Chinese).
[16]	薛传东, 刘星, 杨浩. 2003. 滇中路南石林地区钙华特征与更新世气候变迁[J]. 矿物岩石, 23(3): 61—68.
	XUE Chuan-dong, LIU Xing, YANG Hao. 2003. Travertine character of Lunan stone forest and paleoclimate change in middle Pleistocence in center Yunnan Province[J]. Mineral and Petrology, 23(3): 61—68 (in Chinese).
[17]	业渝光, 和杰, 刁少波, 等, 1990. 西沙石岛风成灰岩的ESR和¹⁴C年龄[J]. 海洋地质与第四纪地质, 10(2): 103—110.
	YE Yu-guang, HE Jie, DIAO Shao-bo, et al. 1990. ¹⁴C and ESR ages of eolian calcarenite from Shidao island of Xisha islands[J]. Marine Geology & Quaternary Geology, 10(2): 103—110 (in Chinese).
[18]	业渝光, 和杰, 刁少波, 等, 1991. 南海全新世珊瑚礁ESR和铀系年龄的研究[J]. 地质评论, 39(2): 165—171.
	YE Yu-guang, HE Jie, DIAO Shao-bo, et al. 1991. ESR and uranium series ages of Holocene coral reefs in the south China Sea[J]. Geological Review, 39(2): 165—171 (in Chinese).
[19]	尹功明, 孙瑛杰, 业渝光, 等. 2001. 大荔人所在层位贝壳的电子自选共振年龄[J]. 人类学报, 20(1): 34—38.
	YIN Gong-ming, SUN Ying-jie, YE Yu-guang, et al. 2001. The ESR age of shells from the bed of Dali with human fossil[J]. Acta Anthropological Sinica, 20(1): 34—38 (in Chinese).
[20]	尹金辉, 杨雪, 郑勇刚. 2016. 基岩就地¹⁴C测年及古地震潜在应用[J]. 地震地质, 38(3): 773—782. DOI
	YIN Jin-hui, YANG Xue, ZHENG Yong-gang. 2016. In-situ ¹⁴C dating of bedrock and potential application of paleoearthquakes[J]. Seismology and Geology, 38(3): 773—782 (in Chinese). DOI
[21]	Bahain J J, Yokoyama Y, Masaoudi H, et al. 1994. Thermal behavior of ESR signal observed in various natural carbonates[J]. Quaternary Geochronology(Quaternary Science Reviews), 13: 671—674.
[22]	Barabas M, Bach A, Mudelsee M, et al. 1992a. General properties of the paramagnetic centre at g=2.000 6 in carbonates[J]. Quaternary Science Reviews, 11: 165—171. DOI URL
[23]	Barabas M, Mudelsee M, Walther R, et al. 1992b. Dose-response and thermal behaviour of the ESR signal at g=2.000 6 in carbonates[J]. Quaternary Science Reviews, 11: 173—179. DOI URL
[24]	Benedetti L, Manighetti I, Gaudemer Y, et al. 2013. Earthquake synchrony and clustering on Fucino faults(Central Italy)as revealed from in situ ³⁶Cl exposure dating[J]. Journal of Geophysical Research: Solid Earth, 118(9): 4948—4974. DOI URL
[25]	Blackwell B A B. 2005. Electron spin resonance(ESR)dating in karst environments[J]. Acta Carsologica, 35(2): 123—153.
[26]	Buhay W M, Schwarcz H P, Grün R. 1988. ESR dating of fault gouge: the effect of grain size[J]. Quaternary Science Reviews, 7(3-4): 515—522. DOI URL
[27]	Burchfiel B C, Chen Z L. 2013. Tectonics of the southeastern Tibetan plateau and its adjacent foreland[C]. Proceedings of Geological Society of America Memoir 210. Geological Society of America:1—164.
[28]	Cowie P A, Phillips R J, Roberts G P, et al. 2017. Orogen-scale uplift in the central Italian Apennines drives episodic behavior of earthquake faults[J]. Scientific Reports, 7: 448—458. DOI
[29]	Debuyst R, Dejehet F, Idrissi S, 1993. Paramagnetic centers in 7-irradiated synthetic monohydrocalcite[J]. Applied Radiation and Isotopes, 44: 293—297. DOI URL
[30]	Fukuchi T, Imai N. 1998. Resetting experiment of E' centers by natural faulting: The case of the Nojima earthquake fault in Japan[J]. Quaternary Science Reviews, 17(11): 1063—1068. DOI URL
[31]	Galli P, Galadini F, Pantosti D. 2008. Twenty years of paleoseismology in Italy[J]. Earth Science Reviews, 88(1-2): 89—117. DOI URL
[32]	Giaccio B, Galadini F, Sposato A, et al. 2003. Image processing and roughness analysis of exposed bedrock fault planes as a tool for paleoseismological analysis: Results from the Campo Felice Fault(central Apennines, Italy)[J]. Geomorphology, 49(3): 281—301. DOI URL
[33]	Handwerger D A, Cerling T E, Bruhn R L. 1999. Cosmogenic ¹⁴C in carbonate rocks[J]. Geomorphology, 27(1): 13—24. DOI URL
[34]	He H L, Wei Z Y, Densmore A. 2016. Quantitative morphology of bedrock fault surfaces and identification of paleo-earthquakes[J]. Tectonophysics, 693: 22—31. DOI URL
[35]	Hennig G J, Grün R. 1983. ESR Dating in Quaternary Geology[J]. Quaternary Science Review, 2: 157—238. DOI URL
[36]	Hennig G J, Herr W, Weber E. 1981. Electron spin resonance(ESR)dating of speleothem of the Caune de l'Arago at Tautavel[G]// Lumley H de, Labeyrie J(eds). Absolute Dating and Isotope Analyses in Prehistory: Methods and Limits: 551—556.
[37]	Hu W, Huang R Q, McSaveney M, et al. 2019. Superheated steam, hot CO₂ and dynamic recrystallization from frictional heat jointly lubricated a giant landslide: Field and experimental evidence[J]. Earth and Planetary Science Letters, 510: 85—93. DOI URL
[38]	Huang X L, Wu Z H, Wu K G. 2018. Surface rupture of the 1515 Yongsheng earthquake in northwest Yunnan, and its seismogeological implications[J]. Acta Geologica Sinica(English Edition), 92(4): 1324—1333.
[39]	Ikeya M. 1977. Electron spin resonance dating and fission track detection of the Petralona stalagmite[J]. Anthropos, 4: 152—168.
[40]	Ikeya M. 1993. New applications of electron spin resonance: Dating, Dosimetry and Microscopy[A]. World Scientific: 1—500.
[41]	Ji H, Liu C R, Zhang P Q. 2022. The upper dating limit of the ESR signal at g=2.000 6 in recrystallized carbonates[J]. Radiation Measurements, 157:106830. DOI URL
[42]	Kong P, Fink D, Na C G, et al. 2010. Dip-slip rate determined by cosmogenic surface dating on a Holocene scarp of the Daju Fault, Yunnan, China[J]. Tectonophysics, 493(1-2): 106—112. DOI URL
[43]	Liu C R, Tian Y Y, Ji H, et al. 2023. Chronology analysis of huge landslide based on ESR dating materials on sliding face in carbonate areas of south eastern Tibet[J]. Quaternary Geochronology, 76:101442. DOI URL
[44]	Liu C R, Yin G M, Zhou Y S, et al. 2014. ESR studies on quartz extracted from shallow fault gouges related to the M_S8.0 Wenchuan earthquake, China: Implications for ESR signal resetting in Quaternary faults[J]. Quaternarie, 25(1): 67—74.
[45]	Mechernich S, Schneiderwind S, Mason J, et al. 2018. The seismic history of the Pisia Fault(eastern Corinth rift, Greece)from fault plane weathering features and cosmogenic ³⁶Cl dating[J]. Journal of Geophysical Research: Solid Earth, 123(5): 4266—4284. DOI URL
[46]	Mitchell S G, Matmon A, Bierman P R, et al. 2001. Displacement history of a limestone normal fault scarp, northern Israel, from cosmogenic ³⁶Cl[J]. Journal of Geophysical Research, 106(B3): 4247—4264. DOI URL
[47]	Molnar P, Tapponnier P. 1975. Cenozoic tectonics of Asia: Effects of a continental collision[J]. Science, 189(4201): 419—426. PMID
[48]	Mouslopoulou V, Moraetis D, Fassoulas C. 2011. Identifying past earthquakes on carbonate faults: Advances and limitations of the ‘Rare Earth Element’ method based on analysis of the Spili Fault, Crete, Greece[J]. Earth and Planetary Science Letters, 309(1-2): 45—55. DOI URL
[49]	Palumbo L, Benedetti L, Bourlès D, et al. 2004. Slip history of the Magnolia Fault(Apennines, Central Italy)from ³⁶Cl surface exposure dating: Evidence for strong earthquakes over the Holocene[J]. Earth and Planetary Science Letters, 225(1-2): 163—176. DOI URL
[50]	Pirouelle F, Bahain J J, Falguères C, et al. 2007. Study of the effect of a thermal treatment on the D_E determination in ESR dating of speleothems[J]. Quaternary Geochronolngy, 2: 386—391.
[51]	Radtke U, Mangini A, Grün R. 1985. ESR dating of marine fossil shells[J]. Nuclear Tracks and Radiation Measurements, 10(4-6): 879—884.
[52]	Rodriguez-Navarro C, Ruiz-Agudo E, Luque A, et al. 2009. Thermal decomposition of calcite: Mechanisms of formation and textural evolution of CaO nanocrystals[J]. American Mineralogist, 94: 578—593. DOI URL
[53]	Schwarcz H P, Grün R, Latham A G, et al. 1988. The Bilzingsleben archaeological site: New dating evidence[J]. Archaeometry, 30(1): 5—17. DOI URL
[54]	Schwartz D P, Coppersmith K J. 1984. Fault behavior and characteristic earthquakes: Examples from the Wasatch and San Andreas fault zones[J]. Journal of Geophysical Research, 89(B7): 5681—5698. DOI URL
[55]	Shasta M M, Fred M P, Marc W C, et al. 2016. CRONUS-Earth cosmogenic ³⁶Cl calibration[J]. Quaternary Geochronology, 31: 199—219. DOI URL
[56]	Shen X M, Li D W, Tian Y T, et al. 2016. Late Pleistocene-Holocene slip history of the Langshan-Seertenshan piedmont fault(Inner Mongolia, northern China)from cosmogenic ¹⁰Be dating on bedrock fault scarp[J]. Journal of Mountain Science, 13(5): 882—890. DOI URL
[57]	Sieh K E. 1980. Lateral offsets and revised dates of large earthquakes at Pallett Creek, California[J]. Journal of Geophysical Research, 89(B9): 7641—7670. DOI URL
[58]	Smith B W, Smart P L, Symons C R. 1985. ESR signals in a variety of speleothem calcites and their suitability for dating[J]. Nuclear Tracks and Radiation Measurements, 10: 837—844.
[59]	Toyoda S, Rink W J, Schwarcz H P, et al. 2000. Crushing effects on TL and OSL on quartz: Relative to fault dating[J]. Radiation Measurements, 32(5-6): 667—672. DOI URL
[60]	Tucker G E, McCoy SW, Whittaker A C, et al. 2011. Geomorphic significance of postglacial bedrock scarps on normal-fault footwalls[J]. Journal of Geophysical Research, 116: F01022.
[61]	Tye A, Stahl T. 2018. Field estimate of paleoseismic slip on a normal fault using the Schmidt hammer and terrestrial LiDAR: Methods and application to the Hebgen Fault(Montana, USA)[J]. Earth Surface Processes and Landforms, 43: 2397—2408. DOI URL
[62]	Vasily A, Susan I O. 2009. How well do we understand production of ³⁶Cl in limestone and dolomite?[J]. Quaternary Geochronology, 4: 462—474. DOI URL
[63]	Wallace R E. 1984. Fault scarps formed during the earthquakes of October 2, 1915, in Pleasant Valley, Nevada, and some tectonic implications [G]. United States Geological Survey Professional Paper, 1274 A: 1—33.
[64]	Wieser A, Göksu H Y, Regulla D F, et al. 1993. ESR and TL dating of travertine from Jordan: Complications in paleodose assessment[J]. ESR Dosimetry and Applications, 44(1-2): 149—152.
[65]	Wu D, Bruhn R L. 1994. Geometry and kinematics of active normal faults, South Oquirrh Mountain, Utah: Implications for fault growth[J]. Journal of Structural Geology, 16(8): 1061—1075. DOI URL
[66]	Yin G M, Liu C R, Yuan R M, et al. 2021. ESR chronology of bedroch fault activity in carbonate area: Preliminary results from the study of the Lijiang-Xiaojinhe Fault, southeastern Tibet, China[J]. Geochronomitrie, 48: 215—221.
[67]	Yokoyama Y, Quaegebeur J P, Bibron R, et al. 1983. ESR dating of Paleolithic calcite: thermal annealing experiment and trapped electron life time[J]. PACT, 9: 371—379.
[68]	Zreda M, Noll J S. 1998. Ages of prehistoric earthquakes revealed by cosmogenic chlorine-36 in a bedrock fault scarp at Hebgen Lake[J]. Science, 282(5391): 1097. PMID