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Izvestiya, Physics of the Solid Earth — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Earth and Planetary Sciences (all) #97 of 186 up up by 7 ranks
Environmental Science (all) #119 of 220 -
journal-quality-icon Journal quality:
Medium
calendar-icon Last 4 years overview: 296 Published Papers | 500 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 03/06/2020
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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.

1.7

13% from 2019

CiteRatio for Izvestiya, Physics of the Solid Earth from 2016 - 2020
Year Value
2020 1.7
2019 1.5
2018 1.3
2017 1.0
2016 0.9
graph view Graph view
table view Table view

0.507

25% from 2019

SJR for Izvestiya, Physics of the Solid Earth from 2016 - 2020
Year Value
2020 0.507
2019 0.405
2018 0.399
2017 0.469
2016 0.329
graph view Graph view
table view Table view

1.054

24% from 2019

SNIP for Izvestiya, Physics of the Solid Earth from 2016 - 2020
Year Value
2020 1.054
2019 0.849
2018 1.123
2017 0.937
2016 0.68
graph view Graph view
table view Table view

insights Insights

  • CiteRatio of this journal has increased by 13% in last years.
  • This journal’s CiteRatio is in the top 10 percentile category.

insights Insights

  • SJR of this journal has increased by 25% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 24% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Izvestiya, Physics of the Solid Earth

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Springer

Izvestiya, Physics of the Solid Earth

Izvestiya, Physics of the Solid Earth (Fizika zemli), founded in 1965, publishes results of original theoretical and experimental research in relevant areas of the physics of the earth's interior and applied geophysics. The journal presents results of studies conducted by rese...... Read More

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Last updated on
02 Jun 2020
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ISSN
1069-3513
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Impact Factor
Medium - 0.618
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Open Access
No
i
Sherpa RoMEO Archiving Policy
Blue faq
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Plagiarism Check
Available via Turnitin
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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/S1069351306080027
Crust and mantle of the Tien Shan from data of the receiver function tomography
Lev Vinnik1, I. M. Aleshin1, Mikhail K. Kaban1, S. G. Kiselev1, Grigoriy Kosarev1, Sergey Oreshin1, Ch. Reigber

Abstract:

A 3-D velocity model of the Tien Shan crust and upper mantle is constructed through the inversion of the receiver functions of P and S waves together with teleseismic traveltime anomalies at nearly 40 local seismic stations. It is found that in the vast central region, where no strong earthquakes have been known over the past... A 3-D velocity model of the Tien Shan crust and upper mantle is constructed through the inversion of the receiver functions of P and S waves together with teleseismic traveltime anomalies at nearly 40 local seismic stations. It is found that in the vast central region, where no strong earthquakes have been known over the past century, the S wave velocity at depths of 10–35 km is lower than in adjacent regions by up to 10%. These data are evidence for mechanical weakness of the crust preventing the accumulation of elastic energy. Apparently, the lower velocity and the weakness of the crust are due to the presence of water. The weakness of the crust is one of the possible reasons for the strain localization responsible for the formation of the present Tien Shan but can also be due in part to the young orogenesis. The crustal thickness is largest (about 60 km) in the Tarim-Tien Shan junction zone. The crust-mantle boundary in this region descends by a jump as a result of an increase in the lower crust thickness. This is probably due to the underthrusting of the Tien Shan by the Tarim lithosphere. This causes the mechanically weak lower crust of the Tarim to delaminate and accumulate in nearly the same way as an accretionary prism during the subduction of oceanic lithosphere. In the upper mantle, the analysis has revealed a low velocity anomaly, apparently related to basaltic outflows of the Upper Cretaceous-Early Paleogene. The Cenozoic Bachu uplift in the northern Tarim depression is also associated with the low velocity anomaly. The Naryn depression is characterized by a high velocity in the upper mantle and can be interpreted as a fragment of an ancient platform. read more read less

Topics:

Oceanic crust (62%)62% related to the paper, Lithosphere (58%)58% related to the paper, Subduction (58%)58% related to the paper, Crust (57%)57% related to the paper, Mantle (geology) (56%)56% related to the paper
62 Citations
open accessOpen access Journal Article
System of electromagnetic field transfer operators for the BEAR array of simultaneous soundings: Methods and results

Abstract:

System of electromagnetic field transfer operators for the BEAR array of simultaneous soundings: Methods and results

Topics:

Electromagnetic field (53%)53% related to the paper
61 Citations
Journal Article DOI: 10.1134/S1069351311040070
Secular geomagnetic variations and volcanic pulses in the Permian-Triassic traps of the Norilsk and Maimecha-Kotui provinces

Abstract:

Detailed paleomagnetic studies have shown that the effusive Permian-Triassic traps in the Kotui River valley were formed as the result of volcanic activity, which occurred in the form of volcanic pulses and individual eruptions with net duration of at most 7000–8000 years, excluding the periods of volcanic quiescence. Accordi... Detailed paleomagnetic studies have shown that the effusive Permian-Triassic traps in the Kotui River valley were formed as the result of volcanic activity, which occurred in the form of volcanic pulses and individual eruptions with net duration of at most 7000–8000 years, excluding the periods of volcanic quiescence. According to the analysis of the paleomagnetic data earlier obtained by Heunemann and his coauthors [2004b] on the Abagalakh and Listvyanka sections in the Norilsk region, those geological units were formed during 25 volcanic pulses and separate eruptions, which all lasted up to 8000 years altogether, whereas the total time of formation (including the periods of volcanic quiescence) exceeded 10000–100000 years for the Norilsk section and was probably a bit shorter for the Kotui section. Comparison of the positions of virtual geomagnetic poles calculated for the Norilsk and the Kotui sections provides no grounds to suggest that these sections were formed at different geological times. The scatter in the positions of the virtual geomagnetic poles (VGP) for the directional groups and individual directions (58 altogether) jointly for the two sections (more than 160 lava flows) indicates that the secular geomagnetic variations at the Permian-Triassic boundary had similar amplitudes to those that occurred in the past 5 Ma. read more read less

Topics:

Geomagnetic pole (54%)54% related to the paper, Lava (54%)54% related to the paper, Volcano (53%)53% related to the paper, Earth's magnetic field (51%)51% related to the paper, Paleomagnetism (51%)51% related to the paper
View PDF
53 Citations
open accessOpen access Journal Article DOI: 10.1134/S1069351308070082
Microseismic field affected by local geological heterogeneities and microseismic sounding of the medium
A. V. Gorbatikov1, M. Yu. Stepanova1, G. E. Korablev1

Abstract:

Experiments and numerical model studies have shown that heterogeneities of the Earth’s crust distort the spectrum of the low frequency microseismic field, decreasing spectral amplitudes of a specific frequency f at the Earth’s surface over high velocity heterogeneities and increasing them above low velocity heterogeneities. T... Experiments and numerical model studies have shown that heterogeneities of the Earth’s crust distort the spectrum of the low frequency microseismic field, decreasing spectral amplitudes of a specific frequency f at the Earth’s surface over high velocity heterogeneities and increasing them above low velocity heterogeneities. The frequency f is connected with the depth of a heterogeneity H and the velocity of the fundamental mode of Rayleigh waves VR(f) through the relation H = 0.5 VR(f)/f. The low frequency microseismic field is considered as the superposition of trains of Rayleigh fundamental modes with different frequency spectra. The paper proposes an experimentally tested technology enabling the determination of the deep structure of complex geological objects using data on the microseismic background field. read more read less

Topics:

Microseism (54%)54% related to the paper, Rayleigh wave (52%)52% related to the paper
View PDF
53 Citations
Journal Article DOI: 10.1134/S1069351314020116
Recognition of earthquake-prone areas: Methodology and analysis of the results
Alexander Soloviev1, A. D. Gvishiani1, Alexander Gorshkov1, M. N. Dobrovolsky1, O. V. Novikova1

Abstract:

We present the results of verifying the areas that were detected as prone to strong earthquakes by the pattern recognition algorithms in different regions of the world with different levels of seismicity and, therefore, different threshold magnitudes demarcating the strong earthquakes The analysis is based on the data present... We present the results of verifying the areas that were detected as prone to strong earthquakes by the pattern recognition algorithms in different regions of the world with different levels of seismicity and, therefore, different threshold magnitudes demarcating the strong earthquakes The analysis is based on the data presented in the catalog of the US National Earthquake Information Center (NEIC) as of August 1, 2012 In each of the regions considered, we examined the locations of the epicenters of the strong earthquakes that occurred in the region after the publication of the corresponding result There were 91 such earthquakes in total The epicenters of 79 of these events (87%) fall in the recognized earthquake-prone areas, including 27 epicenters located in the areas where no strong earthquakes had ever been documented up to the time of publication of the result Our analysis suggests that the results of the recognition of areas prone to strong earthquakes are reliable and that it is reasonable to use these results in the applications associated with the assessment of seismic risks The comparison of the recognition for California with the analysis of seismicity of this region by the Discrete Perfect Sets (DPS) algorithm demonstrates the agreement between the results obtained by these two different methods read more read less

Topics:

Induced seismicity (56%)56% related to the paper
48 Citations
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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 Izvestiya, Physics of the Solid Earth citation style.

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13. What is Sherpa RoMEO Archiving Policy for Izvestiya, Physics of the Solid Earth?

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 Izvestiya, Physics of the Solid Earth. 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 Izvestiya, Physics of the Solid Earth?

The 5 most common citation types in order of usage for Izvestiya, Physics of the Solid Earth 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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