Example of Carbonates and Evaporites format
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Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format Example of Carbonates and Evaporites format
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Carbonates and Evaporites — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Geochemistry and Petrology #93 of 128 down down by 12 ranks
journal-quality-icon Journal quality:
Medium
calendar-icon Last 4 years overview: 362 Published Papers | 588 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 07/07/2020
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Related Journals

open access Open Access

Springer

Quality:  
High
CiteRatio: 5.9
SJR: 2.078
SNIP: 1.439
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SJR: 1.78
SNIP: 2.18
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open access Open Access
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SJR: 1.991
SNIP: 2.319

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.

1.6

23% from 2019

CiteRatio for Carbonates and Evaporites from 2016 - 2020
Year Value
2020 1.6
2019 1.3
2018 1.4
2017 1.3
2016 0.9
graph view Graph view
table view Table view

0.309

6% from 2019

SJR for Carbonates and Evaporites from 2016 - 2020
Year Value
2020 0.309
2019 0.329
2018 0.327
2017 0.334
2016 0.206
graph view Graph view
table view Table view

0.727

7% from 2019

SNIP for Carbonates and Evaporites from 2016 - 2020
Year Value
2020 0.727
2019 0.781
2018 0.622
2017 0.638
2016 0.467
graph view Graph view
table view Table view

insights Insights

  • CiteRatio of this journal has increased by 23% in last years.
  • This journal’s CiteRatio is in the top 10 percentile category.

insights Insights

  • SJR of this journal has decreased by 6% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has decreased by 7% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Carbonates and Evaporites

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Springer

Carbonates and Evaporites

Established in 1979, the international journal Carbonates and Evaporites provides a forum for the exchange of concepts, research and applications on all aspects of carbonate and evaporite geology. This includes the origin and stratigraphy of carbonate and evaporite rocks and i...... Read More

Geochemistry and Petrology

Earth and Planetary Sciences

i
Last updated on
06 Jul 2020
i
ISSN
0891-2556
i
Impact Factor
Low - 0.471
i
Open Access
No
i
Sherpa RoMEO Archiving Policy
Green 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: 10.1007/BF03176484
Eogenetic karst from the perspective of an equivalent porous medium
H. L. Vacher1, John E. Mylroie2

Abstract:

The porosity of young limestones experiencing meteoric diagenesis in the vicinity of their deposition (eogenetic karst) is mainly a double porosity consisting of touching-vug channels and preferred passageways lacing through a matrix of interparticle porosity. In contrast, the porosity of limestones experiencing subaerial ero... The porosity of young limestones experiencing meteoric diagenesis in the vicinity of their deposition (eogenetic karst) is mainly a double porosity consisting of touching-vug channels and preferred passageways lacing through a matrix of interparticle porosity. In contrast, the porosity of limestones experiencing subaerial erosion following burial diagenesis and uplift (telogenetic karst) is mainly a double porosity consisting of conduits within a network of fractures. The stark contrast between these two kinds of karst is illustrated by their position on a graph showing the hydraulic characteristics of an equivalent porous medium consisting of straight, cylindrical tubes (n-D space, where n is porosity,D is the diameter of the tubes, and logn is plotted against logD). Studies of the hydrology of small carbonate islands show that large-scale, horizontal hydraulic conductivity (K) increases by orders of magnitude during the evolution of eogenetic karst. Earlier petrologic studies have shown there is little if any change in the total porosity of the limestone during eogenetic diagenesis. The limestone of eogenetic karst, therefore, tracks horizontally inn-D space. In contrast, the path from initial sedimentary material to telogenetic karst comprises a descent on the graph with reduction ofn during burial diagenesis, then a sideways shift with increasingD due to opening of fractures during uplift and exposure, and finally an increase inD andn during development of the conduits along the fractures. Eogenetic caves are mainly limited to boundaries between geologic units and hydrologic zones: stream caves at the contact between carbonates and underlying impermeable rocks (and collapse-origin caves derived therefrom); vertical caves along platform-margin fractures; epikarst; phreatic pockets (banana holes) along the water table; and flank margin caves that form as mixing chambers at the coastal freshwater-saltwater “interface”. In contrast, the caverns of telogenetic karst are part of a system of interconnected conduits that drain an entire region. The eogenetic caves of small carbonate islands are, for the most part, not significantly involved in the drainage of the island. read more read less

Topics:

Karst (57%)57% related to the paper, Diagenesis (52%)52% related to the paper
240 Citations
Journal Article DOI: 10.1007/BF03175390
Geochemical and neomorphic alteration of dolomite: A review
S. J. Mazzullo1

Abstract:

Many ancient dolomites are suspected of being alteration products of preexisting dolomite phases rather than being originally formed, unaltered dolomites Such diagenetic alteration commonly results in changes in geochemistry and/or neomorphic changes in dolomite crystal sizes and textures Hence, previous studies that have int... Many ancient dolomites are suspected of being alteration products of preexisting dolomite phases rather than being originally formed, unaltered dolomites Such diagenetic alteration commonly results in changes in geochemistry and/or neomorphic changes in dolomite crystal sizes and textures Hence, previous studies that have interpreted environments of initial dolomitization based on presumed preservation of diagnostic geochemical compositions and textures must be reevaluated because these parameters ar known to reequilibrate during later diagenesis The principal driving forces for neomorphism are the inherent thermodynamic instability of preexisting, non-stoichiometric dolomites, and to an unknown extent, the surface free energy-driven recrystallization of fine crystalline mosaics to coarser crystalline textures The four inter-related criteria that are used commonly as collective evidence of alternation of preexisting dolomites are: (1)) non-stoichiometric and poorly-ordered dolomites have an inherent tendency to transform to the more stoichiometric and better ordere phase typical of many ancient dolomites, a process that commonly is concurrent with (2) the neomorphic change from fine crystalline to coarse crystalline mosaics of either planar or nonplanar texture; (3) based on comparison to modern dolomites, depletion in18O isotopic composition and Sr and Na concentrations relative to ppresumed preexisting phases; and (4) homogenization of primary cathodoluminescent zonation that may have been present in the preexisting phase Although certainly not unequivocal, the inference or recognition of such changes suggest the complexity of diagenetic modifications that have affected many ancient dolomites read more read less

Topics:

Neomorphism (53%)53% related to the paper, Dolomitization (52%)52% related to the paper, Recrystallization (geology) (51%)51% related to the paper
183 Citations
Journal Article DOI: 10.1007/S13146-017-0341-X
Synthesis of precipitated calcium carbonate: a review
Onimisi A. Jimoh1, Kamar Shah Ariffin1, Hashim Hussin1, Adesuji Elijah Temitope2

Abstract:

The current high global demand for high-quality paper, paint, adhesive/sealant, and plastic, filler industries cannot survive without unique and high-quality precipitated calcium carbonate (PCC). They are used as fillers, additives, and reinforcements. PCC is a key constituent of the modern paper and plastic industry. This ar... The current high global demand for high-quality paper, paint, adhesive/sealant, and plastic, filler industries cannot survive without unique and high-quality precipitated calcium carbonate (PCC). They are used as fillers, additives, and reinforcements. PCC is a key constituent of the modern paper and plastic industry. This article reports the effect of various organic and inorganic additives used in the synthesis of the different polymorph of calcium carbonate. The use of precipitated calcium carbonate fillers is the recommended choice in enhancing optical properties, durability, smoothness and ink adsorption in papermaking and improving the mechanical properties of plastic. PCC can best be synthesized using solid–liquid route or the gas–solid–liquid carbonation route, which consists of bubbling gaseous CO2 through a concentrated calcium hydroxide (Ca(OH)2) and/or calcium magnesium hydroxide (Ca·Mg(OH)2) slurry with suitable organic additives. The use of several organic and synthetic additives in conjunction with different reaction parameters for the synthesis of the various polymorph of precipitated calcium carbonate is reported. Depending on the desired end use, PCC polymorphs such as aragonite, vaterite and calcite are vital in the plastic and rubber industries. read more read less

Topics:

Calcium carbonate (61%)61% related to the paper, Vaterite (59%)59% related to the paper, Calcium hydroxide (57%)57% related to the paper, Calcite (55%)55% related to the paper, Aragonite (53%)53% related to the paper
116 Citations
Journal Article DOI: 10.1007/BF03175104
Relationships between sulphate reduction and oxidation of organic compounds to carbonate diagenesis, hydrocarbon accumulations, salt domes, and metal sulphide deposits
Hans G. Machel1

Abstract:

The association of dissolved sulphate species and organic compounds generally is thermodynamically unstable in diagenetic environments. Unless kinetically inhibited, reduction-oxidation reactions take place between dissolved sulphate and organic compounds. These reactions take place bacterially at temperatures up to about 85°... The association of dissolved sulphate species and organic compounds generally is thermodynamically unstable in diagenetic environments. Unless kinetically inhibited, reduction-oxidation reactions take place between dissolved sulphate and organic compounds. These reactions take place bacterially at temperatures up to about 85°C (equivalent to vitrinite reflectance of approximately 0.2–0.3% RO) and abiologically/thermochemically at temperatures in excess of about 100–135°C (equivalent to vitrinite reflectance of approximately >1.5% RO). Thereby, sulphate is reduced to sulphide (in the form of H2S, HS−, and S2−) and to elemental sulphur, and organic compounds are oxidized to solid bitumen, bicarbonate, and/or carbon dioxide. A number of minerals may precipitate if the respective cations are available in sufficient amounts: these include calcite, dolomite, siderite, ankerite, pyrite, sphalerite, galena, and other minerals. Secondary and tertiary porosity, as well as solution-collapse brecciation, may occur due to the dissolution of solid sulphates and/or carbonates. Products of redox-reactions between sulphate and organic compounds are nearly ubiquitous in nature. In particular, hydrocarbon accumulations, salt domes, and several types of metal sulphide deposits (e.g. Mississippi-Valley-Type, base metal sulphide, and roll-type uranium deposits) are related genetically through these redox-reactions. Most commonly the reaction products occur in close association with carbonate and evaporite rocks that have been invaded by crude oil and/or natural gas. In some cases, however, long-distance migration of sulphate and/or metals is indicated. read more read less

Topics:

Carbonate (56%)56% related to the paper, Sphalerite (53%)53% related to the paper, Ankerite (53%)53% related to the paper, Galena (51%)51% related to the paper, Siderite (51%)51% related to the paper
90 Citations
Journal Article DOI: 10.1007/BF03175407
Blue holes: Definition and genesis
John E. Mylroie1, James L. Carew2, Audra I. Moore1

Abstract:

Blue holes are karst features that were initially described from Bahamian islands and banks, which have been documented for over 100 years. They are water-filled vertical openings in the carbonate rock that exhibit complex morphologies, ecologies, and water chemistries. Their deep blue color, for which they are named, is the ... Blue holes are karst features that were initially described from Bahamian islands and banks, which have been documented for over 100 years. They are water-filled vertical openings in the carbonate rock that exhibit complex morphologies, ecologies, and water chemistries. Their deep blue color, for which they are named, is the result of their great depth, and they may lead to cave systems below sea level. Blue holes are polygenetic in origin, having formed: by drowning of dissolutional sinkholes and shafts developed in the vadose zone; by phreatic dissolution along an ascending halocline; by progradational collapse upward from deep dissolution voids produced in the phreatic zone; or by fracture of the bank margin. Blue holes are the cumulative result of carbonate deposition and dissolution cycles which have been controlled by Quaternary glacioeustatic fluctuations of sea-level. read more read less

Topics:

Phreatic (56%)56% related to the paper, Sinkhole (53%)53% related to the paper, Vadose zone (53%)53% related to the paper, Phreatic zone (52%)52% related to the paper, Carbonate rock (50%)50% related to the paper
89 Citations
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Frequently asked questions

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Yes, the template is compliant with the Carbonates and Evaporites 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 Carbonates and Evaporites?

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 Carbonates and Evaporites citation style.

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5. Can I use a manuscript in Carbonates and Evaporites 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 Carbonates and Evaporites that you can download at the end.

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

12. Is Carbonates and Evaporites'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 Carbonates and Evaporites?

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 Carbonates and Evaporites. 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 Carbonates and Evaporites?

The 5 most common citation types in order of usage for Carbonates and Evaporites 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 Carbonates and Evaporites 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 Carbonates and Evaporites Endnote style according to Elsevier guidelines.

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