Example of Russian Journal of Pacific Geology format
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Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format
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Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format Example of Russian Journal of Pacific Geology format
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Russian Journal of Pacific Geology — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Geophysics #91 of 131 down down by 10 ranks
Stratigraphy #31 of 43 down down by 2 ranks
Geology #182 of 251 down down by 21 ranks
Paleontology #77 of 100 up up by 3 ranks
Oceanography #100 of 128 down down by 6 ranks
Geochemistry and Petrology #106 of 128 down down by 9 ranks
journal-quality-icon Journal quality:
Medium
calendar-icon Last 4 years overview: 164 Published Papers | 163 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 06/06/2020
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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.

0.375

29% from 2018

Impact factor for Russian Journal of Pacific Geology from 2016 - 2019
Year Value
2019 0.375
2018 0.528
2017 0.397
2016 0.427
graph view Graph view
table view Table view

1.0

43% from 2019

CiteRatio for Russian Journal of Pacific Geology from 2016 - 2020
Year Value
2020 1.0
2019 0.7
2018 0.6
2017 0.8
2016 0.8
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has decreased by 29% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 43% 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.

0.425

55% from 2019

SJR for Russian Journal of Pacific Geology from 2016 - 2020
Year Value
2020 0.425
2019 0.274
2018 0.286
2017 0.374
2016 0.381
graph view Graph view
table view Table view

0.883

29% from 2019

SNIP for Russian Journal of Pacific Geology from 2016 - 2020
Year Value
2020 0.883
2019 0.683
2018 0.545
2017 0.59
2016 0.792
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has increased by 55% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 29% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Russian Journal of Pacific Geology

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Springer

Russian Journal of Pacific Geology

Russian Journal of Pacific Geology (Tikhookeanskaya Geologiya) publishes the results of research on the Earth crust and mantle composition, and provides articles on the geological structure and patterns of distribution of mineral deposits in the Pacific Ocean, marginal seas an...... Read More

Stratigraphy

Geophysics

Geology

Oceanography

Palaeontology

Geochemistry and Petrology

Earth and Planetary Sciences

i
Last updated on
06 Jun 2020
i
ISSN
1819-7140
i
Impact Factor
Medium - 0.679
i
Open Access
No
i
Sherpa RoMEO Archiving Policy
Blue faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
i
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: 10.1134/S1819714019030035
Albian–Cenomanian Orogenic Belt and Igneous Province of Pacific Asia
A. I. Khanchuk1, Andrei V. Grebennikov1, V. V. Ivanov1

Abstract:

Geological data and about 300 precision geochronological and geochemical determinations are analyzed to identify the Albian–Cenomanian continental-margin orogenic belt and simultaneous igneous province of Pacific Asia. The orogenic belt represents a newly formed region of continental lithosphere that resulted from the deforma... Geological data and about 300 precision geochronological and geochemical determinations are analyzed to identify the Albian–Cenomanian continental-margin orogenic belt and simultaneous igneous province of Pacific Asia. The orogenic belt represents a newly formed region of continental lithosphere that resulted from the deformation of mainly Jurassic–Early Cretaceous epioceanic terranes. The igneous province is made up of volcanic and intrusive complexes of mostly Albian age, which are syn-orogenic within the belt and post-orogenic beyond it. The igneous rocks include A-, I-, and S-type granitoids; adakites; and VAB- and OIB-type basalts and their intrusive analogues. Both the orogenic belt and the igneous province were formed in a tectonic setting of a transform continental margin between 110 and 95 Ma. The interval of 103–97 Ma became the peak of orogenic and magmatic activity caused by upwelling of the hot asthenospheric mantle through destructed stagnant slabs of the pre-Albian subduction. The Albian–Cenomanian age of the large gold, copper, tungsten, tin, and other ore deposits argues in favor of recognition of the corresponding metallogenic province. The first age data (100–97 Ma) are reported for the granite from the Malmyzh deposit within the Sikhote-Alin Ridge. read more read less

Topics:

Igneous rock (57%)57% related to the paper, Terrane (53%)53% related to the paper, Adakite (53%)53% related to the paper, Basalt (52%)52% related to the paper, Continental margin (52%)52% related to the paper
46 Citations
Journal Article DOI: 10.1134/S1819714007050053
Age and geochemistry of the Early Mesozoic granitoid massifs of the southern Bureya terrane of the Russian Far East
Andrey A. Sorokin1, N. M. Kudryashov1, A. B. Kotov1

Abstract:

A massif of porhyritic microcline biotite granites located in the southern part of the Bureya (Turan) terrane has an age of 185 ± 1 Ma. The granites are characterized by (K2O + Na2O) > 8%, a K2O predominance over Na2O, and a moderately differentiated REE distribution pattern ((La/Yb)n = 14.7–28.5). The obtained age indicates ... A massif of porhyritic microcline biotite granites located in the southern part of the Bureya (Turan) terrane has an age of 185 ± 1 Ma. The granites are characterized by (K2O + Na2O) > 8%, a K2O predominance over Na2O, and a moderately differentiated REE distribution pattern ((La/Yb)n = 14.7–28.5). The obtained age indicates that at least one stage of the Early Mesozoic granitoid magmatism in the Bureya terrane occurred in the Early Jurassic. The formation of early Mesozoic granitoids was presumably related to collision between North Asian and Sino-Korean cratons, and the intervening Amur superterrane, although a subduction origin also cannot be completely ruled out. read more read less

Topics:

Terrane (57%)57% related to the paper, Massif (50%)50% related to the paper
34 Citations
Journal Article DOI: 10.1134/S181971401303007X
Shear structural paragenesis and its role in continental rifting of the East Asian margin
V. P. Utkin1

Abstract:

The spatial-genetic relationships between transit fault systems of the East Asian global shear zone (EAGSZ) are analyzed. It is established that the EAGSZ internal structure between the Okhotsk and South China seas is identical to that of world-known natural and experimental shear zones, which confirms its development as an i... The spatial-genetic relationships between transit fault systems of the East Asian global shear zone (EAGSZ) are analyzed. It is established that the EAGSZ internal structure between the Okhotsk and South China seas is identical to that of world-known natural and experimental shear zones, which confirms its development as an integral structure. The structural-kinematic analysis included the Tan-Lu-Sikhote-Alin (TS) system of left-lateral strike-slip faults (NNE 25°–30°) and the Bohai-Amur (BA) system of updip-strike-slip faults (NE 50°–70°). It is shown that these systems were formed as structural parageneses during two stages. The first and shear-thrust stage (Jurassic-Early Cretaceous) was marked by general NNW-oriented compression with the formation of the TS system of left-lateral strike-slip faults and their structural parageneses (compression structures) such as the BA system of updip-thrusts. The second, strike-slip-pull apart stage (Late Cretaceous-Cenozoic) was characterized by SE-directed tangential compression, which was generated by the SW left-lateral displacement of the continental crust along the Central Sikhote-Alin deep-seated fault. In such dynamic settings, the updip-thrust kinematics of the BA system gave way to that of left-lateral strike-slip faults. The strike-slip faults were formed in the transtension regime (shear with extension), which determined the development of pull-apart structures, where the left-lateral shear extension component played the decisive role. Simultaneously, the extension involved the Tan-Lu strike-slip fault with the formation of the rift valley and the discrete development of sedimentary basins along the latter. read more read less

Topics:

Transtension (62%)62% related to the paper, Shear zone (59%)59% related to the paper, Shear (geology) (58%)58% related to the paper, Rift (54%)54% related to the paper, Sedimentary basin (53%)53% related to the paper
28 Citations
Journal Article DOI: 10.1134/S1819714011040087
Stratigraphy and Structure of the Central East Sakhalin Accretionary Wedge (Eastern Russia)
S. V. Zyabrev1

Abstract:

The East Sakhalin accretionary wedge is a part of the Cretaceous-Paleogene accretionary system, which developed on the eastern Asian margin in response to subduction of the Pacific oceanic plates. Its for� mation was related to the evolution of the Early Cretaceous Kem-Samarga island volcanic arc and Late Cre� taceous-Paleoge... The East Sakhalin accretionary wedge is a part of the Cretaceous-Paleogene accretionary system, which developed on the eastern Asian margin in response to subduction of the Pacific oceanic plates. Its for� mation was related to the evolution of the Early Cretaceous Kem-Samarga island volcanic arc and Late Cre� taceous-Paleogene East Sikhote Alin continentalmargin volcanic belt. The structure, litho�, and biostratig� raphy of the accretionary wedge were investigated in the central part of the East Sakhalin Mountains along two profiles approximately 40 km long crossing the Nabil and Rymnik zones. The general structure of the examined part of the accretionary wedge represents a system of numerous eastvergent tectonic slices. These tectonic slices. tens to hundreds of meters thick. are composed of various siliciclastic rocks, which were formed at the convergent plate boundary, and subordinate oceanic pelagic cherts and basalts, and hemipelagic siliceous and tuffaceous-siliceous mudstones. The siliciclastic deposits include trenchfill mudstones and turbidites and draping sediments. The structure of the accretionary wedge was presumably formed owing to offscraping and tectonic underplating. The offscrape d and tectonically underplated fragments were proba� bly tectonically juxtaposed along outofsequence thrusts with draping deposits. The radiolarian fauna was used to constrain the ages of rocks and time of the accretion episodes in different parts of the accretionary wedge. The defined radiolarian assemblages were correlated with the radiolarian scale for the Tethyan region using the method of unitary associations. In the Nabil zone, the age of pelagic sediments is estimated to have lasted from the Late Jurassic to Early Cretaceous (Barremian); that of hemipelagic sediments, from the early Aptian to middle Albian; and trenchfill and draping depo sits of the accretionary complex date back to the middle-late Albian. In the Rymnik zone, the respective ages of cherts, hemipelagic sediments, and trench facies with draping deposits have been determined as Late Jurassic to Early Cretaceous (middle Albian), mid� dle Aptian-middle Cenomanian, and middle-late Cenomanian. East of the rear toward the frontal parts of the accretionary wedge, stratigraphic boundaries between sediments of different lithology become succes� sively younger. Timing of accretion episodes is based on the age of trenchfill and draping sediments of the accretionary wedge. The accretion occurred in a period lasting from the terminal Aptian to the middle Albian in the western part of the Nabil zone and in the middle Cenomanian in the eastern part of the Rymnik zone. The western part of the Nabil zone accreted synchronously with the Kiselevka-Manoma accretionary wedge located westerward on the continent. These accretionary wedges presumably formed along a single conver� gent plate margin, with the Sakhalin accretionary system located to the south of the Kiselevka-Manoma ter� rane in the Albian. read more read less

Topics:

Accretionary wedge (72%)72% related to the paper, Accretion (geology) (58%)58% related to the paper, Cenomanian (54%)54% related to the paper, Aptian (54%)54% related to the paper, Volcanic arc (53%)53% related to the paper
27 Citations
Journal Article DOI: 10.1134/S1819714010010021
Geochemical Evolution of Middle-Late Cenozoic Magmatism in the Northern Part of the Rio Grande Rift, Western United States
Sergei Rasskazov1, T. A. Yasnygina1, N. N. Fefelov1, E. V. Saranina1

Abstract:

Geochemical studies of the Middle—Late Cenozoic succession of volcanic rocks from the northern part of the Rio Grande Rift were conducted. The initial activation of the rift structure was coeval with voluminous eruptions of lava and pyroclastic material of mainly intermediate and acid compositions in the San Juan volcanic fie... Geochemical studies of the Middle—Late Cenozoic succession of volcanic rocks from the northern part of the Rio Grande Rift were conducted. The initial activation of the rift structure was coeval with voluminous eruptions of lava and pyroclastic material of mainly intermediate and acid compositions in the San Juan volcanic field 35–27 Ma. The composition of the volcanic products after the rifting was dominated by basic and intermediate lavas. It is shown that the basanites and alkali basalts of the territory had geochemical characteristics of sublithospheric slab and above–sl ab sources. The processes of the riftogenic thinning of lithosphere are expressed by geochemical parameters that reflect the interaction between the liquids from the sublithospheric mantle and the rocks from different levels of both the lithospheric mantle and lower crust. In the 35–18 Ma interval, melts of different–depth sublithospheric and lithospheric sources erupted simultaneously in the northern part of the rift. However, the products of interaction between the sublithospheric and lithospheric materials dominated later in the past 15 Ma, although the sublithospheric magmatic liquids erupted at the northern structural termination of the rift within the Yampa volcanic field at about 10 Ma. read more read less

Topics:

Rift (62%)62% related to the paper, Volcanic rock (57%)57% related to the paper, Pyroclastic rock (55%)55% related to the paper, Lava (54%)54% related to the paper, Volcano (53%)53% related to the paper
26 Citations
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13. What is Sherpa RoMEO Archiving Policy for Russian Journal of Pacific Geology?

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 Russian Journal of Pacific Geology. 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 Russian Journal of Pacific Geology?

The 5 most common citation types in order of usage for Russian Journal of Pacific Geology 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 Russian Journal of Pacific Geology Endnote style according to Elsevier guidelines.

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