Example of Journal of Iberian Geology format
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Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format Example of Journal of Iberian Geology format
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open access Open Access

Journal of Iberian Geology — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Geology #90 of 251 down down by 36 ranks
Stratigraphy #17 of 43 down down by 4 ranks
journal-quality-icon Journal quality:
Good
calendar-icon Last 4 years overview: 133 Published Papers | 384 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 10/06/2020
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Quality:  
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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.

1.233

33% from 2018

Impact factor for Journal of Iberian Geology from 2016 - 2019
Year Value
2019 1.233
2018 0.929
2017 1.302
2016 1.891
graph view Graph view
table view Table view

2.9

45% from 2019

CiteRatio for Journal of Iberian Geology from 2016 - 2020
Year Value
2020 2.9
2019 2.0
2018 2.2
2017 3.3
2016 4.0
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has increased by 33% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 45% 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.

0.593

30% from 2019

SJR for Journal of Iberian Geology from 2016 - 2020
Year Value
2020 0.593
2019 0.455
2018 0.423
2017 0.55
2016 0.704
graph view Graph view
table view Table view

1.017

103% from 2019

SNIP for Journal of Iberian Geology from 2016 - 2020
Year Value
2020 1.017
2019 0.5
2018 0.571
2017 0.696
2016 0.894
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has increased by 30% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 103% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Journal of Iberian Geology

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Springer

Journal of Iberian Geology

Approved by publishing and review experts on SciSpace, this template is built as per for Journal of Iberian Geology formatting guidelines as mentioned in Springer author instructions. The current version was created on and has been used by 266 authors to write and format their manuscripts to this journal.

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Last updated on
09 Jun 2020
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ISSN
1886-7995
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Open Access
Hybrid
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Plagiarism Check
Available via Turnitin
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Endnote Style
Download Available
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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

open accessOpen access Journal Article DOI: 10.5209/JIGE.33882
The lead and copper isotopic composition of copper ores from the Sierra Morena (Spain)
Sabine Klein1, Claude Domergue, Yann Lahaye1, Gerhard P. Brey, H. M. Von Kaenel

Abstract:

The paper presents lead and copper isotope analyses of 51 copper ore samples from the Sierra Morena, South of Spain. They are from ancient mines of the Iberian Peninsula collected by Claude Domergue during various field campaigns in the central Sierra Morena from 1965 to 1975. Most samples consist of copper oxide minerals suc... The paper presents lead and copper isotope analyses of 51 copper ore samples from the Sierra Morena, South of Spain. They are from ancient mines of the Iberian Peninsula collected by Claude Domergue during various field campaigns in the central Sierra Morena from 1965 to 1975. Most samples consist of copper oxide minerals such as malachite, azurite and chrysocolla and stem from the surficial sections of the ore deposits. The aim of the study was to supplement the existing reference data bank on lead isotopic compositions of ancient copper mines from the Iberian Peninsula. This is particularly important for the Sierra Morena for which data exist mostly for lead-zinc but not for copper ores. The lead isotope ratios range from 18.165 to 19.712 (206Pb/204Pb), 0.797 to 0.859 (207Pb/206Pb) and 1.955 to 2.108 (208Pb/206Pb). Two separate fields can be distinguished with a major field intermediate between the ore deposits from SW and SE Spain and a second at higher 208Pb/206Pb values. Copper isotopes were analysed additionally to provide further constraints for provenance studies. The copper isotope ratios δ65Cu of the copper oxide samples are mostly positive and higher on average than those of sulphide minerals. They are a potential tool to distinguish between either sulphide ore or oxide ore deposit derived artefacts. read more read less

Topics:

Azurite (55%)55% related to the paper, Copper oxide (54%)54% related to the paper, Copper (52%)52% related to the paper
87 Citations
open accessOpen access Journal Article DOI: 10.5209/REV_JIGE.2014.V40.N1.44093
Villafranchian large mammals from the Iberian Peninsula: paleobiogeography, paleoecology and dispersal events

Abstract:

The Pleistocene of the Iberian Peninsula is currently a focus of intense paleontological, archaeological and geological research. To a large extent, these inquiries are intended to decipher the ecological factors that might have conditioned early Homo dispersals into the European continent during the late Early Pleistocene. I... The Pleistocene of the Iberian Peninsula is currently a focus of intense paleontological, archaeological and geological research. To a large extent, these inquiries are intended to decipher the ecological factors that might have conditioned early Homo dispersals into the European continent during the late Early Pleistocene. In this respect, the research carried out during the last twenty years in several areas of the Iberian Peninsula (the Guadix-Baza Basin, the Sierra de Atapuerca, the Vallparadis Section and the Banyoles-Besalu Basin) have yielded a large amount of new significant data. Here we review such data and provide for the first time a comprehensive synthesis from a faunal, geologi­cal and paleoecological perspectives, by focusing on the relationship between paleoenvironmental conditions and early human dispersals during the late Early Pleistocene in the Iberian Peninsula. In particular, the Iberian fossil record of Early to Late Villafranchian large mam­mals is synthesized, on the basis of recent publications and unpublished data collected by the authors during the last five years, in order to provide the adequate faunal and paleocological framework for understanding the factors that limited or conditioned human dispersal events. read more read less

Topics:

Early Pleistocene (56%)56% related to the paper, Villafranchian (55%)55% related to the paper, Peninsula (51%)51% related to the paper, Paleoecology (51%)51% related to the paper, Pleistocene (50%)50% related to the paper
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80 Citations
open accessOpen access Journal Article DOI: 10.5209/REV_JIGE.2012.V38.N1.39219
The Quaternary Active Faults Database of Iberia (QAFI v.2.0)

Abstract:

The Quaternary Active Faults Database of Iberia (QAFI) is an initiative lead by the Institute of Geology and Mines of Spain (IGME) for building a public repository of scientific data regarding faults having documented activity during the last 2.59 Ma (Quaternary). QAFI also addresses a need to transfer geologic knowledge to p... The Quaternary Active Faults Database of Iberia (QAFI) is an initiative lead by the Institute of Geology and Mines of Spain (IGME) for building a public repository of scientific data regarding faults having documented activity during the last 2.59 Ma (Quaternary). QAFI also addresses a need to transfer geologic knowledge to practitioners of seismic hazard and risk in Iberia by identifying and characterizing seismogenic fault-sources. QAFI is populated by the information freely provided by more than 40 Earth science researchers, storing to date a total of 262 records. In this article we describe the development and evolution of the database, as well as its internal architecture. Additionally, a first global analysis of the data is provided with a special focus on length and slip-rate fault parameters. Finally, the database completeness and the internal consistency of the data are discussed. Even though QAFI v.2.0 is the most current resource for calculating fault-related seismic hazard in Iberia, the database is still incomplete and requires further review. read more read less
View PDF
80 Citations
open accessOpen access Journal Article DOI: 10.5209/JIGE.33940
Overview of laboratory methods employed for obtaining diffusion coefficients in FEBEX compacted bentonite

Abstract:

Este trabajo describe las principales metodologias empleadas para obtener parametros de difusion en arcillas compactadas, asi como las soluciones analiticas que pueden usarse dependiendo de la configuracion experimental y de las condiciones iniciales y de interaccontorno. Cada metodo tiene diferentes ventajas y limitaciones, ... Este trabajo describe las principales metodologias empleadas para obtener parametros de difusion en arcillas compactadas, asi como las soluciones analiticas que pueden usarse dependiendo de la configuracion experimental y de las condiciones iniciales y de interaccontorno. Cada metodo tiene diferentes ventajas y limitaciones, en funcion del tipo de elemento estudiado: neutro, anionico o cationico. Las especies neutras, como el tritio (HTO), no interactuan con el solido y usan toda la porosidad para el transporte difusivo; los elementos anionicos, como el cloro, tampoco se adsorben, pero sufren exclusion anionica. La difusion de los elementos cationicos se ve retardada por la existencia de sorcion. Para describir como determinar los parametros de difusion (coeficientes de difusion aparente, Da, efectivo, De, y porosidad accesible) se utilizan numerosos ejemplos de ensayos de difusion realizados con la bentonita espanola FEBEX. Se obtuvieron el coeficiente de difusion aparente del tritio, cloruro, yoduro, sulfato, cesio, uranio, estroncio, selenio, renio y europio. Se determino el coeficiente de difusion efectivo del tritio, cloruro, yoduro, sulfato, cesio, uranio, estroncio, selenio, tecnecio, sodio y calcio. Asimismo, se obtuvo la porosidad accesible para el tritio, cloruro, yoduro y sulfato. En particular, el comportamiento frente a la difusion del HTO y Cl-, se estudio en funcion de la densidad seca de la bentonita. Tanto el coeficiente de difusion efectivo como el aparente muestran un descenso exponencial al aumentar la densidad seca, mas pronunciado en el caso del Cl-. Se encontro, que la porosidad accesible para el HTO es igual a la porosidad total. En el caso del cloruro (y otros aniones) solo una muy pequena parte de la porosidad total, a la densidad de compactacion utilizada para un almacenamiento, es accesible al transporte por difusion. En este trabajo se presenta un resumen de todos los resultados experimentales obtenidos con la bentonita FEBEX. read more read less
71 Citations
open accessOpen access Journal Article DOI: 10.5209/REV_JIGE.2012.V38.N1.39203
Active Tectonics of the Pyrenees: a review
Pierre Lacan1, María Ortuño1

Abstract:

The Pyrenees have experienced at least seven earthquakes with magnitude M > 5 in the last 400 years. During the last decades, several seismotectonic, neotectonic and paleoseismological studies have focused on identifying the main active structures of the areas experiencing damaging earthquakes. In spite of these studies, the ... The Pyrenees have experienced at least seven earthquakes with magnitude M > 5 in the last 400 years. During the last decades, several seismotectonic, neotectonic and paleoseismological studies have focused on identifying the main active structures of the areas experiencing damaging earthquakes. In spite of these studies, the regional stress regime is still discussed and there is no unequivocal seismotectonic model at the scale of the range. In this paper, we first present a revision of the former works on active faults in the Pyrenees, and then we discuss the main results in terms of their neotectonic setting. We have distinguished five neotectonic regions according to their seismicity, faulting style and morphologic evolution: the westernmost Pyrenees, the North Western Pyrenean zone, the Foreland basins, the Lower Thrust Sheets Domain and the Eastern Pyrenees. This review lead us to differentiate the range into two major domains: the High Chain, where active faults are controlled by vertical maximum stresses, and the Low Chain, where horizontal maximum stresses of variable orientation seem to be dominant. We propose that these different stress domains are related to the isostatic rebound in response to either the difference in crustal thickness and/or the distribution of the Plio-Quaternary erosion. read more read less

Topics:

Neotectonics (51%)51% related to the paper, Active fault (51%)51% related to the paper, Tectonics (50%)50% related to the paper, Foreland basin (50%)50% related to the paper
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71 Citations
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Frequently asked questions

1. Can I write Journal of Iberian Geology in LaTeX?

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

2. Do you follow the Journal of Iberian Geology guidelines?

Yes, the template is compliant with the Journal of Iberian Geology 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 Iberian Geology?

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 Iberian Geology 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 Iberian Geology.

5. Can I use a manuscript in Journal of Iberian Geology 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 Journal of Iberian Geology that you can download at the end.

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12. Is Journal of Iberian Geology'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 Iberian 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 Journal of Iberian 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 Journal of Iberian Geology?

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

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