Example of Mineralium Deposita format
Recent searches

Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format
Sample paper formatted on SciSpace - SciSpace
This content is only for preview purposes. The original open access content can be found here.
Look Inside
Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format Example of Mineralium Deposita format
Sample paper formatted on SciSpace - SciSpace
This content is only for preview purposes. The original open access content can be found here.
open access Open Access
recommended Recommended

Mineralium Deposita — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Geophysics #5 of 131 up up by 7 ranks
Economic Geology #2 of 38 down down by None rank
Geochemistry and Petrology #11 of 128 up up by 8 ranks
journal-quality-icon Journal quality:
High
calendar-icon Last 4 years overview: 266 Published Papers | 2076 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 22/06/2020
Related journals
Insights
General info
Top papers
Popular templates
Get started guide
Why choose from SciSpace
FAQ

Related Journals

open access Open Access

Springer

Quality:  
High
CiteRatio: 5.9
SJR: 2.078
SNIP: 1.439
open access Open Access
recommended Recommended

Springer

Quality:  
High
CiteRatio: 7.5
SJR: 1.78
SNIP: 2.18
open access Open Access
recommended Recommended

Springer

Quality:  
High
CiteRatio: 11.5
SJR: 1.991
SNIP: 2.319
open access Open Access

Elsevier

Quality:  
High
CiteRatio: 5.0
SJR: 1.089
SNIP: 1.081

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.

4.323

27% from 2018

Impact factor for Mineralium Deposita from 2016 - 2019
Year Value
2019 4.323
2018 3.397
2017 3.37
2016 3.396
graph view Graph view
table view Table view

7.8

28% from 2019

CiteRatio for Mineralium Deposita from 2016 - 2020
Year Value
2020 7.8
2019 6.1
2018 6.2
2017 6.0
2016 5.8
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has increased by 27% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 28% 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.

1.51

18% from 2019

SJR for Mineralium Deposita from 2016 - 2020
Year Value
2020 1.51
2019 1.28
2018 2.115
2017 1.601
2016 1.841
graph view Graph view
table view Table view

1.687

19% from 2019

SNIP for Mineralium Deposita from 2016 - 2020
Year Value
2020 1.687
2019 1.413
2018 1.613
2017 1.769
2016 1.709
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has increased by 18% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

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

Mineralium Deposita

Guideline source: View

All company, product and service names used in this website are for identification purposes only. All product names, trademarks and registered trademarks are property of their respective owners.

Use of these names, trademarks and brands does not imply endorsement or affiliation. Disclaimer Notice

Springer

Mineralium Deposita

This journal introduces new observations, principles, and interpretations from the field of economic geology, including nonmetallic mineral deposits, experimental and applied geochemistry, with emphasis on mineral deposits. It contains short and comprehensive articles, review ...... Read More

Geophysics

Geochemistry and Petrology

Earth and Planetary Sciences

i
Last updated on
22 Jun 2020
i
ISSN
0026-4598
i
Impact Factor
High - 1.169
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/S00126-012-0446-Z
Major types and time–space distribution of Mesozoic ore deposits in South China and their geodynamic settings
Mao Jingwen, Cheng Yanbo1, Chen Maohong1, Franco Pirajno2
01 Mar 2013 - Mineralium Deposita

Abstract:

The ore deposits of the Mesozoic age in South China can be divided into three groups, each with different metal associations and spatial distributions and each related to major magmatic events. The first event occurred in the Late Triassic (230–210 Ma), the second in the Mid–Late Jurassic (170–150 Ma), and the third in the Ea... The ore deposits of the Mesozoic age in South China can be divided into three groups, each with different metal associations and spatial distributions and each related to major magmatic events. The first event occurred in the Late Triassic (230–210 Ma), the second in the Mid–Late Jurassic (170–150 Ma), and the third in the Early–Mid Cretaceous (120–80 Ma). The Late Triassic magmatic event and associated mineralization is characterized by peraluminous granite-related W–Sn–Nb–Ta mineral deposits. The Triassic ore deposits are considerably disturbed or overprinted by the later Jurassic and Cretaceous tectono-thermal episodes. The Mid–Late Jurassic magmatic and mineralization events consist of 170–160 Ma porphyry–skarn Cu and Pb–Zn–Ag vein deposits associated with I-type granites and 160–150 Ma metaluminous granite-related polymetallic W–Sn deposits. The Late Jurassic metaluminous granite-related W–Sn deposits occur in a NE-trending cluster in the interior of South China, such as in the Nanling area. In the Early–Mid Cretaceous, from about 120 to 80 Ma, but peaking at 100–90 Ma, subvolcanic-related Fe deposits developed and I-type calc-alkaline granitic intrusions formed porphyry Cu–Mo and porphyry-epithermal Cu–Au–Ag mineral systems, whereas S-type peraluminous and/or metaluminous granitic intrusions formed polymetallic Sn deposits. These Cretaceous mineral deposits cluster in distinct areas and are controlled by pull-apart basins along the South China continental margin. Based on mineral assemblage, age, and space–time distribution of these mineral systems, integrated with regional geological data and field observations, we suggest that the three magmatic–mineralization episodes are the result of distinct geodynamic regimes. The Triassic peraluminous granites and associated W–Sn–Nb–Ta mineralization formed during post-collisional processes involving the South China Block, the North China Craton, and the Indo-China Block, mostly along the Dabie-Sulu and Songma sutures. Jurassic events were initially related to the shallow oblique subduction of the Izanagi plate beneath the Eurasian continent at about 175 Ma, but I-type granitoids with porphyry Cu and vein-type Pb–Zn–Ag deposits only began to form as a result of the breakup of the subducted plate at 170–160 Ma, along the NNE-trending Qinzhou-Hangzhou belt (also referred to as Qin-Hang or Shi-Hang belt), which is the Neoproterozoic suture that amalgamates the Yangtze Craton and Cathaysia Block. A large subduction slab window is assumed to have formed in the Nanling and adjacent areas in the interior of South China, triggering the uprise of asthenospheric mantle into the upper crust and leading to the emplacement of metaluminous granitic magma and associated polymetallic W–Sn mineralization. A relatively tectonically quiet period followed between 150 and 135 Ma in South China. From 135 Ma onward, the angle of convergence of the Izanagi plate changed from oblique to parallel to the coastline, resulting in continental extensional tectonics and reactivation of regional-scale NE-trending faults, such as the Tan-Lu fault. This widespread extension also promoted the development of NE-trending pull-apart basins and metamorphic core complexes, accompanied by volcanism and the formation of epithermal Cu–Au deposits, granite-related polymetallic Sn–(W) deposits and hydrothermal U deposits between 120 and 80 Ma (with a peak activity at 100–90 Ma). read more read less

Topics:

Slab window (54%)54% related to the paper, Craton (54%)54% related to the paper, Extensional tectonics (52%)52% related to the paper, Metamorphic core complex (51%)51% related to the paper, Cretaceous (51%)51% related to the paper
683 Citations
Journal Article DOI: 10.1007/S00126-011-0334-Y
Discriminant diagrams for iron oxide trace element fingerprinting of mineral deposit types
C. Dupuis1, Georges Beaudoin1
08 Feb 2011 - Mineralium Deposita

Abstract:

Magnetite and hematite are common minerals in a range of mineral deposit types. These minerals form partial to complete solid solutions with magnetite, chromite, and spinel series, and ulvospinel as a result of divalent, trivalent, and tetravalent cation substitutions. Electron microprobe analyses of minor and trace elements ... Magnetite and hematite are common minerals in a range of mineral deposit types. These minerals form partial to complete solid solutions with magnetite, chromite, and spinel series, and ulvospinel as a result of divalent, trivalent, and tetravalent cation substitutions. Electron microprobe analyses of minor and trace elements in magnetite and hematite from a range of mineral deposit types (iron oxide-copper-gold (IOCG), Kiruna apatite–magnetite, banded iron formation (BIF), porphyry Cu, Fe-Cu skarn, Fe-Ti, V, Cr, Ni-Cu-PGE, Cu-Zn-Pb volcanogenic massive sulfide (VMS) and Archean Au-Cu porphyry and Opemiska Cu veins) show compositional differences that can be related to deposit types, and are used to construct discriminant diagrams that separate different styles of mineralization. The Ni + Cr vs. Si + Mg diagram can be used to isolate Ni-Cu-PGE, and Cr deposits from other deposit types. Similarly, the Al/(Zn + Ca) vs. Cu/(Si + Ca) diagram can be used to separate Cu-Zn-Pb VMS deposits from other deposit types. Samples plotting outside the Ni-Cu-PGE and Cu-Zn-Pb VMS fields are discriminated using the Ni/(Cr + Mn) vs. Ti + V or Ca + Al + Mn vs. Ti + V diagrams that discriminate for IOCG, Kiruna, porphyry Cu, BIF, skarn, Fe-Ti, and V deposits. read more read less

Topics:

Iron oxide copper gold ore deposits (55%)55% related to the paper, Ulvöspinel (54%)54% related to the paper, Magnetite (54%)54% related to the paper, Hematite (52%)52% related to the paper, Volcanogenic massive sulfide ore deposit (52%)52% related to the paper
400 Citations
open accessOpen access Journal Article
In situ U-Pb zircon dating using laser ablation-multi ion counting-ICP-MS
Hou Ke, Mrl Key1
01 Jan 2009 - Mineralium Deposita

Abstract:

High resolution in situ U-Pb zircon geochronology on zoned grains can obtain isotope signatures from multiple growth or thermal events.We present a method using laser ablation-multicollector-inductively coupled plasma-mass spectrometry(LA-MC-ICP-MS) to overcome complications associated with intricately zoned zircon crystals t... High resolution in situ U-Pb zircon geochronology on zoned grains can obtain isotope signatures from multiple growth or thermal events.We present a method using laser ablation-multicollector-inductively coupled plasma-mass spectrometry(LA-MC-ICP-MS) to overcome complications associated with intricately zoned zircon crystals through in situ sampling of zircon volumes as small as 12 μm,25 μm and 40 μm in diameter by about 10 μm in depth.High precision U-Pb age of a series of zircon standard covering a wide age range of 30 to 1 065 Ma was acquired using LA-MC-ICP-MS.The precision of measured Pb/U ratios in homogeneous zircon is about 2%(2σ),resulting in routinely achieved precision of U-Pb ages obtained by external calibration of~1%(2σ) or better.All masses of interest can be simultaneously recorded with a multi-ion counting system(MIC) operating in static mode,and the short ablation required to achieve such precision results in spatial resolution that is superior to comparable U-Pb zircon analyses by single collector ICP-MS.The resulting present U-Pb age for five zircon reference samples and two geological samples show an excellent agreement with the previously reported ID-TIMS or SHRIMP data. read more read less

Topics:

Zircon (59%)59% related to the paper
396 Citations
Journal Article DOI: 10.1007/BF02431596
The crustal continuum model for late-Archaean lode-gold deposits of the Yilgarn Block, Western Australia
David I. Groves1
01 Jan 1993 - Mineralium Deposita

Abstract:

Most Archaean gold ores belong to a coherent genetic group of structurally controlled lode-deposits that are characteristically enriched in Au with variable enrichments in Ag, As, W, Sb, Bi, Te, B and Pb, but rarely Cu or Zn, and are surrounded by wallrock alteration haloes enriched in K, LILE and CO2, with variable Na and/or... Most Archaean gold ores belong to a coherent genetic group of structurally controlled lode-deposits that are characteristically enriched in Au with variable enrichments in Ag, As, W, Sb, Bi, Te, B and Pb, but rarely Cu or Zn, and are surrounded by wallrock alteration haloes enriched in K, LILE and CO2, with variable Na and/or Ca addition. Evidence from the Yilgarn Block of Western Australia, combined with similar evidence from Canada and elsewhere, indicates that such deposits represent a crustal continuum that formed under a variety of crustal regimes over at least a 15 km crustal profile at PT conditions ranging from 180°C at <1 kb to 700°C at 5 kb. Individual deposits, separated by tens to hundreds of kilometres, collectively show transitional variations in structural style of mineralisation, vein textures, and mineralogy of wallrock alteration that relate to the PT conditions of their formation at varying crustal depths. Specific transitions within the total spectrum may be shown also by deposits within gold camps, although nowhere is the entire continuum of deposits recorded from a single gold camp or even greenstone belt. Recognition of the crustal continuum of deposits implicates the existence of giant late-Archaean hydrothermal systems with a deep source for the primary ore fluid. A number of deep fluid and solute reservoirs are possible, including the basal segments of greenstone belts, deep-level intrusive granitoids, mid-to lower-crustal granitoidgneisses, mantle lithosphere, or even subducted oceanic lithosphere, given the probable convergent-margin setting of the host greenstone terranes. Individual stable and radiogenic isotope ratios of fluid and solute components implicate fluid evolution from, or equilibrium with, a number of these reservoirs, stressing the potential complexity of pathways for fluid advection to depositional sites. Lead and strontium isotope ratios of ore-associated minerals provide the most persuasive evidence for fluid advection through deep-level intrusive granitoids or granitoid-gneiss crust, whereas preliminary oxygen isotope data show that mixing of deeply sourced fluid and surface waters only occurred at the highest crustal levels recorded by the lode gold deposits. read more read less

Topics:

Greenstone belt (55%)55% related to the paper, Terrane (52%)52% related to the paper, Lode (51%)51% related to the paper, Archean (51%)51% related to the paper, Vein (geology) (50%)50% related to the paper
383 Citations
Author Pic

SciSpace is a very innovative solution to the formatting problem and existing providers, such as Mendeley or Word did not really evolve in recent years.

- Andreas Frutiger, Researcher, ETH Zurich, Institute for Biomedical Engineering

Get MS-Word and LaTeX output to any Journal within seconds
1
Choose a template
Select a template from a library of 40,000+ templates
2
Import a MS-Word file or start fresh
It takes only few seconds to import
3
View and edit your final output
SciSpace will automatically format your output to meet journal guidelines
4
Submit directly or Download
Submit to journal directly or Download in PDF, MS Word or LaTeX

(Before submission check for plagiarism via Turnitin)

clock Less than 3 minutes

What to expect from SciSpace?

Speed and accuracy over MS Word

''

With SciSpace, you do not need a word template for Mineralium Deposita.

It automatically formats your research paper to Springer formatting guidelines and citation style.

You can download a submission ready research paper in pdf, LaTeX and docx formats.

Time comparison

Time taken to format a paper and Compliance with guidelines

Plagiarism Reports via Turnitin

SciSpace has partnered with Turnitin, the leading provider of Plagiarism Check software.

Using this service, researchers can compare submissions against more than 170 million scholarly articles, a database of 70+ billion current and archived web pages. How Turnitin Integration works?

Turnitin Stats
Publisher Logos

Freedom from formatting guidelines

One editor, 100K journal formats – world's largest collection of journal templates

With such a huge verified library, what you need is already there.

publisher-logos

Easy support from all your favorite tools

Mineralium Deposita format uses SPBASIC citation style.

Automatically format and order your citations and bibliography in a click.

SciSpace allows imports from all reference managers like Mendeley, Zotero, Endnote, Google Scholar etc.

Frequently asked questions

1. Can I write Mineralium Deposita in LaTeX?

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

2. Do you follow the Mineralium Deposita guidelines?

Yes, the template is compliant with the Mineralium Deposita 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 Mineralium Deposita?

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 Mineralium Deposita citation style.

4. Can I use the Mineralium Deposita 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 Mineralium Deposita.

5. Can I use a manuscript in Mineralium Deposita 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 Mineralium Deposita that you can download at the end.

6. How long does it usually take you to format my papers in Mineralium Deposita?

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

7. Where can I find the template for the Mineralium Deposita?

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 Mineralium Deposita'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 Mineralium Deposita'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. Mineralium Deposita an online tool or is there a desktop version?

SciSpace's Mineralium Deposita 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 Mineralium Deposita?

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 Mineralium Deposita?”

11. What is the output that I would get after using Mineralium Deposita?

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

12. Is Mineralium Deposita'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 Mineralium Deposita?

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 Mineralium Deposita. 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 Mineralium Deposita?

The 5 most common citation types in order of usage for Mineralium Deposita 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 Mineralium Deposita?

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 Mineralium Deposita's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

16. Can I download Mineralium Deposita 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 Mineralium Deposita Endnote style according to Elsevier guidelines.

Fast and reliable,
built for complaince.

Instant formatting to 100% publisher guidelines on - SciSpace.

Available only on desktops 🖥

No word template required

Typset automatically formats your research paper to Mineralium Deposita formatting guidelines and citation style.

Verifed journal formats

One editor, 100K journal formats.
With the largest collection of verified journal formats, what you need is already there.

Trusted by academicians

I spent hours with MS word for reformatting. It was frustrating - plain and simple. With SciSpace, I can draft my manuscripts and once it is finished I can just submit. In case, I have to submit to another journal it is really just a button click instead of an afternoon of reformatting.

Andreas Frutiger
Researcher & Ex MS Word user
Use this template