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

Publisher: Springer
Categories Rank Trend in last 3 yrs
Geophysics #87 of 131 down down by 10 ranks
Geology #168 of 251 down down by 13 ranks
Geochemistry and Petrology #103 of 128 down down by 12 ranks
journal-quality-icon Journal quality:
Medium
calendar-icon Last 4 years overview: 138 Published Papers | 160 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 27/06/2020
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Related Journals

open access Open Access

Springer

Quality:  
Medium
CiteRatio: 1.0
SJR: 0.425
SNIP: 0.883
open access Open Access

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

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Quality:  
High
CiteRatio: 7.8
SJR: 1.51
SNIP: 1.687

Journal Performance & Insights

CiteRatio

SCImago Journal Rank (SJR)

Source Normalized Impact per Paper (SNIP)

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

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.

1.2

14% from 2019

CiteRatio for Journal of Volcanology and Seismology from 2016 - 2020
Year Value
2020 1.2
2019 1.4
2018 1.1
2017 1.0
2016 1.0
graph view Graph view
table view Table view

0.437

4% from 2019

SJR for Journal of Volcanology and Seismology from 2016 - 2020
Year Value
2020 0.437
2019 0.455
2018 0.422
2017 0.318
2016 0.421
graph view Graph view
table view Table view

0.878

36% from 2019

SNIP for Journal of Volcanology and Seismology from 2016 - 2020
Year Value
2020 0.878
2019 1.366
2018 1.221
2017 1.076
2016 0.969
graph view Graph view
table view Table view

insights Insights

  • CiteRatio of this journal has decreased by 14% in last years.
  • This journal’s CiteRatio is in the top 10 percentile category.

insights Insights

  • SJR of this journal has decreased by 4% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has decreased by 36% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Journal of Volcanology and Seismology

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Springer

Journal of Volcanology and Seismology

Journal of Volcanology and Seismology (Vulkanologiya i Seismologiya) publishes theoretical and experimental studies, communications, and reports on volcanic, seismic, geodynamic, and magmatic processes occurring in the areas of island arcs and other active regions of the Earth...... Read More

Geology

Geophysics

Geochemistry and Petrology

Earth and Planetary Sciences

i
Last updated on
27 Jun 2020
i
ISSN
0742-0463
i
Impact Factor
Medium - 0.706
i
Open Access
No
i
Sherpa RoMEO Archiving Policy
Blue faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
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Bibliography Name
SPBASIC
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Citation Type
Author Year
(Blonder et al, 1982)
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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: 10.1134/S074204631001001X
The magmatic system of the Klyuchevskaya group of volcanoes inferred from data on its eruptions, earthquakes, deformation, and deep structure
S. A. Fedotov1, N. A. Zharinov1, L. I. Gontovaya1

Abstract:

The study of magmatic plumbing systems of volcanoes (roots of volcanoes) is one of the main tasks facing volcanology. One major object of this research is the Klyuchevskaya group of volcanoes (KGV), in Kamchatka, which is the greatest such group that has been found at any island arc and subduction zone. We summarize the compr... The study of magmatic plumbing systems of volcanoes (roots of volcanoes) is one of the main tasks facing volcanology. One major object of this research is the Klyuchevskaya group of volcanoes (KGV), in Kamchatka, which is the greatest such group that has been found at any island arc and subduction zone. We summarize the comprehensive research that has been conducted there since 1931. Several conspicuous results derived since the 1960s have been reported, emerging from the study of magma sources, eruptions, earthquakes, deformation, and the deep structure for the KGV. Our discussion of these subjects incorporates the data of physical volcanology relating to the mechanism of volcanic activity and data from petrology as to magma generation. The following five parts can be distinguished in the KGV plumbing system and the associated geophysical model: the source of energy and material at the top of the Pacific Benioff zone at a depth of about 160 km, the region of magma ascent in the asthenosphere, the region of magma storage in the crust-mantle layer at depths of 40–25 km, magma chambers and channelways in the crust, and the bases of volcanic edifices. We discuss and explain the properties of and the relationships between these parts and the mechanisms of volcanic activity and of the KGV plumbing system as they exist today. Methods for calculating magma chambers and conduits, the amount of magma in the system, and its other properties are available. read more read less

Topics:

Magma chamber (65%)65% related to the paper, Magma (61%)61% related to the paper, Volcanic arc (60%)60% related to the paper, Volcanic pipe (60%)60% related to the paper, Island arc (60%)60% related to the paper
70 Citations
Journal Article DOI: 10.1134/S0742046313010028
The system of detailed seismological observations in Kamchatka in 2011

Abstract:

This paper presents the main results from the development of the detailed seismological observation system in Kamchatka and the information on the system as of 2011. We describe the networks of seismological stations, the systems for the acquisition, storage, and processing of seismological observations and their technical, m... This paper presents the main results from the development of the detailed seismological observation system in Kamchatka and the information on the system as of 2011. We describe the networks of seismological stations, the systems for the acquisition, storage, and processing of seismological observations and their technical, methodological, and software support. We discuss the basic characteristics of the recording channels and the system as a whole. We present the information resources of the Kamchatka seismological data bank that provide for basic research in earth sciences. In 2011, the system of seismological observation in Kamchatka was a specialized network for acquisition (recording), storage, transmission, and processing of seismic and geophysical data that provides support for the effective monitoring of seismic and volcanic activities, as well as tsunami warning. read more read less
68 Citations
Journal Article DOI: 10.1134/S0742046316020068
A study of volcanogenic exhalation mineralization
Lidiya P. Vergasova1, Stanislav K. Filatov2

Abstract:

This paper considers volcanogenic exhalation mineralization using data from 35 years of observation of fumarole activity during an earlier phase of the posteruptive activity of the Second Cone, which is one of the New Tolbachik volcanoes that were formed during the eruption at the North Vent of the Great Tolbachik Fissure Eru... This paper considers volcanogenic exhalation mineralization using data from 35 years of observation of fumarole activity during an earlier phase of the posteruptive activity of the Second Cone, which is one of the New Tolbachik volcanoes that were formed during the eruption at the North Vent of the Great Tolbachik Fissure Eruption (Kamchatka, 1975–1976). We describe the main types of mineral associations, identify the key mineral species and the secondary and accessory minerals, as well as the sequence of mineral generation. We provide a summary of minerals and compounds that have been identified in ejecta of fumaroles on the Second Cone. read more read less

Topics:

Fumarole (52%)52% related to the paper
View PDF
56 Citations
Journal Article DOI: 10.1134/S0742046312050053
New Mineral Species in Products of Fumarole Activity of the Great Tolbachik Fissure Eruption
Lidiya P. Vergasova1, Stanislav K. Filatov2

Abstract:

A summary is given and some physical properties and chemistry are described for new natural compounds of seven different classes from the deposits of fumaroles of the Great Tolbachik Fissure Eruption (1975–1976, Kamchatka), which were determined on the basis of mineralogical and crystal chemistry studies A summary is given and some physical properties and chemistry are described for new natural compounds of seven different classes from the deposits of fumaroles of the Great Tolbachik Fissure Eruption (1975–1976, Kamchatka), which were determined on the basis of mineralogical and crystal chemistry studies read more read less

Topics:

Fumarole (51%)51% related to the paper
43 Citations
Journal Article DOI: 10.1134/S0742046314050029
The first quantitative estimates of parameters for the Tolbachik Fissure Eruption of 2012–2013 from aerophotogrammetric observations
Viktor N. Dvigalo1, I. Yu. Svirid1, A. V. Shevchenko1

Abstract:

This paper presents quantitative estimates of parameters for the Tolbachik Fissure Eruption of 2012–2013 (TFE) for the period between November 27, 2012 and June 5, 2013. It is shown that the eruption was the most violent during the first 2 days (with a mean lava discharge rate of 440 m3/s), when the maximum number of lava ven... This paper presents quantitative estimates of parameters for the Tolbachik Fissure Eruption of 2012–2013 (TFE) for the period between November 27, 2012 and June 5, 2013. It is shown that the eruption was the most violent during the first 2 days (with a mean lava discharge rate of 440 m3/s), when the maximum number of lava vents were active along the entire fissured zone. The rate was decreasing during the subsequent 2 weeks (the mean was 140 m3/s). Lava effusion had been occurring at an almost uniform rate at near 18 m3/s from the later half of December 2012 to June 2013. The eruption was predominantly effusive in character. Six months of activity yielded 0.52 km3 lava to cover an area of 35.23 km2. The volume of pyroclastics within 1.5 km of the new fissured zone did not exceed 0.1 km3. We made maps to show the location of the fissured zone, the main vents, and lava flows on the slope of Ploskii Tolbachik Volcano. It was found that the 1975–1976 collapse pit in the smaller summit caldera of Ploskii Tolbachik has been left nearly intact during the Tolbachik Fissure Eruption of 2012–2013. read more read less

Topics:

Effusive eruption (67%)67% related to the paper, Lava (59%)59% related to the paper, Volcano (52%)52% related to the paper
36 Citations
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Frequently asked questions

1. Can I write Journal of Volcanology and Seismology in LaTeX?

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2. Do you follow the Journal of Volcanology and Seismology guidelines?

Yes, the template is compliant with the Journal of Volcanology and Seismology guidelines. Our experts at SciSpace ensure that. If there are any changes to the journal's guidelines, we'll change our algorithm accordingly.

3. Can I cite my article in multiple styles in Journal of Volcanology and 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 Volcanology and Seismology citation style.

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12. Is Journal of Volcanology and 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 Volcanology and 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 Volcanology and 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 Volcanology and Seismology?

The 5 most common citation types in order of usage for Journal of Volcanology and 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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16. Can I download Journal of Volcanology and Seismology in Endnote format?

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 Volcanology and Seismology Endnote style according to Elsevier guidelines.

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