Example of Geological Magazine format
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Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format
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Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format Example of Geological Magazine format
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Geological Magazine — Template for authors

Categories Rank Trend in last 3 yrs
Geology #61 of 251 down down by 15 ranks
journal-quality-icon Journal quality:
High
calendar-icon Last 4 years overview: 408 Published Papers | 1694 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 20/06/2020
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Related Journals

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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.

2.365

5% from 2018

Impact factor for Geological Magazine from 2016 - 2019
Year Value
2019 2.365
2018 2.49
2017 2.341
2016 1.965
graph view Graph view
table view Table view

4.2

9% from 2019

CiteRatio for Geological Magazine from 2016 - 2020
Year Value
2020 4.2
2019 4.6
2018 4.2
2017 4.1
2016 3.8
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has decreased by 5% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has decreased by 9% 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.

0.935

27% from 2019

SJR for Geological Magazine from 2016 - 2020
Year Value
2020 0.935
2019 1.28
2018 1.074
2017 0.966
2016 0.876
graph view Graph view
table view Table view

1.026

19% from 2019

SNIP for Geological Magazine from 2016 - 2020
Year Value
2020 1.026
2019 1.259
2018 1.028
2017 0.95
2016 0.879
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has decreased by 27% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has decreased by 19% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Geological Magazine

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Cambridge University Press

Geological Magazine

Geological Magazine, established in 1864, is one of the oldest and best-known periodicals in the Earth Sciences. Its worldwide circulation, broad scope and high production values keep the journal at the forefront of the field. It publishes original papers, review articles, rap...... Read More

Geology

Earth and Planetary Sciences

i
Last updated on
20 Jun 2020
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ISSN
0016-7568
i
Impact Factor
High - 1.067
i
Open Access
No
i
Sherpa RoMEO Archiving Policy
Green faq
i
Plagiarism Check
Available via Turnitin
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Endnote Style
Download Available
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Bibliography Name
unsrt
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Citation Type
Numbered
[25]
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Bibliography Example
G E Blonder, M Tinkham, and T M Klapwijk. Transition from metallic to tunneling regimes in superconducting microconstrictions: Excess current, charge imbalance, and supercurrent conversion. Phys. Rev. B, 25(7):4515–4532, 1982. 10.1103/PhysRevB.25.4515.

Top papers written in this journal

Journal Article DOI: 10.1017/S0016756800059987
The Mechanics of Oblique Slip Faulting
Martin Harold Phillips Bott1
01 Mar 1959 - Geological Magazine

Abstract:

The various mechanisms which could cause oblique slip faulting are briefly reviewed. It is thought that such faulting may frequently arise from the existence of preferred planes of fracture within the rocks. The dynamics of this mechanism is studied in some detail and an expression is obtained for the first direction of slip ... The various mechanisms which could cause oblique slip faulting are briefly reviewed. It is thought that such faulting may frequently arise from the existence of preferred planes of fracture within the rocks. The dynamics of this mechanism is studied in some detail and an expression is obtained for the first direction of slip within the plane under the influence of a general stress system of given orientation it is found that the initial slip may occur in any possible direction within the plane, the direction depending on the relative values of the three principle pressures. The theory suggests that when a pre-existing fault is subjected to a reorientated stress system (typical or rotated) the movement after fracture will usually be oblique. In conclusion, the general implications of the theory are discussed. read more read less

Topics:

Slip (materials science) (69%)69% related to the paper, Plane stress (51%)51% related to the paper, Stress intensity factor (51%)51% related to the paper, Oblique case (50%)50% related to the paper
View PDF
1,036 Citations
Journal Article DOI: 10.1017/S0016756800022330
The origins of granulites: a metamorphic perspective
Simon L. Harley1
01 May 1989 - Geological Magazine

Abstract:

Although many recent reviews emphasize a uniformity in granulite pressure–temperature (P–T) conditions and paths, granulites in reality preserve a spectrum of important petrogenetic features which indicate diversity in their modes of formation. A thorough survey of over 90 granulite terranes or occurrences reveals that over 5... Although many recent reviews emphasize a uniformity in granulite pressure–temperature (P–T) conditions and paths, granulites in reality preserve a spectrum of important petrogenetic features which indicate diversity in their modes of formation. A thorough survey of over 90 granulite terranes or occurrences reveals that over 50% of them record P–T conditions outside the 7.5 ± 1 kbar and 800 ± 50 °C average granulite regime preferred by many authors. In particular, an increasing number of very high temperature (900−1000 °C) terranes are being recognized, both on the basis of distinctive mineral assemblages and geothermobarometry. Petrogenetic grid and geothermobarometric approaches to the determination and interpretation of P–T histories are both evaluated within the context of reaction textures to demonstrate that the large range in P–T conditions is indeed real, and that both near-isothermal decompression (ITD) and near-isobaric cooling (IBC) P–T paths are important. Amphibolite–granulite transitions promoted by the passage of CO2-rich fluids, as observed in southern India and Sri Lanka, are exceptional and not representative of fluid-related processes in the majority of terranes. It is considered, on the contrary, that fluid-absent conditions are typical of most granulites at or near the time of their recorded thermal maxima.ITD granulites are interpreted to have formed in crust thickened by collision, with magmatic additions being an important extra heat source. Erosion alone is not, however, considered to be the dominant post-collisional thinning process. Instead, the ITD paths are generated during more rapid thinning (1−2 mm/yr exposure) related to tectonic exhumation during moderate-rate or waning extension. IBC granulites may have formed in a variety of settings. Those which show anticlockwise P–T histories are interpreted to have formed in and beneath areas of voluminous magmatic accretion, with or without additional crustal extension. IBC granulites at shallow levels (< 5 kbar) may also be formed during extension of normal thickness crust, but deeper-level IBC requires more complex models. Many granulites exhibiting IBC at deep crustal levels may have formed in thickened crust which underwent very rapid (5 mm/yr) extensional thinning subsequent to collision. It is suggested that the preservation of IBC paths rather than ITD paths in many granulites is primarily related to the rate and timescale of extensional thinning of thickened crust, and that hybrid ITD to IBC paths should also be observed.Most IBC granulites, and probably many ITD granulites, have not been exposed at the Earth's surface as a result of the tectonic episodes which produced them, but have resided in the middle and lower crust for long periods of time (100−2000 Ma) following these events. The eventual exhumation of most granulite terranes only occur through their incorporation in later tectonic and magmatic events unrelated to their formation. read more read less

Topics:

Granulite (58%)58% related to the paper, Ultra-high-temperature metamorphism (52%)52% related to the paper, Terrane (50%)50% related to the paper, Geothermobarometry (50%)50% related to the paper
View PDF
932 Citations
open accessOpen access Journal Article DOI: 10.1017/S001675681100046X
Zagros orogeny: a subduction-dominated process
01 Nov 2011 - Geological Magazine

Abstract:

This paper presents a synthetic view of the geodynamic evolution of the Zagros orogen within the frame of the Arabia-Eurasia collision. The Zagros orogen and the Iranian plateau preserve a record of the long-standing convergence history between Eurasia and Arabia across the Neo-Tethys, from subduction/obduction processes to p... This paper presents a synthetic view of the geodynamic evolution of the Zagros orogen within the frame of the Arabia-Eurasia collision. The Zagros orogen and the Iranian plateau preserve a record of the long-standing convergence history between Eurasia and Arabia across the Neo-Tethys, from subduction/obduction processes to present-day collision (from ~ 150 to 0 Ma). We herein combine the results obtained on several geodynamic issues, namely the location of the oceanic suture zone, the age of oceanic closure and collision, the magmatic and geochemical evolution of the Eurasian upper plate during convergence (as testified by the successive Sanandaj-Sirjan, Kermanshah and Urumieh-Dokhtar magmatic arcs), the P-T-t history of the few Zagros blueschists, the convergence characteristics across the Neo-Tethys (kinematic velocities, tomographic constraints, subduction zones and obduction processes), together with a survey of recent results gathered by others. We provide lithospheric-scale reconstructions of the Zagros orogen from ~ 150 to 0 Ma across two SW-NE transects. The evolution of the Zagros orogen is also compared to those of the nearby Turkish and Himalayan orogens. In our geotectonic scenario for the Zagros convergence, we outline three main periods/regimes: (1) the Mid to Late Cretaceous (115-85 Ma) corresponds to a distinctive period of perturbation of subduction processes and interplate mechanical coupling marked by blueschist exhumation and upper-plate fragmentation, (2) the Paleocene-Eocene (60-40 Ma) witnesses slab break-off, major shifts in arc magmatism and distributed extension within the upper plate, and (3) from the Oligocene onwards (~ 30-0 Ma), collision develops with a progressive SW migration of deformation and topographic build-up (Sanandaj-Sirjan Zone: 20-15 Ma, High Zagros: ~12-8 Ma; Simply Folded Belt: 5-0 Ma) and with partial slab tear at depths (~10 Ma to present). Our reconstructions underline the key role played by subduction throughout the whole convergence history. We finally stress that such a long-lasting subduction system with changing boundary conditions also makes the Zagros orogen an ideal natural laboratory for subduction processes. read more read less

Topics:

Zagros fold and thrust belt (61%)61% related to the paper, Subduction (56%)56% related to the paper, Obduction (53%)53% related to the paper, Eclogitization (53%)53% related to the paper, Orogeny (52%)52% related to the paper
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781 Citations
Journal Article DOI: 10.1017/S0016756800101256
Geological Society of London
01 Mar 1920 - Geological Magazine

Abstract:

CONTENTS. Introduction. Generic distinctions and nomenclature of the Prohoscidea. Dinotherium. Mastodon and Elephas. The distinctive and specific characters of Mastodon and Elephas. The British fossil Mastodon, and its comparison with M. angustideas, M. ~4rvernen~, and M. longiroslris. Mastodon angustidens. M. .4rvernensis an... CONTENTS. Introduction. Generic distinctions and nomenclature of the Prohoscidea. Dinotherium. Mastodon and Elephas. The distinctive and specific characters of Mastodon and Elephas. The British fossil Mastodon, and its comparison with M. angustideas, M. ~4rvernen~, and M. longiroslris. Mastodon angustidens. M. .4rvernensis and M. longirostris. British specimens of Mastodon. Molars. Premolars. Milk-molars. Lower jaw. Geological age of the Mastodons. Mastodon angustideus, M. longirostris, and M. [lrvernensis. Mastodon of the Crag, in particular. Conclusion. read more read less
707 Citations
Journal Article DOI: 10.1017/S0016756800008244
Climatic and oceanographic isotopic signals from the carbonate rock record and their preservation
Jim D. Marshall1
01 Mar 1992 - Geological Magazine

Abstract:

Stable isotopic data from marine limestones and their constituent fossils and marine cements can provide quantitative evidence for changes in global climate and ocean circulation. Oxygen isotopic data can indicate changes in temperature and ocean composition whereas stratigraphic variation in carbon isotope ratios may reflect... Stable isotopic data from marine limestones and their constituent fossils and marine cements can provide quantitative evidence for changes in global climate and ocean circulation. Oxygen isotopic data can indicate changes in temperature and ocean composition whereas stratigraphic variation in carbon isotope ratios may reflect changes in the carbon cycle that can be linked to changes in oceanic productivity and atmospheric greenhouse gases. Terrestrial carbonates–meteoric cements, calcretes and speleothems–similarly offer significant potential for understanding the evolution of terrestrial climates by providing evidence for the composition of rainwater and the nature of vegetative cover.Primary environmental isotopic signals may be obscured by the effects of post-depositional diagenetic alteration. Cementation and replacement reactions can take place in a wide range of diagenetic environments; the diagenetic history of an individual limestone is determined by a combination of its mineralogical diagenetic potential and depositional setting, together with subsequent changes in relative sea-level and burial history. Carbon isotopic values are less prone to alteration during diagenesis than oxygen values but shifts can be significant where organogenic carbon is incorporated. Linear covariation of carbon and oxygen values is not a reliable indicator of diagenetic alteration: water-rock interaction and fluid mixing may produce non-linear distributions.Attempts to determine long-term changes in climatic and oceanographie conditions through isotope stratigraphy of shallow-water limestones must include an assessment of the diagenetic history of the materials analysed. Petrographic examination using conventional microscopy backed up, where appropriate, by cathodoluminescence and scanning electron microscopy together with elemental and strontium isotopic analysis can help to identify the effects of diagenetic alteration. Where material with a range of different degrees of alteration is preserved in the same sediment it may be possible to compare patterns of isotopic and elemental variation and to attempt to unravel the effects of diagenesis in order to determine primary, environmental, isotopic signals. Recent research has shown that these techniques can be successfully employed in both Phanerozoic and Precambrian sediments. read more read less

Topics:

Isotope analysis (55%)55% related to the paper, Diagenesis (52%)52% related to the paper
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630 Citations
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Geological Magazine format uses unsrt citation style.

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Frequently asked questions

1. Can I write Geological Magazine in LaTeX?

Absolutely not! Our tool has been designed to help you focus on writing. You can write your entire paper as per the Geological Magazine guidelines and auto format it.

2. Do you follow the Geological Magazine guidelines?

Yes, the template is compliant with the Geological Magazine 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 Geological Magazine?

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 Geological Magazine citation style.

4. Can I use the Geological Magazine templates for free?

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 Geological Magazine.

5. Can I use a manuscript in Geological Magazine that I have written in MS Word?

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 Geological Magazine that you can download at the end.

6. How long does it usually take you to format my papers in Geological Magazine?

It only takes a matter of seconds to edit your manuscript. Besides that, our intuitive editor saves you from writing and formatting it in Geological Magazine.

7. Where can I find the template for the Geological Magazine?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Geological Magazine's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

8. Can I reformat my paper to fit the Geological Magazine's guidelines?

Of course! You can do this using our intuitive editor. It's very easy. If you need help, our support team is always ready to assist you.

9. Geological Magazine an online tool or is there a desktop version?

SciSpace's Geological Magazine is currently available as an online tool. We're developing a desktop version, too. You can request (or upvote) any features that you think would be helpful for you and other researchers in the "feature request" section of your account once you've signed up with us.

10. I cannot find my template in your gallery. Can you create it for me like Geological Magazine?

Sure. You can request any template and we'll have it setup within a few days. You can find the request box in Journal Gallery on the right side bar under the heading, "Couldn't find the format you were looking for like Geological Magazine?”

11. What is the output that I would get after using Geological Magazine?

After writing your paper autoformatting in Geological Magazine, you can download it in multiple formats, viz., PDF, Docx, and LaTeX.

12. Is Geological Magazine'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 Geological Magazine?

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 Geological Magazine. 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 Geological Magazine?

The 5 most common citation types in order of usage for Geological Magazine are:.

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

15. How do I submit my article to the Geological Magazine?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Geological Magazine's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

16. Can I download Geological Magazine 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 Geological Magazine Endnote style according to Elsevier guidelines.

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