Relevant bibliographies by topics / Gujarat Earthquake

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Gujarat Earthquake'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 January 2023

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Gujarat Earthquake.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Gujarat Earthquake"

1

SRIVASTAVA, H. N., S. N. BHATTACHARYA, D. T. RAO, and S. SRIVASTAVA. "Strange attractor in earthquake swarms near Valsad (Gujarat), India." MAUSAM 58, no. 4 (November 26, 2021): 543–50. http://dx.doi.org/10.54302/mausam.v58i4.1439.

Full text
Abstract:
Valsad district in south Gujarat near the western coast of the peninsular India experienced earthquake swarms since early February 1986. Seismic monitoring through a network of micro earthquake seismographs showed a well concentrated seismic activity over an area of 7 × 10 km2 with the depth of foci extending from 1 to 15 km. A total number of 21,830 earthquakes were recorded during March 1986 to June 1988. The daily frequency of earthquakes for this period was utilized to examine deterministic chaos through evaluation of dimension of strange attractor and Lyapunov exponent. The low dimension of 2.1 for the strange attractor and positive value of the largest Lyapunov exponent suggest chaotic dynamics in Valsad earthquake swarms with at least 3 parameters for earthquake predictability. The results indicate differences in the characteristics of deterministic chaos in intraplate and interplate regions of India.
APA, Harvard, Vancouver, ISO, and other styles
2

Chatterjee, Patralekha. "kutch, gujarat One year after the Gujarat earthquake." Lancet 359, no. 9303 (January 2002): 327. http://dx.doi.org/10.1016/s0140-6736(02)07559-1.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Sharma, Vinod K. "Gujarat earthquake – some emerging issues." Disaster Prevention and Management: An International Journal 10, no. 5 (December 2001): 349–55. http://dx.doi.org/10.1108/09653560110416184.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

RAO, D. T., B. B. JAMBUSARIA, SANJAY SRIVASTAVA, N. P. SRIVASTAVA, ABDUL HAMID, B. N. DESAI, and H. N. SRIVASTAVA. "Earthquake swarm activity in south Gujarat." MAUSAM 42, no. 1 (February 28, 2022): 89–98. http://dx.doi.org/10.54302/mausam.v42i1.3028.

Full text
Abstract:
South Gujarat, a part of western coast of Indian Peninsula started experiencing earth tremors of mild intensity since early February 1986. The shocks were widely felt with rumbling sound in these areas. More than 23000 micro earthquakes have since been recorded tilt December 1988, with a major event, ML=4.6 which occurred on.27 April.1986: In view of the location of multi-purpose projects like Ukai, Damanganga, .Jhuj, Kflia etc the monitoring this activity was Immediately started through a network of seven temporary- microearthquake recording stations. This was followed by various other studies such as geodetic, geomagnatic, radon gas monitoring and temperature measurements 9f hot springs. The Unai and Mola-Amba hot springs situated in this area have indicated the temperature of about 57oC and 37°C respectively against the normal atmospheric temperature of 33o C. The analysis by Hypo- 71 program on IBM computer of India Met. Dep., New Delhi, using a velocity model Koyna region has shown a well concentrated seismic activity over area of 7x 10 km2 and focal depth of 1-15 km. Clear migration of the activity has been observed. The activity which concentrated around Kella dam m early February-April 1986 migrated up to 18km to its south and back again to the religion around Kelia reservoir, by September 1987 with depth of foci progressively becoming shallower towards north .The 'b" value of 1.04 is higher than that of a few tectonic sequences of Peninsular India. The rate of decay of the activity was 0.52 which is rather slow compared to other sequences of the region. Hence, the reactivation of the existing fracturies/lineaments might be responsible or the recent activity. The geomagnetic studies in this area have corroborated tile existence of NW-SE to NNE-SSW trending conductive fractures. The earthquake activity during 1988 is quite low compared to earlier years.
APA, Harvard, Vancouver, ISO, and other styles
5

Vemuri, Jayaprakash, Subramaniam Kolluru, and Sumer Chopra. "Surface Level Synthetic Ground Motions for M7.6 2001 Gujarat Earthquake." Geosciences 8, no. 12 (November 22, 2018): 429. http://dx.doi.org/10.3390/geosciences8120429.

Full text
Abstract:
The 2001 Gujarat earthquake was one of the most destructive intraplate earthquakes ever recorded. It had a moment magnitude of M w 7.6 and had a maximum felt intensity of X on the Modified Mercalli Intensity scale. No strong ground motion records are available for this earthquake, barring PGA values recorded on structural response recorders at thirteen sites. In this paper, synthetic ground motions are generated at surface level using the stochastic finite-fault method. Available PGA data from thirteen stations are used to validate the synthetic ground motions. The validated methodology is extended to various sites in Gujarat. Response spectra of synthetic ground motions are compared with the prescribed spectra based on the seismic zonation given in the Indian seismic code of practice. Ground motion characteristics such as peak ground acceleration, peak ground velocity, frequency content, significant duration, and energy content of the ground motions are analyzed. Response spectra of ground motions for towns situated in the highest zone, seismic zone 5, exceeded the prescribed spectral acceleration of 0.9 g for the maximum considered earthquake. The response spectra for towns in seismic zone 5 exhibit peaks in the low period ranges, indicating high vulnerability of low rise structures designed as per the provisions of the Indian seismic code of practice. The response spectra for towns situated in seismic zone 3 were considerably lower than the prescribed maximum spectral acceleration of 0.4 g. The substantial damage reported in towns situated in seismic zone 3 is due to poor construction practices and non-compliance with provisions of seismic design standards.
APA, Harvard, Vancouver, ISO, and other styles
6

Sharma, R. "Gujarat earthquake causes major mental health problems." BMJ 324, no. 7332 (February 2, 2002): 259c—259. http://dx.doi.org/10.1136/bmj.324.7332.259c.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Sanderson, David, Anshu Sharma, and Juliet Anderson. "NGO permanent housing 10 years after the Gujarat earthquake: revisiting the FICCI–CARE Gujarat rehabilitation programme." Environment and Urbanization 24, no. 1 (April 2012): 233–47. http://dx.doi.org/10.1177/0956247811431218.

Full text
Abstract:
The January 2001 earthquake that struck the state of Gujarat in India damaged or destroyed some 8,000 villages and 490 towns. In the months and years after the earthquake, many organizations undertook widespread reconstruction programmes. One such collaboration between the NGO CARE India and the Federation of Indian Chambers of Commerce and Industry (FICCI) built 5,554 permanent houses as well as schools and community centres in 23 villages. This paper revisits 10 of the 23 villages that were partially or fully rebuilt by FICCI–CARE, 10 years after the earthquake. It finds that while the houses remain structurally strong and are mostly in use, residents’ levels of satisfaction, perception and usage are mixed. A central theme concerns the initial prioritization of seismic safety, which has sacrificed longer-term considerations of comfort, adaptability and the environment. The paper describes the houses that were built and presents findings according to structural condition, engagement in design, adaptations, house selling and perceptions of safety. The discussion presents four issues that emerge from the findings and wider research. The paper ends by proposing a simple equation for good housing, which places people’s involvement in building processes as the vital component.
APA, Harvard, Vancouver, ISO, and other styles
8

Kumar, Sushil, Hiroaki Negishi, Jim Mori, and Tamao Sato. "Role of crustal fluid in triggering moderate to major earthquakes: evidence from aftershock data of two recent large tremors." Journal of Nepal Geological Society 38 (September 25, 2008): 29–38. http://dx.doi.org/10.3126/jngs.v38i0.31479.

Full text
Abstract:
A number of models have been proposed for the role of fluids and high pore pressures in the mechanics of fault slip and the nucleation of earthquakes, e.g., dilatancy-diffusion, mineral dehydration, frictional heating, fluid pressure-activated fault valves and hydrofracturing, partially sealed fault zones, a spatially varying stress tensor without hydrofracturing, and fluid­ involved weak and strong patch failures. In this study, the availability of fluid in the upper and lower crust was analysed carefully, as the fluid may be responsible for triggering large earthquakes. The anomalies observed in the three-dimensional tomographic images from the source regions of the 2001 Gujarat and 1995 Kobe earthquakes, obtained after inversion of aftershock data, can be attributed to the presence of the fluid. A tomographic inversion was also applied to the aftershock data from the 26 January 2001 Bhuj earthquake (Mw 7.7) in the state of Gujarat in western India. We used arrival times from 8,374 P and 7,994 S waves of 1,404 aftershocks recorded on 25 temporary seismic stations. It seems that the aftershock distribution corresponds to the high-velocity anomalies. Low P- to S-wave velocity ratio (Vp/Vs) anomalies are generally found at depths of 10 to 35 km, i.e. the depth range of the aftershock distribution. However, relatively high Vp/Vs and low Vs characterise the deeper region below the hypocentre of the mainshock, at depths of 35 to 45km.This anomaly may be due to a weak fractured and fluid-filled rock matrix, which might have contributed to triggering this earthquake. This anomaly exists in the depth range of 35 to 45 km, and extends 10 to 12 km laterally. This earthquake occurred on a relatively deep and steeply dipping reverse fault with a large stress drop. Similarly, the 17 January 1995 Kobe earthquake (M 7.2) in southwest Japan had a strike-slip focal mechanism and it caused a rupture at a 17 km depth. The Kobe main shock hypocentre is located in a distinctive zone characterised by low P- and S-wave velocities and a high Poisson's ratio. This anomaly exists in a depth range of 16to 21 km, and extends 15to 20km laterally. This anomaly can be attributed to a fluid-filled, fractured rock matrix that contributed to the initiation of the Kobe earthquake. The existence of fluids in and below the seismogenic layer may affect the long-term structural and compositional evolution of the fault zone, change the fault zone strength, and alter the local stress regime. These influences can be exerted through the physical role of fluid pressure and a variety of chemical effects, such as stress corrosion and pressure solution. These influences would have enhanced stress concentration in the seismogenic layer leading to mechanical failure of a strong asperity, and thus may have contributed to the nucleation of the Kobe earthquake. The area of low Vs and high Vp/Vs values can be seen in a depth range of35 to45km beneath the main shock hypocentre. These features are very similar to the velocity anomaly also observed, in a depth range of 16 to 21 km, in the hypocentre region of the1995 Kobe earthquake. Such an anomaly possibly indicates the existence of a fluid-filled, fractured rock matrix, which may have contributed to the initiation of large earthquakes. The fluid in a depth range of35to45km might have also triggered the 200I Gujarat earthquake.
APA, Harvard, Vancouver, ISO, and other styles
9

Shukla, J., and D. Choudhury. "Estimation of seismic ground motions using deterministic approach for major cities of Gujarat." Natural Hazards and Earth System Sciences 12, no. 6 (June 26, 2012): 2019–37. http://dx.doi.org/10.5194/nhess-12-2019-2012.

Full text
Abstract:
Abstract. A deterministic seismic hazard analysis has been carried out for various sites of the major cities (Ahmedabad, Surat, Bhuj, Jamnagar and Junagadh) of the Gujarat region in India to compute the seismic hazard exceeding a certain level in terms of peak ground acceleration (PGA) and to estimate maximum possible PGA at each site at bed rock level. The seismic sources in Gujarat are very uncertain and recurrence intervals of regional large earthquakes are not well defined. Because the instrumental records of India specifically in the Gujarat region are far from being satisfactory for modeling the seismic hazard using the probabilistic approach, an attempt has been made in this study to accomplish it through the deterministic approach. In this regard, all small and large faults of the Gujarat region were evaluated to obtain major fault systems. The empirical relations suggested by earlier researchers for the estimation of maximum magnitude of earthquake motion with various properties of faults like length, surface area, slip rate, etc. have been applied to those faults to obtain the maximum earthquake magnitude. For the analysis, seven different ground motion attenuation relations (GMARs) of strong ground motion have been utilized to calculate the maximum horizontal ground accelerations for each major city of Gujarat. Epistemic uncertainties in the hazard computations are accounted for within a logic-tree framework by considering the controlling parameters like b-value, maximum magnitude and ground motion attenuation relations (GMARs). The corresponding deterministic spectra have been prepared for each major city for the 50th and 84th percentiles of ground motion occurrence. These deterministic spectra are further compared with the specified spectra of Indian design code IS:1893-Part I (2002) to validate them for further practical use. Close examination of the developed spectra reveals that the expected ground motion values become high for the Kachchh region i.e. Bhuj city and moderate in the Mainland Gujarat, i.e. cities of Surat and Ahmedabad. The seismic ground motion level in the Saurashtra is moderate but marginally differs from that as presently specified in IS:1893-Part I (2002). Based on the present study, the recommended PGA values for the cities studied are 0.13 g, 0.15 g, 0.64 g, 0.14 g and 0.2 g for Ahmedabad city, Surat City, Bhuj City, Jamnagar City and Junagadh city, respectively. The prepared spectra can be further used for seismic resistant design of structures within the above major city boundaries of Gujarat to quantify seismic loading on structures.
APA, Harvard, Vancouver, ISO, and other styles
10

Hainzl, S., S. K. Aggarwal, P. K. Khan, and B. K. Rastogi. "Monsoon-induced earthquake activity in Talala, Gujarat, India." Geophysical Journal International 200, no. 1 (January 1, 2014): 627–37. http://dx.doi.org/10.1093/gji/ggu421.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Gujarat Earthquake"

1

Sayegh, Tracy 1976. "Corporate involvement in disaster response and recovery : an analysis of the Gujarat Earthquake." Thesis, Massachusetts Institute of Technology, 2004. http://hdl.handle.net/1721.1/17708.

Full text
Abstract:
Thesis (M.C.P.)--Massachusetts Institute of Technology, Dept. of Urban Studies and Planning, 2004.
Includes bibliographical references (p. 110-114).
Disaster vulnerability is a serious issue in developing countries where globalization, development patterns, poverty and environmental degradation are placing more people at risk to natural disasters. Recent appeals for greater multi-sectoral collaboration to tackle complex disaster situations have raised the need for private sector participation in disaster management. The private sector is already beginning to play more engaged roles in disaster response and recovery on a voluntary basis, yet limited understanding currently exists about their activities in this area. Given the problem of rising vulnerability to natural disasters and the emergence of increased private sector involvement in disaster activities, this thesis seeks to understand: 1) why firms become involved in disaster response and recovery on voluntary (i.e. philanthropic) terms; and 2) the nature and implementation of corporate initiatives in this context. To illustrate private sector motivations and roles in the disaster response and recovery, the study focused on corporate responses to the Gujarat Earthquake in India in 2001. The research was informed by concepts of corporate social responsibility (CSR). The analysis produced three sets of findings, based on in-depth interviews with national and multinational companies which responded to the Gujarat Earthquake. The research indicates that corporations are motivated to become involved in disaster response and recovery based on six organizational factors: social values, disaster sensitivity, internal organization, external pressures, and perceived benefits.
(cont.) These dimensions expand our prior understanding of corporate motivations which focuses primarily on organizational benefits and stakeholder expectations, and introduces the critical influences of social values, commitment to philanthropy, and resource availability and relevancy. The research also identifies differences in the nature of response versus recovery initiatives. In terms of disaster response, companies pursued unilateral disaster response activities, often implementing large-scale, top-down relief and infrastructure-oriented initiatives. Corporations coordinate with the government and leverage their internal resources for response, but do not emphasize community participation in their approach. In contrast, recovery initiatives were focused on participatory, community-oriented reconstruction and livelihood-generating programs. Recovery efforts tended to be structured as formal, collaborative partnerships with NGOs, wherein both parties play complementary roles in implementation. The analysis further reveals the differences between national and multinational corporate efforts in disaster response and recovery.
by Tracy Sayegh.
M.C.P.
APA, Harvard, Vancouver, ISO, and other styles
2

Thiruppugazh, V. "Post-disaster reconstruction : policies, performance and politics ; a comparative study of three states in India." Phd thesis, 2012. http://hdl.handle.net/1885/150774.

Full text
Abstract:
The study compares evidence from the major reconstruction programs undertaken in three states in India after catastrophic disasters: Maharashtra earthquake (1993), Gujarat earthquake (2001) and Asian tsunami in Tamil Nadu (2004). It poses the central question: why, within the same broad political, social, economic and cultural framework, did some reconstruction programs go beyond pre-impact restoration to build back better? I argue that post-disaster reconstruction is a political process in which vision, political leadership, political will and political culture are key ingredients. Reconstruction prescriptions must, therefore, go beyond the technical and embrace the political realm. One of the basic policy dilemmas is the choice between restoration status quo ante and betterment reconstruction. Discussions on the factors that contribute to effective use of post-disaster opportunity have remained largely normative with very little validation through intensive empirical research, particularly in the Indian context. This study has attempted to bridge this gap. This research has identified some of the key factors behind success in "building back better." This has been accomplished using extensive primary data (compiled from household-level surveys, village meetings and interviews), rigorous field visits, archival research, international comparison and personal experience. The study has identified, analyzed and categorized the myriad factors driving the reconstruction programs. The findings emphasize that disaster reconstruction cannot be depoliticized. It finds that the commitment of the State is a critical variable determining the leap forward after a disaster and that vision and political leadership define the scope and role of the State. Since betterment reconstruction is a long-drawn-out process, continued political commitment is needed to go beyond short-term objectives. The evidence indicates that the determinants of political will are not confined to the narrow domain of leadership, but are inseparable from the specific political cultures. The research finds that political culture is an over-arching determinant of policy choices, program implementation and the nature of stakeholder engagement. The study demonstrates that in a country like India, besides the national ethos, the political cultures of different states or even sub-cultures within them shape the larger contours of the reconstruction. This finding underscores the importance of understanding political culture while formulating policy prescriptions and designing programs. The thesis is in three parts. The first examines the recovery after the three disasters in three areas: housing reconstruction, economic transformation and disaster management. The second isolates and analyses key factors behind differential outcomes from the perspective of stakeholders and global literature. The third dwells on reconstruction as a political process.
APA, Harvard, Vancouver, ISO, and other styles

Books on the topic "Gujarat Earthquake"

1

The pain and horror: Gujarat earthquake. New Delhi: A.P.H. Pub. Corp., 2001.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

M, Eidinger John, ed. Gujarat (Kutch) India M7.7 earthquake of January 26, 2001 and Napa M5.2 earthquake of Sept. 3, 2000: Lifeline performance. Reston, Va: American Society of Civil Engineers, 2001.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
3

Duyne, Jennifer E. Housing reconstruction in post-earthquake Gujarat: A comparative analysis. London: Overseas Development Institute, 2006.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

Iyengar, Sudarshan. Rikṭara skela, bhūkampa 2001no dastāveja. Mumbaī: Navabhārata Sāhitya Mandira, 2001.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

Vaux, Tony. Disaster and vulnerability: SEWA's response to the earthquake in Gujarat, summary report. Ahmedabad: Disaster Mitigation Institute with Self Employed Women's Association, 2002.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
6

(Organization), UNNATI, ed. Water & sanitation: Intervention of Oxfam GB - India in Gujarat earthquake 2001. Ahmedabad: Unnati--Organisation for Development Education, 2007.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
7

Geevan, C. P. Water & sanitation: Intervention of Oxfam GB--India in Gujarat earthquake 2001. Ahmedabad: UNNATI-Organisation for Development Education, 2007.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
8

Geevan, C. P. Water & sanitation: Intervention of Oxfam GB--India in Gujarat earthquake 2001. Ahmedabad: UNNATI-Organisation for Development Education, 2007.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
9

Giratī mañzileṃ. Naī Dillī: Samaya Prakāśana, 2005.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
10

Datta, Anupama. Community based disaster preparedness manual: Post Earthquake Reconstruction Project EU Gujarat (PERPEUG). New Delhi: HelpAge India, 2006.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Book chapters on the topic "Gujarat Earthquake"

1

Thakkar, M. G. "Gujarat Earthquake." In Natural Hazards, 1–28. Boca Raton, Florida : Taylor & Francis, 2018. | “A CRC title, part of the Taylor & Francis imprint, a member of the Taylor & Francis Group, the academic division of T&F Informa plc.”: CRC Press, 2018. http://dx.doi.org/10.1201/9781315166841-1.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Thakkar, M. G. "Gujarat Earthquake." In Natural Hazards, 29–48. Boca Raton, Florida : Taylor & Francis, 2018. | “A CRC title, part of the Taylor & Francis imprint, a member of the Taylor & Francis Group, the academic division of T&F Informa plc.”: CRC Press, 2018. http://dx.doi.org/10.1201/9781315166841-2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Tiwari, Asmita. "Capacity Crisis After the 2001 Earthquake in Gujarat, India." In The Capacity Crisis in Disaster Risk Management, 19–29. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09405-2_2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Rastogi, B. K., Kapil Mohan, B. Sairam, A. P. Singh, and Vasu Pancholi. "Geotechnical, Geological and Geophysical Investigations for Seismic Microzonation and Site-Specific Earthquake Hazard Analysis in Gujarat." In Advances in Earthquake Geotechnics, 73–91. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-3330-1_4.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Bhadra, Subhasis. "Failure and Hope: Living or Not with Disability after the 2001 Gujarat Earthquake." In Disability and Disaster, 61–68. London: Palgrave Macmillan UK, 2015. http://dx.doi.org/10.1057/9781137486004_6.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Rihal, Satwant, William Koh, and Anjali Mehrotra. "Seismic Behavior of Historical Royal Cenotaphs (Chhatris) in Gujarat, India During the 2001 Bhuj Earthquake." In Lecture Notes in Civil Engineering, 539–55. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-90788-4_43.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Rastogi, B. K., Pallabee Choudhury, Rakesh Dumka, K. M. Sreejith, and T. J. Majumdar. "Stress Pulse Migration by Viscoelastic Process for Long-Distance Delayed Triggering of Shocks in Gujarat, India, After the 2001 Mw 7.7 Bhuj Earthquake." In Extreme Events and Natural Hazards: The Complexity Perspective, 63–73. Washington, D. C.: American Geophysical Union, 2012. http://dx.doi.org/10.1029/2011gm001061.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Magrin, A., I. A. Parvez, F. Vaccari, A. Peresan, B. K. Rastogi, S. Cozzini, D. Bisignano, et al. "Neo-deterministic Definition of Seismic and Tsunami Hazard Scenarios for the Territory of Gujarat (India)." In Earthquakes and Their Impact on Society, 193–212. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-21753-6_7.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Sahoo, Sushanta Kumar, and Katlamudi Madhusudan Rao. "Assessment of Soil Gas Radon (Rn222) Emission in Kachchh, Gujarat, India: Influence of Meteorological Parameters and Identification of Precursors to Impending Earthquakes." In Lecture Notes in Civil Engineering, 347–63. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-6140-2_28.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

"The Gujarat Earthquake." In Disaster Management and Civil Society. I.B.Tauris, 2006. http://dx.doi.org/10.5040/9780755620210.ch-004.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Gujarat Earthquake"

1

Edwards, Curtis. "Lifeline Damage from the January 26, 2001 M7.7 Gujarat, India Earthquake." In Sixth U.S. Conference and Workshop on Lifeline Earthquake Engineering (TCLEE) 2003. Reston, VA: American Society of Civil Engineers, 2003. http://dx.doi.org/10.1061/40687(2003)32.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Gujarat Earthquake' for particular source types:
Journal articles Books
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography