Example of Journal of Seismology format
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Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format
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Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format Example of Journal of Seismology format
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Journal of Seismology — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Geophysics #58 of 131 down down by 2 ranks
Geochemistry and Petrology #72 of 128 up up by 1 rank
journal-quality-icon Journal quality:
Good
calendar-icon Last 4 years overview: 344 Published Papers | 936 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 01/06/2020
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Related Journals

open access Open Access

Springer

Quality:  
High
CiteRatio: 5.9
SJR: 2.078
SNIP: 1.439
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CiteRatio: 7.5
SJR: 1.78
SNIP: 2.18
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CiteRatio: 7.8
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open access Open Access
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Springer

Quality:  
High
CiteRatio: 11.5
SJR: 1.991
SNIP: 2.319

Journal Performance & Insights

Impact Factor

CiteRatio

Determines the importance of a journal by taking a measure of frequency with which the average article in a journal has been cited in a particular year.

A measure of average citations received per peer-reviewed paper published in the journal.

1.325

11% from 2018

Impact factor for Journal of Seismology from 2016 - 2019
Year Value
2019 1.325
2018 1.494
2017 1.128
2016 1.089
graph view Graph view
table view Table view

2.7

23% from 2019

CiteRatio for Journal of Seismology from 2016 - 2020
Year Value
2020 2.7
2019 2.2
2018 2.1
2017 1.9
2016 2.3
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has decreased by 11% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 23% in last years.
  • This journal’s CiteRatio is in the top 10 percentile category.

SCImago Journal Rank (SJR)

Source Normalized Impact per Paper (SNIP)

Measures weighted citations received by the journal. Citation weighting depends on the categories and prestige of the citing journal.

Measures actual citations received relative to citations expected for the journal's category.

0.52

2% from 2019

SJR for Journal of Seismology from 2016 - 2020
Year Value
2020 0.52
2019 0.532
2018 0.564
2017 0.646
2016 0.627
graph view Graph view
table view Table view

1.008

6% from 2019

SNIP for Journal of Seismology from 2016 - 2020
Year Value
2020 1.008
2019 0.952
2018 1.049
2017 1.081
2016 0.969
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has decreased by 2% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 6% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Journal of Seismology

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Springer

Journal of Seismology

Journal of Seismology is an international journal specialising in all observational and theoretical aspects related to earthquake occurrence. Research topics may cover: seismotectonics, seismicity, historical seismicity, seismic source physics, strong ground motion studies, se...... Read More

Geophysics

Geochemistry and Petrology

Earth and Planetary Sciences

i
Last updated on
01 Jun 2020
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ISSN
1383-4649
i
Impact Factor
High - 1.032
i
Open Access
No
i
Sherpa RoMEO Archiving Policy
Green faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
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Bibliography Name
SPBASIC
i
Citation Type
Author Year
(Blonder et al, 1982)
i
Bibliography Example
Beenakker CWJ (2006) Specular andreev reflection in graphene. Phys Rev Lett 97(6):067,007, URL 10.1103/PhysRevLett.97.067007

Top papers written in this journal

Journal Article DOI: 10.1007/S10950-006-9012-4
Empirical Global Relations Converting M S and m b to Moment Magnitude
Emmanuel M. Scordilis1
22 Apr 2006 - Journal of Seismology

Abstract:

The existence of several magnitude scales used by seismological centers all over the world and the compilation of earthquake catalogs by many authors have rendered globally valid relations connecting magnitude scales a necessity. This would allow the creation of a homogeneous global earthquake catalog, a useful tool for earth... The existence of several magnitude scales used by seismological centers all over the world and the compilation of earthquake catalogs by many authors have rendered globally valid relations connecting magnitude scales a necessity. This would allow the creation of a homogeneous global earthquake catalog, a useful tool for earthquake research. Of special interest is the definition of global relations converting different magnitude scales to the most reliable and useful scale of magnitude, the moment magnitude, MW. In order to accomplish this, a very large sample of data from international seismological sources (ISC, NEIC, HRVD, etc.) has been collected and processed. The magnitude scales tested against MW are the surface wave magnitude, MS, the body wave magnitude, mb, and the local magnitude, ML. The moment magnitudes adopted have been taken from the CMT solutions of HRVD and USGS. The data set used in this study contains 20,407 earthquakes, which occurred all over the world during the time period 1.1.1976–31.5.2003, for which moment magnitudes are available. It is shown that well-defined relations hold between MW and mb and MS and that these relations can be reliably used for compiling homogeneous, with respect to magnitude, earthquake catalogs. read more read less

Topics:

Surface wave magnitude (70%)70% related to the paper, Body wave magnitude (69%)69% related to the paper, Richter magnitude scale (66%)66% related to the paper, Moment magnitude scale (64%)64% related to the paper, Magnitude (mathematics) (55%)55% related to the paper
468 Citations
open accessOpen access Journal Article DOI: 10.1007/S10950-005-9006-7
Criteria for selecting and adjusting ground-motion models for specific target regions: Application to Central Europe and rock sites
Fabrice Cotton1, Frank Scherbaum2, Julian J. Bommer3, Hilmar Bungum4
09 May 2006 - Journal of Seismology

Abstract:

A vital component of any seismic hazard analysis is a model for predicting the expected distribution of ground motions at a site due to possible earthquake scenarios. The limited nature of the datasets from which such models are derived gives rise to epistemic uncertainty in both the median estimates and the associated aleato... A vital component of any seismic hazard analysis is a model for predicting the expected distribution of ground motions at a site due to possible earthquake scenarios. The limited nature of the datasets from which such models are derived gives rise to epistemic uncertainty in both the median estimates and the associated aleatory variability of these predictive equations. In order to capture this epistemic uncertainty in a seismic hazard analysis, more than one ground-motion prediction equation must be used, and the tool that is currently employed to combine multiple models is the logic tree. Candidate ground-motion models for a logic tree should be selected in order to obtain the smallest possible suite of equations that can capture the expected range of possible ground motions in the target region. This is achieved by starting from a comprehensive list of available equations and then applying criteria for rejecting those considered inappropriate in terms of quality, derivation or applicability. Once the final list of candidate models is established, adjustments must be applied to achieve parameter compatibility. Additional adjustments can also be applied to remove the effect of systematic differences between host and target regions. These procedures are applied to select and adjust ground-motion models for the analysis of seismic hazard at rock sites in West Central Europe. This region is chosen for illustrative purposes particularly because it highlights the issue of using ground-motion models derived from small magnitude earthquakes in the analysis of hazard due to much larger events. Some of the pitfalls of extrapolating ground-motion models from small to large magnitude earthquakes in low seismicity regions are discussed for the selected target region. read more read less

Topics:

Seismic hazard (55%)55% related to the paper, Seismic risk (54%)54% related to the paper, Uncertainty quantification (52%)52% related to the paper
View PDF
346 Citations
Journal Article DOI: 10.1023/A:1009758820546
2D and 3D elastic wave propagation by a pseudo-spectral domain decomposition method
Ezio Faccioli1, Fabio Maggio, Roberto Paolucci1, Alfio Quarteroni1
01 Nov 1997 - Journal of Seismology

Abstract:

A new numerical method is presented for propagating elastic waves in heterogeneous earth media, based on spectral approximations of the wavefield combined with domain decomposition techniques. The flexibility of finite element techniques in dealing with irregular geologic structures is preserved, together with the high accura... A new numerical method is presented for propagating elastic waves in heterogeneous earth media, based on spectral approximations of the wavefield combined with domain decomposition techniques. The flexibility of finite element techniques in dealing with irregular geologic structures is preserved, together with the high accuracy of spectral methods. High computational efficiency can be achieved especially in 3D calculations, where the commonly used finite-difference approaches are limited both in the frequency range and in handling strongly irregular geometries. The treatment of the seismic source, introduced via a moment tensor distribution, is thoroughly discussed together with the aspects associated with its numerical implementation. The numerical results of the present method are successfully compared with analytical and numerical solutions, both in 2D and 3D. read more read less

Topics:

Spectral element method (60%)60% related to the paper, Domain decomposition methods (58%)58% related to the paper, Spectral method (56%)56% related to the paper, Mixed finite element method (56%)56% related to the paper, Numerical analysis (55%)55% related to the paper
336 Citations
open accessOpen access Journal Article DOI: 10.1007/S10950-012-9335-2
The SHARE European Earthquake Catalogue (SHEEC) 1000–1899
01 Apr 2013 - Journal of Seismology

Abstract:

In the frame of the European Commission project “Seismic Hazard Harmonization in Europe” (SHARE), aiming at harmonizing seismic hazard at a European scale, the compilation of a homogeneous, European parametric earthquake catalogue was planned. The goal was to be achieved by considering the most updated historical dataset and ... In the frame of the European Commission project “Seismic Hazard Harmonization in Europe” (SHARE), aiming at harmonizing seismic hazard at a European scale, the compilation of a homogeneous, European parametric earthquake catalogue was planned. The goal was to be achieved by considering the most updated historical dataset and assessing homogenous magnitudes, with support from several institutions. This paper describes the SHARE European Earthquake Catalogue (SHEEC), which covers the time window 1000–1899. It strongly relies on the experience of the European Commission project “Network of Research Infrastructures for European Seismology” (NERIES), a module of which was dedicated to create the European “Archive of Historical Earthquake Data” (AHEAD) and to establish methodologies to homogenously derive earthquake parameters from macroseismic data. AHEAD has supplied the final earthquake list, obtained after sorting duplications out and eliminating many fake events; in addition, it supplied the most updated historical dataset. Macroseismic data points (MDPs) provided by AHEAD have been processed with updated, repeatable procedures, regionally calibrated against a set of recent, instrumental earthquakes, to obtain earthquake parameters. From the same data, a set of epicentral intensity-to-magnitude relations has been derived, with the aim of providing another set of homogeneous Mw estimates. Then, a strategy focussed on maximizing the homogeneity of the final epicentral location and Mw, has been adopted. Special care has been devoted also to supply location and Mw uncertainty. The paper focuses on the procedure adopted for the compilation of SHEEC and briefly comments on the achieved results. read more read less

Topics:

Seismic hazard (56%)56% related to the paper
View PDF
287 Citations
Journal Article DOI: 10.1023/A:1009788904007
Ocean-generated microseismic noise located with the Gräfenberg array
A. Friedrich, Frank Krüger1, K. Klinge2
01 Mar 1998 - Journal of Seismology

Abstract:

The main cause for mid-period seismic ground distortions are ocean waves generated by atmospheric disturbances. These act upon the earth through different mechanisms. The microseismic wavefield can be divided into primary (T =12–18 s) and secondary (T = 6–9 s) noise. Classical theory tells that the origin of these induced gro... The main cause for mid-period seismic ground distortions are ocean waves generated by atmospheric disturbances. These act upon the earth through different mechanisms. The microseismic wavefield can be divided into primary (T =12–18 s) and secondary (T = 6–9 s) noise. Classical theory tells that the origin of these induced ground distortions depends on the location and the intensity of the low pressure region. A considerable part of the microseismic wave field reaches the GRF-array in southern Germany with high coherency and almost constant amplitudes. Thus it is possible to locate the generating areas using frequency-wavenumber analysis. Five discrete generating areas for secondary microseisms and three generating areas for primary microseisms could be determined in the Atlantic Ocean, the Arctic Sea and the Mediterranean Sea by investigating broadband continuous recordings over four months in winter 1995/96. An essential result is the long-time constancy of the backazimuths of the coherent part of the microseismic wavefield with respect to the origin areas, independent of the location of the moving low pressure zone. Results from a triangulation using additionally broadband data from the NORSAR-array and an independent estimation of the distance of the source region with water wave dispersion data indicate an origin of the secondary microseismic wavefield near the north-Norwegian coast for the strongest source. The array analysis of a temporary network of ten three-component broadband stations in south-east Germany shows that the ratio of energy between coherent Love and Rayleigh waves is much higher for the primary than for the secondary microseismic noise wavefield. This indicates differences in the source mechanisms. read more read less

Topics:

Microseism (58%)58% related to the paper, Rayleigh wave (51%)51% related to the paper, Wind wave (50%)50% related to the paper
268 Citations
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Absolutely not! Our tool has been designed to help you focus on writing. You can write your entire paper as per the Journal of Seismology guidelines and auto format it.

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3. Can I cite my article in multiple styles in Journal of Seismology?

Of course! We support all the top citation styles, such as APA style, MLA style, Vancouver style, Harvard style, and Chicago style. For example, when you write your paper and hit autoformat, our system will automatically update your article as per the Journal of Seismology citation style.

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Sign up for our free trial, and you'll be able to use all our features for seven days. You'll see how helpful they are and how inexpensive they are compared to other options, Especially for Journal of Seismology.

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Yes. You can choose the right template, copy-paste the contents from the word document, and click on auto-format. Once you're done, you'll have a publish-ready paper Journal of Seismology that you can download at the end.

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12. Is Journal of Seismology's impact factor high enough that I should try publishing my article there?

To be honest, the answer is no. The impact factor is one of the many elements that determine the quality of a journal. Few of these factors include review board, rejection rates, frequency of inclusion in indexes, and Eigenfactor. You need to assess all these factors before you make your final call.

13. What is Sherpa RoMEO Archiving Policy for Journal of Seismology?

SHERPA/RoMEO Database

We extracted this data from Sherpa Romeo to help researchers understand the access level of this journal in accordance with the Sherpa Romeo Archiving Policy for Journal of Seismology. The table below indicates the level of access a journal has as per Sherpa Romeo's archiving policy.

RoMEO Colour Archiving policy
Green Can archive pre-print and post-print or publisher's version/PDF
Blue Can archive post-print (ie final draft post-refereeing) or publisher's version/PDF
Yellow Can archive pre-print (ie pre-refereeing)
White Archiving not formally supported
FYI:
  1. Pre-prints as being the version of the paper before peer review and
  2. Post-prints as being the version of the paper after peer-review, with revisions having been made.

14. What are the most common citation types In Journal of Seismology?

The 5 most common citation types in order of usage for Journal of Seismology are:.

S. No. Citation Style Type
1. Author Year
2. Numbered
3. Numbered (Superscripted)
4. Author Year (Cited Pages)
5. Footnote

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Yes, SciSpace provides this functionality. After signing up, you would need to import your existing references from Word or Bib file to SciSpace. Then SciSpace would allow you to download your references in Journal of Seismology Endnote style according to Elsevier guidelines.

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