Seismic source characteristics in Kachchh and Saurashtra regions of Western India: b-value and fractal dimension mapping of aftershock sequences
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Abstract
Seismic source characteristics in the Kachchh rift basin and Saurashtra horst tectonic blocks in the stable continental region (SCR) of western peninsular India are studied using the earthquake catalog data for the period 2006–2011 recorded by a 52-station broadband seismic network known as Gujarat State Network (GSNet) running by Institute of Seismological Research (ISR), Gujarat. These data are mainly the aftershock sequences of three mainshocks, the 2001 Bhuj earthquake (M w 7.7) in the Kachchh rift basin, and the 2007 and 2011 Talala earthquakes (M w ≥ 5.0) in the Saurashtra horst. Two important seismological parameters, the frequency–magnitude relation (b-value) and the fractal correlation dimension (D c) of the hypocenters, are estimated. The b-value and the D c maps indicate a difference in seismic characteristics of these two tectonic regions. The average b-value in Kachchh region is 1.2 ± 0.05 and that in the Saurashtra region 0.7 ± 0.04. The average D c in Kachchh is 2.64 ± 0.01 and in Saurashtra 2.46 ± 0.01. The hypocenters in Kachchh rift basin cluster at a depth range 20–35 km and that in Saurashtra at 5–10 km. The b-value and D c cross sections image the seismogenic structures that shed new light on seismotectonics of these two tectonic regions. The mainshock sources at depth are identified as lower b-value or stressed zones at the fault end. Crustal heterogeneities are well reflected in the maps as well as in the cross sections. We also find a positive correlation between b- and D c-values in both the tectonic regions.
Keywords
Mainshock Aftershocks b-value Fractal dimension Seismotectonics HeterogeneityNotes
Acknowledgments
We sincerely acknowledge Dr. B. K. Rastogi, Director General, Institute of Seismological Research (ISR), Gujarat, for his encouragement, support and kind permission to publish this work. The author IGR extends gratefulness to the Director General for his kind invitation to the ISR as a Visiting Fellow and for providing necessary support and hospitality during his stay at the institute.
References
- Aki K (1965) Maximum likelihood estimate of b in the formula log N = a−b M and its confidence limits. Bull Earth Res Inst Univ Tokyo 43:237–239Google Scholar
- Aki K (1981) A probabilistic synthesis of precursory phenomena, in earthquake prediction. In: Simpson DW, Richards PG (eds) An international review, Maurice Ewing Set, vol 4. AGU, Washington, pp 566–574Google Scholar
- Anderson RN, Hasegawa A, Umeno N, Takagi A (1980) Phase changes and frequency magnitude distribution in the upper plate of deep seismic beneath Tohoku, Japan. J Geophys Res 85:1389–1398CrossRefGoogle Scholar
- Bender B (1983) Maximum likelihood estimation of b-values for magnitude grouped data. Bull Seismol Soc Am 73:831–851Google Scholar
- Bhattacharya SN, Karanth RV, Dattatrayam RS, Sohoni PS (2004) Earthquake sequence in and around Bhavnagar, Saurashtra, western India during August–December 2000 and associated tectonic features. Curr Sci 86:1165–1170Google Scholar
- BIS (2004) Seismic zoning map of India. Bureau Indian Standard (BIS), New DelhiGoogle Scholar
- Biswas SK (1987) Regional framework, structure and evaluation of the western marginal basins of India. Tectonophysics 135:307–327CrossRefGoogle Scholar
- Biswas SK (2005) A review of structure and tectonics of Kutch Basin, western India with special reference to earthquakes. Curr Sci 88:1592–1600Google Scholar
- Bridges DL, Gao SS (2006) Spatial variation of seismic b-values beneath Makushin Volcano, Unalaska Island, Alaska. Earth Planet Sci Lett 245:408–415CrossRefGoogle Scholar
- Chandra R (1995) Geochemistry and petrogenesis of layered sequence in Girnar ijolitic series (GIS), India: The role of differentiation and allied factors. In: Srivastava RK, Chandra R (eds) Magmatism in Relation to Diverse Tectonic Settings. Oxford and IBH, New DelhiGoogle Scholar
- Chandrasekhar DV, Singh B, Firozishah Md, Mishra DC (2005) Analysis of Gravity and Magnetic anomalies of Kachchh rift basin, India and its comparison with New Madrid seismic zone, USA. Curr Sci 8:1601–1608Google Scholar
- Chandrasekhar E, Mathew G, Harinarayana T (2012) A new hypothesis for the deep subsurface structures near Bhuj 2001 earthquake (M w 7.6) hypocenter zone and tectonic implications. Geophys J Int 190:761–768CrossRefGoogle Scholar
- Chen CC, Wang WC, Chang YF, Wu YM, Lee YH (2006) A correlation between b-value and fractal dimension from aftershock sequence of the 1999 Chi–Chi Taiwan earthquake. Geophys J Int 167:1215–1219Google Scholar
- Dimri VP, Vedanti N, Chattopadhyay S (2005) Fractal analysis of aftershock sequence of the Bhuj earthquake: a wavelet-based approach. Curr Sci 88:1617–1620Google Scholar
- Gangopadhyay A, Talwani P (2003) Symptomatic features of intraplate earthquakes. Seismol Res Lett 74:863–883Google Scholar
- Gerstenberger M, Wiemer S, Giardini D (2001) A systematic test of the hypothesis that the b-value varies with depth in California. Geophys Res Lett 28:57–60CrossRefGoogle Scholar
- Grassberger P, Procaccia I (1983) Characterization of strange attractors. Phys Rev Lett 50:346–349CrossRefGoogle Scholar
- GSI (2003) Kutch (Bhuj) Earthquake 26 January, 2001. In: Pande P, Kayal JR (eds) Geol Surv India, Spl Pub, 76, 282 p Google Scholar
- Guo Z, Ogata Y (1995) Correlations between characteristic parameters of aftershock distributions in time space and magnitude. Geophys Res Lett 22:993–996Google Scholar
- Gupta HK, Rastogi BK (1976) Dams and earthquakes. Elsevier, AmsterdamGoogle Scholar
- Gutenberg B, Richter CF (1944) Frequency of earthquakes in California. Bull Seismol Soc Am 34:185–188Google Scholar
- Gutenberg B, Richter CF (1954) Seismicity of the earth and associated phenomena, 2nd edn. Princeton Press, PrincetonGoogle Scholar
- Hirata T (1989) A correlation between the b value and the fractal dimension of earthquakes. J Geophys Res 94:7507–7514CrossRefGoogle Scholar
- Ishimoto M, Iida K (1939) Observations of earthquakes registered with the microseismograph constructed recently. Bull Earthq Res Inst 17:443–478Google Scholar
- Kagan YY (1991) Fractal dimension of brittle fracture. J Nonlinear Sci 1:1–16Google Scholar
- Kagan YY, Knopoff L (1978) Statistical study of the occurrence of shallow earthquakes. Geophys J R Astron Soc 55:67–86CrossRefGoogle Scholar
- Kagan YY, Knopoff L (1980) Spatial distribution of earthquakes: the two point correlation function. Geophys J R Astron Soc 62:303–320CrossRefGoogle Scholar
- Kayal JR (2008) Microearthquake seismology and seismotectonics of South Asia. Springer, GermanyGoogle Scholar
- Kayal JR, De R, Sagina R, Srirama BV, Gaonkar SG (2002a) Aftershocks of the 26 January, 2001 Bhuj earthquake in western India and its seismotectonic implications. J Geol Soc Ind 59:395–417Google Scholar
- Kayal JR, Zhao D, Mishra OP, De R, Singh OP (2002b) The 2001 Bhuj earthquake: tomographic evidence for fluids at the hypocenter and its implications for rupture nucleation. Geophys Res Lett 29:2152CrossRefGoogle Scholar
- Kayal JR, Das V, Ghosh U (2012) An appraisal of the 2001 Bhuj Earthquake (Mw 7.7, India) source zone: fractal dimension and b-value mapping of the aftershock sequence. Pure Appl Geophys 169:2127–2138Google Scholar
- Khattri KN (1995) Fractal description of seismicity of India and inferences regarding earthquake hazard. Curr Sci 69:361–366Google Scholar
- King G (1983) The accommodation of large strains in the upper lithosphere of the earth and other solids by selfsimilar fault systems: The geometrical origin of b value. Pure Appl Geophys 121:761–815Google Scholar
- Kumar N, Yadav DK, Mondal SK, Roy PNS (2013) Stress drop and its relation to tectonic and structural elements for the meizoseismal region of great 1905 Kangra earthquake of the NW Himalaya. Nat Hazards. doi: 10.1007/s11069-013-0793-9 Google Scholar
- Lee WHK, Lahr JC (1975) HYPO71 (revised): a computer program for determining hypocenter magnitude and first motion pattern of local earthquakes. USGS Open-File Rep 116:75–311Google Scholar
- Mandal P (2012) Seismogenesis of the uninterrupted occurrence of the aftershock activity in the 2001 Bhuj earthquake zone, Gujarat, India, during 2001–2010. Nat Hazards 65:1063–1083Google Scholar
- Mandal P, Rastogi BK (2005) Self-organized fractal seismicity and b-value of aftershocks of the 2001 Bhuj earthquake in Kutch (India). Pure Appl Geophys 162:53–72CrossRefGoogle Scholar
- Mandal P, Rastogi BK, Satyanarayana HVS, Kousalya M, Vijayraghavan R, Satyamurty C, Raju IP, Sarma ANS, Kumar N (2004a) Characterization of the causative fault system for the 2001 Bhuj aftershocks of Mw 7.7. Tectonophysics 378:105–121Google Scholar
- Mandal P, Rastogi BK, Satyanarayana HVS, Kousalya M (2004b) Results from local earthquake velocity Tomography: implications toward the source process involved in generating the 2001 Bhuj earthquake in the lower crust beneath Kachchh (India). Bull Seismol Soc Am 94:633–649CrossRefGoogle Scholar
- Mandal P, Chadha RK, Raju IP, Kumar N, Satyamurty C, Narsaiah R, Maji A (2007) Coulomb static stress variations in the Kachchh Gujarat, India; Implications for the occurrences of two recent earthquakes (Mw = 5.6) in the 2001 Bhuj earthquake region. Geophys J Int 169:281–285CrossRefGoogle Scholar
- Merh SS (1995) Geology of Gujarat. Geol Soc Ind, pp 222Google Scholar
- Mishra OP, Zhao D (2003) Crack density saturation rate and porosity at the 2001 Bhuj, India, earthquake hypocenter: a fluid driven earthquake?. Earth Planet Sci Lett 212:393–405Google Scholar
- Mogi K (1962) Magnitude-frequency relation for elastic shocks accompanying fractures of various materials and some related problems in earthquakes. Bull Earth Res Inst Univ Tokyo 40:831–853Google Scholar
- Monterroso D, Kulhanek O (2003) Spatial variations of b-values in the subduction zone of Central America. Geofisica Int 42:1–13Google Scholar
- Naini BR, Kolla V (1982) Tectonics and sedimentation along the continental margin of western India, Pakistan and adjacent Arabian Sea. Am As Petrol Geol Bull 66:611 (Abstract)Google Scholar
- Nanjo K, Nagahama H (2000) Spatial distribution of aftershock and fractal structure of active fault systems. Pure Appl Geophys 157:575–588CrossRefGoogle Scholar
- Pande P (2013) Geoseismological investigation of the January 26, 2001 Bhuj earthquake in western peninsular India. Nat Hazards 65:1045–1062CrossRefGoogle Scholar
- Paul DK, Potts PJ, Rex DC, Beckinsale RD (1977) Geochemical and petrogenetic study of the Girnar igneous complex, Deccan volcanic province, India. Bull Geol Soc Am 88:227–234CrossRefGoogle Scholar
- Rajendran K, Rajendran CP (1999) Seismogenesis in the stable continental interiors: an appraisal based on two examples from India. Tectonophysics 305:355–370CrossRefGoogle Scholar
- Rajendran CP, Rajendran K (2001) Characteristics of deformation and past seismicity associated with the the 1819 Kutch earthquake, Northwestern India. Bull Seismol Soc Am 91:407–426Google Scholar
- Rajendran K, Rajendran CP, Thakkar M, Tuttle MP (2001) The 2001 Kutch (Bhuj) earthquake: coseismic surface features and their significance. Curr Sci 80:1397–1405Google Scholar
- Ram A, Roy PNS (2005) Fractal dimensions of blocks using a box-counting technique for the 2001 Bhuj earthquake, Gujarat, India. Pure Appl Geophys 162:531–548CrossRefGoogle Scholar
- Ramasamy SM (1995) Deformation tectonics of Deccan volcanics of southern Saurashtra, India and its relation to western extension of Narmada lineament. In: Srivastava RK, Chandra R (eds) Magmatism related to diverse tectonic settings. Oxford and IBH Pub. Co., New DelhiGoogle Scholar
- Rao BR (2000) Historical seismicity and deformation rates in Indian Peninsular Shields. J Seismol 4:247–258CrossRefGoogle Scholar
- Rao BR, Rao PS (1984) Historical seismicity of peninsular India. Bull Seismol Soc Am 74:2519–2533Google Scholar
- Rastogi BK, Chopra S, Gadhvi MS, Patel H, Aggarwal S, Sairam B, Gupta AK, Chauhan M., Bhatt KM (2008) Investigation of magnitude 5.0 Talala earthquake of November 6, 2007 in Junagadh District. Technical Report ISR-2008-11Google Scholar
- Roy PNS, Nath SK (2007) Precursory correlation dimensions for three great earthquakes. Curr Sci 93(11):1522–1529Google Scholar
- Roy PNS, Ram A (2006) A correlation integral approach to the study of 26 January 2001 Bhuj earthquake, Gujarat India. J Geodyn 41:385–399CrossRefGoogle Scholar
- Sadovskiy MA, Golubeva TV, Pisarenko VF, Shnirman MG (1984) Characteristic dimensions of rock and hierarchical properties of seismicity. Izv Acad Sci USSR Phys Solid Earth 20:87–96Google Scholar
- Scholz CH (1968) The frequency-magnitude relation of microfracturing in rock and its relation to earthquakes. Bull Seismol Soc Am 58:399–415Google Scholar
- Schorlemmer D, Wiemer S, Wyss M (2005) Variations in earthquake-size distribution across different stress regimes. Nature 437:539–542Google Scholar
- Seth HC, Choudhary AK, Cucciniello C, Bhattacharyya S, Laishramb R, Gurav T (2012) Geology, petrochemistry, and genesis of the bimodal lavas of Osham Hill, Saurashtra, northwestern Deccan Traps. J Asian Earth Sci 43(1):176–192CrossRefGoogle Scholar
- Shi Y, Bolt BA (1982) The standard error of the magnitude-frequency b value. Bull Seismol Soc Am 72:1677–1687Google Scholar
- Singh AP (2013) Three dimensional seismic structure and Seismotectonics of Kachchh, Gujarat, India: implications for seismic Hazard. Ph.D. thesis, Department of Geophysics, Kurukshetra University, Haryana, India, pp 187Google Scholar
- Singh AP, Mishra OP, Rastogi BK, Kumar D (2011) 3-D seismic structure of the Kachchh, Gujarat and its implications for the earthquake hazard mitigation. Nat Hazards 57:83–105CrossRefGoogle Scholar
- Singh AP, Mishra OP, Kumar D, Kumar S, Yadav RBS (2012) Spatial variation of the aftershock activity across the Kachchh Rift Basin and its seismotectonic implications. J Earth Syst Sci 121:439–451CrossRefGoogle Scholar
- Singh AP, Mishra OP, Rastogi BK, Kumar S (2013) Crustal heterogeneities beneath the 2011 Talala, Saurashtra earthquake, Gujarat, India source zone: seismological evidence for neo-tectonics. J Asian Earth Sci 62:672–684CrossRefGoogle Scholar
- Talwani P, Gangopadhyay A (2001) Tectonic framework of the Kachchh earthquake of 26 January 2001. Seismol Res Lett 72:336–345Google Scholar
- Turcotte DL (1986) A fractal model for crustal deformation. Tectonophys 132:261–269Google Scholar
- Urbancic TI, Trifu CI, Long JM, Young RP (1992) Space-time correlations of b-values with stress release. Pure Appl Geophys 139:449–462CrossRefGoogle Scholar
- Utsu T (1965) A method for determining the value of b in a formula log N (M) = a − b M showing the magnitude frequency for earthquakes. Geophys Bull Hokkaido Univ 13:99–103Google Scholar
- Veeraswamy KM, Azeez KKA, Mohan K, Gupta AK, Devi S, Harinarayana T, Rastogi BK (2013) Electrical conductivity structure beneath the Wagad uplift inferred from magnetotellurics, International Symposium on Advances in Earthquake Sciences, AES-2013 at the Institute of Seismological Research, Gandhinagar, Gujarat, India 1–2 February, 2013, pp 58Google Scholar
- Wiemer S (2001) A software package to analyze seismicity ZMAP. Seismol Res Lett 72:373–382CrossRefGoogle Scholar
- Wiemer S, Benoit J (1996) Mapping the b value anomaly at 100 km depth in the Alaska and New Zealand subduction zones. Geophys Res Lett 23:1557–1560CrossRefGoogle Scholar
- Wiemer S, Wyss M (1997) Mapping the frequency-magnitude distribution in asperities: an improved technique to calculate recurrence times? J Geophys Res 102:15115–15128CrossRefGoogle Scholar
- Wiemer S, Wyss M (2002) Mapping spatial variability of the frequency-magnitude distribution of earthquakes. Adv Geophys 45:259–302CrossRefGoogle Scholar
- Wyss M (1973) Towards a physical understanding of the earthquake frequency distribution. Geophys J R Astron Soc 31:341–359CrossRefGoogle Scholar
- Wyss M, Pacchiani F, Deschamps A, Patau G (2008) Mean magnitude variations of earthquakes as a function of depth: different crustal stress distribution depending on tectonic setting. Geophys Res Lett 35:L01307. doi: 10.1029/2007GL031057 CrossRefGoogle Scholar
- Wyss M, Sammis CG, Nadeau RM, Wiemer S (2004) Fractal dimension and b–value on creeping and locked patches of the San-Andreas fault near Parkfield, California. Bull Seismol Soc Am 94:410–421Google Scholar
- Yadav RBS, Papadimitriou EE, Karakostas VG, Shanker D, Rastogi BK, Chopra S, Singh AP, Kumar S (2011) The 2007 Talala, Saurashtra, Western India earthquake sequence: tectonic implications and seismicity triggering. J Asian Earth Sci 40:303–314Google Scholar