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Journal/NDM52 2018 eng — различия между версиями

Строка 1: Строка 1:
==== '''New Data on Minerals 2020 (Volume 54).''' ====
+
==== I. GENERAL ====
 +
* The journal “New Mineral Data” publishes original articles (including short messages in the Mineralogical Notes section), reviews, historical materials, discussions, reviews, personalities and chronicles of current events (exhibitions, conferences, anniversaries, etc.), relating to mineralogy, crystallography, crystal chemistry, as well as museology and mineralogical collections.<br>
 +
*
 +
* It publishes materials submitted by graduate students, applicants, doctoral students, specialists and experts in this field of research.<br>
 +
*
 +
* Article submission and editorial processing is free of charge.<br>
 +
*
 +
* Articles received by the editors are submitted for review. At the request of the reviewer, the article may be rejected or sent to the authors for revision. In the latter case, the authors must return the corrected version of the article, taking into account all the comments of the reviewer.<br>
 +
*
 +
* Author rights are protected as per the relevant international rules.<br>
 +
*
 +
* Articles published in Russian and English.<br>
 +
==== II. RECOMMENDATIONS TO THE AUTHOR BEFORE SUBMITTING A MANUSCRIPT ====
 +
* This manuscript has not been published earlier in any other journal.<br>
 +
*
 +
* This manuscript is not under consideration in another journal.<br>
 +
*
 +
* Bulleted list item
 +
* Its co-authors have agreed to publish the current version of the manuscript.<br>
 +
*
 +
* The new minerals described in the article must pass a preliminary approbation in the Commission on new minerals and mineral names.<br>
 +
==== III. MANUSCRIPT SUBMISSION GUIDELINES ====
 +
* To the Editor to send a paper copy of the article, signed by all authors, e-copy (required) and approximate layout of electronic paper.<br>
 +
 
 +
* The manuscript volume shall not exceed 40,000 characters (including spaces), excluding tables, references and illustrations/figures. Short communications: maximum length - 10,000–12,000 characters (including spaces), plus a list of references.<br>
 +
 
 +
* Page numbers in the lower right corner.<br>
 +
 
 +
* A manuscript shall contain the following:<br>
 +
'''Article title''' - The title of the article should be written in lowercase and bold letters, in italics.<br>
 +
'''Authors surnames and initials'''<br>
 +
Affiliation - Complete official name of the organization, and complete postal address, including zip code, city and country. The author shall indicate all affiliations related to the study. For contact with the authors also indicate email address.
 +
Summary - (100-180 words) to build so that readers without going to the full text of received ideas about the subject and level of published results.<br>
 +
'''Keywords''' - up to 7 words.'''<br>
 +
Text of the article''' - without figures and tables.<br>
 +
'''Bibliographic references'''<br>
 +
'''Funding''' - It is required to specify all sources of funding for the study.<br>
 +
'''Acknowledgments'''<br><br>
 +
'''Tables''' (each on a separate page)<br>
 +
'''Figures''' (each on a separate page)<br>
 +
'''Figure captions''' (on a separate page)<br>
 +
====  IV. MANUSCRIPT FORMAT GUIDELINES ====
 +
* Text
 
   
 
   
==== DEADLINE FOR ARTICLES ====
+
Text page set-up: A4, Microsoft Word, double interval spacing, Times New Roman (Size 12), 2 cm margins all round, justified alignment. Each paragraph shall be indented by 1.25 cm. No hyphenation. Page numbers in the lower right corner.<br>
*Issue 1 - March 31, 2020
+
No abbreviations are allowable in the text, except the standard ones complying with the International System of Units. Decimal separator: period (i.e. point, or dot).<br>
*Issue 2 - May 31, 2020
+
Mathematical formulas: Microsoft Word (depending on the version).<br>
*Issue 3 - August 31, 2020
+
You can use subheadings to structure your article. They stand out in bold and lowercase letters. Subtitle Separated from Text spaces, no dot at the end of the subtitle.<br>
*Issue 4 - November 30, 2020<br>
+
* Tables
<br>
+
Tables shall be in the editable text format (not as a scan or a drawing). Large tables shall be given in separate pages in the text format.<br>
==== '''CONTENTS Vol.54''' ====
+
A table header shall include its number and name, no dot at the end of the table header. Notes and footnotes to tables should be printed directly below them (Times New Roman (size 8-10 pt).<br>
==== '''''Issue 1''''' ====
+
Tables shall be numbered in Arabic numerals through the text. If the text contains only one table, this table shall not be assigned any number. References to the tables: e.g., «Table 1 gives…», «It is noted that ... (see Table 2)».<br>
{{NDM_article
+
* Illustrations
| Авторы = Smolyaninova V.N.  
+
Each figure should be in good quality and needs to have a figure caption. Full-colour illustrations, as well as extended explanations for the figures (as part of the figure captions) are welcome.<br>
| Название = Devoted to the 110th anniversary of the birth of Natalia Nikolaevna Smolyaninova, pp. 1-18
+
Vector graphics: CorelDRAW. Submit in CorelDRAW or InDesign formats etc.<br>
| Аннотация = Natalia Nikolaevna Smolyaninova (1919–2013) - mineralogist, daughter of the famous mineralogist Nikolai Alekseevich Smolyaninov. She worked at IGEM USSR Academy of Sciences, studied the mineralogy of the radium-uranium-vanadium deposits of Tyuya-Muyun (Kyrgyzstan) and the tungsten-molybdenum deposits of Akchatau and Batystau (Kazakhstan). She was main-editor of five of the 12 issues of the encyclopedic guide "Minerals".
+
Raster graphics (photographs, scanned materials): TIFF or JPEG format (JPEG format of maximum or high quality). Resolution: min 600 dpi for black-and-white figures (Bitmap); min 300 dpi for photos. The scale and direction of the "top-bottom" should be indicated on the photographs.<br>
| Файл = Smolianinova_1_2020-1_rus.pdf
+
Required elements of a figure caption: figure number and its title. Figure numbers should be Arabic. If the manuscript contains only one figure, no number should be assigned to this figure. References to the figures: «Figure 3 shows that… «; «It is indicated that ... (fig. 3)».<br>
| Приложения =
+
* References
}}{{NDM_article
+
References to the cited literature shall be given in the text in brackets: e.g. one author – (Smith, 1999), two authors - [Smith, Jones, 1999], more than two authors - [Smith et al., 1999].<br>
| Авторы = Karpenko V.Yu., Pautov L.A., Shodibekov M., Makhmadsharif S., Mirakov M.A. 
+
A list of references shall be compiled in the alphabetical order. It shall be separated from the text by a blank line. Names of all the authors shall be given and printed in italics. Full names of journals cited shall be given.<br>
| Название = Coconinoite: find at the Zor-Yarchi-Chak ore occurrence, Eastern Pamir, pp. 19-25
+
References in the text shall strictly correspond to the list of references. Should the authors fail to meet this requirement, the Editorial Board reserves the right to correct references in the text and, if required, delete a reference from the list.<br>
| Аннотация = The find of the coconinoite Fe2Al2 (UO2) 2 (PO4) 4 (SO4) (OH) 2 ∙ 20H2O in the oxidation zone at the uranium occurrence Zor-Yarchi-Chak (right bank of the South Ak-Baital River, Eastern Pamir, Tajikistan) is described. The mineral was found in fissures of substantially quartz rock in the form of dense clay-like masses of yellowish color (up to 2 cm2 in area), consisting of lamellar individuals 5–10 microns in diameter across. The refractive index nm = 1.589 (3) at 589 nm. The IR spectrum of the mineral is given. Composition (molecular weight, wt.%, Average for 24 analyzes; range for Al and Fe; H2O - CNH analysis, average for 2 analyzes, wt.%): Al2O3 6.95 (5.44–7.70), Fe2O3 11.13 (9.77–12.91), UO3 39.09, P2O5 18.35, SO3 4.64, H2O 22.7, total 102.86. The overestimation of the amount may be associated with partial dehydration of the mineral during microprobe analysis. The empirical formula is Fe2.07Al2.12U + 62.08P3.93S0.88О24 (OH) 2 · 18.16H2O (calculated on 24O + 2OH). Unit cell parameters: a = 12.45 (1), b = 12.87 (1), c = 22.75 (1), β = 105.66 (4). An analysis of the variations of Al and Fe in coconinoite from different locations (up to the high-aluminum non-iron analogue, Koscheka, Uzbekistan) confirms the existence of a natural series with extreme Al and Fe dominant members.
+
'''Journals'''
| Файл = Karpenko_2_2020-1_rus.pdf
+
Nekrylov, N. A., Popov, D. V., Plechov, P. Y., Shcherbakov, V. D., Danyushevsky, L. V., and Dirksen, O. V., 2018, Garnet-Pyroxenite-Derived End-Member Magma Type in Kamchatka: Evidence from Composition of Olivine and Olivine-Hosted Melt Inclusions in Holocene Rocks of Kekuknaisky Volcano. Petrology, v. 26, p. 329-350.<br>
| Приложения =
+
'''Books'''
}}{{NDM_article
+
Magnus Wangen, 2010. Principles of Sedimentary Basin Analysis. Cambridge University Press, Cambridge, 527 p.<br>
| Авторы = Pautov L.A., Karpenko V.Yu., Mirakov M.A., Alinazarov U.S., Shodibekov M.A., Iskandarov F.Sh.
+
'''Articles/chapters in books'''
| Название = About bismuthocolumbite from myarolite granite pegmatites in the Eastern Pamirs, pp. 26-37
+
Sun S.S., McDonough W.F., 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: A.D. Sounders, M.J. Norry (Eds), Magmatism in the ocean basins. Geological Society Special Publication, vol. 42, p. 313–345.<br>
| Аннотация = Findings of bismuthocolumbumite in myarolite granite pegmatites of the Rangkul pegmatite field in the Eastern Pamirs, Gorno-Badakhshan Autonomous Area, Tajikistan are described. The mineral was found in the form of crystals up to 2 cm in the myarol cavities of the pegmatite veins Mika, Malysh and in the form of sprouts of 20–30 μm in Sc-containing columbite-Mn in intergrowth with eschinitis- (Y) in the near-myarol complex of pegmatite Dorozhny. The crystals were measured on a goniometer; the calculated and measured coordinates of the faces are given (in the setup a <c <b). The habitus of the crystals is prismatic, determined by the faces of the rhombic prism m {110}; minor and weakly expressed faces of the prismatic belt: pinacoid {010}, prisms {130}, {150}, {160}, {170}; the usual faces of the head are the rhombic prism i {101} and the dipyramid u {111}, the more rare prism f {032}. The color of bismuthocolumbite in crystals is dark brown, almost black, shines reddish-brown, in small fragments reddish-brown to light brown. The trait is light brown. Cleavage perfect according to (010). The measured density, g / cm3, 7.36 (1) (Kid), 7.61 (1) (Mika). Optically biaxial (+), 2V = 70 (10) °, the dispersion is strong, r> v. The plane of the optical axes is perpendicular to the (010) plane. The refractive indices of bismuthocolumbite from Mick's pegmatite: np = 2.42 (1), nm = 2.45 (1), ng = 2.50 (2). In reflected light, gray with a faint bluish tint, medium reflectivity, strong anisotropy, strong reflections from yellow to reddish-brown. Reflection spectra are given. Microhardness VHN100 = 360 (Kid), 353 (Mika). 6 m. analyzes. Chem. composition (wt.%, selective an., Kid, Mika, Dorozhniy): Ta2O5 2.11, 11.66, 8.61; Nb2O5 35.54, 28.11, 8.61; WO3 0.08, 0.11, 3.60; TiO2 0.02, 0.00, 0.58; PbO 0.10, 0.10, 0.00; SnO2 0.03, 0.12, 0.00; MnO 0.00, 0.01, 0.26; FeO 0.03, 0.00, 0.11; Sb2O3 0.78, 1.77, 8.55; Bi2O3 62.50, 57.59, 49.75; amount 101.19, 99.47, 100.10. X-ray powder diffraction patterns are shown. Parameters of the rhombic unit cell (Å): a = 4.982 (2), b = 11.719 (4); c = 5.677 (2) (Kid); a = 4.981 (2), b = 11.746 (4); c = 5.670 (2) (Mika). Possible reasons for the rarity of bismuthocolocolumbite as compared to stibiocolumbite and their Ta analogues are discussed.
+
'''Electronic resources/sources:'''
| Файл = Pautov_3_2020-1_rus.pdf
+
International Seismological Centre, On-line Bulletin, 2012. Available from: http://www.isc.ac.uk (last accessed 27.08.2012).<br>
| Приложения =
+
 
}}{{NDM_article
+
Register article in edition only carried out subject to the rules for authors. In case of a substantial revision of Article date of its receipt is the date of the submission of a corrected version.
| Авторы = Kasatkin A.V.
+
According to the actual content of materials, precision bibliographic references, quotations, writing geographical names and proper names liable authors of the manuscript.<br>
| Название = To the question of re-studying mineralogical samples from museum collections. I. General Aspects, pp. 38-51
 
| Аннотация = The article is devoted to the problem of re-studying the samples of minerals stored in museum collections. Two main areas of revision of museum material are examined in detail. One of them is the re-study of the originals of the first study of minerals (type specimens), specifically aimed at clarifying the essential characteristics of insufficiently studied mineral species. The second direction covers all other samples stored in museum collections. The results of their re-study can be the discovery of new mineral species or clarification of the characteristics of already known minerals, finds, including the first, of rare minerals in a certain region and, in any case, an increase in the degree of knowledge or reliability of the diagnosis of a particular mineral. The significance of the results of such studies determines the relevance of the re-study of museum material and increases the value of museum collections.
 
| Файл = Kasatkin_4_2020-1_rus.pdf
 
| Приложения =
 
}}
 
  
==== '''''Issue 2''''' ====
+
'''Editorial office:''' 119071 Moscow, Leninsky Prospekt 18, Building 2, tel. +7(495)952-0067, mineral@fmm.ru.
{{NDM_article
 
| Авторы = Kasatkin A.V., Skoda R., Chukanov N.V.
 
| Название = To the question of re-studying mineralogical samples from museum collections. II. Cannonite and legernite from the Bukuk deposit (Transbaikalia), pp. 53-60
 
| Аннотация = Rare bismuth sulfates cannonite Bi <sub> 2 </sub> O (SO <sub> 4 </sub>) (OH) <sub> 2 </sub> and legernite Bi <sub> 12.67 </sub> O <sub > 14 </sub> (SO <sub> 4 </sub>) <sub> 5 </sub> as a result of our re-study of bismuth samples from the tungsten deposit Bukuk (V. Transbaikalia) stored in the systematic collection of the Mineralogical Museum named after A.E. Fersman Institute of RAS, number 56077. Both minerals are closely fused together in the composition of polymineral pseudomorphs according to roughly formed bismuthine crystals, forming veins up to 4 cm long and up to 0.5 cm thick. Empirical formulas: Cannonite Bi <sub> 2.06 </sub> S <sub> 0.97 </sub> O <sub> 5 </sub> (OH) <sub> 2 </sub>, legnite Bi <sub> 12.67 </sub> S <sub> 5.00 </sub> O <sub> 34 </sub>. Parameters of monoclinic unit cells: cannonite <i> a </i> = 7.691 (1), <i> b </i> = 13.874 (2), <i> c </i> = 5.6569 (8) Å, β = 109.23 (1) °, <i> V </i> = 569.90 (9) ų and <i> Z </i> = 4; in legernite: <i> a </i> = 11.197 (2), <i> b </i> = 5.714 (1), <i> c </i> = 11.879 (2) Å, β = 99.37 ( 2) °, <i> V </i> = 749.9 (2) ų and <i> Z </i> = 1. Strong bands in the Raman spectra: for cannonite 111, 121, 144, 184, 221, 318 , 437, 450, 560, 619, 983, 1059, 3439 cm <sup> –1 </sup>, for legernite 150, 183, 216, 313, 474, 969 cm <sup> –1 </sup>. Both minerals were found for the first time in the Russian Federation.
 
| Файл = Kasatkin_1_2020-2_rus.pdf
 
| Приложения =
 
}}
 

Версия 08:05, 25 мая 2020

I. GENERAL

  • The journal “New Mineral Data” publishes original articles (including short messages in the Mineralogical Notes section), reviews, historical materials, discussions, reviews, personalities and chronicles of current events (exhibitions, conferences, anniversaries, etc.), relating to mineralogy, crystallography, crystal chemistry, as well as museology and mineralogical collections.
  • It publishes materials submitted by graduate students, applicants, doctoral students, specialists and experts in this field of research.
  • Article submission and editorial processing is free of charge.
  • Articles received by the editors are submitted for review. At the request of the reviewer, the article may be rejected or sent to the authors for revision. In the latter case, the authors must return the corrected version of the article, taking into account all the comments of the reviewer.
  • Author rights are protected as per the relevant international rules.
  • Articles published in Russian and English.

II. RECOMMENDATIONS TO THE AUTHOR BEFORE SUBMITTING A MANUSCRIPT

  • This manuscript has not been published earlier in any other journal.
  • This manuscript is not under consideration in another journal.
  • Bulleted list item
  • Its co-authors have agreed to publish the current version of the manuscript.
  • The new minerals described in the article must pass a preliminary approbation in the Commission on new minerals and mineral names.

III. MANUSCRIPT SUBMISSION GUIDELINES

  • To the Editor to send a paper copy of the article, signed by all authors, e-copy (required) and approximate layout of electronic paper.
  • The manuscript volume shall not exceed 40,000 characters (including spaces), excluding tables, references and illustrations/figures. Short communications: maximum length - 10,000–12,000 characters (including spaces), plus a list of references.
  • Page numbers in the lower right corner.
  • A manuscript shall contain the following:

Article title - The title of the article should be written in lowercase and bold letters, in italics.
Authors surnames and initials
Affiliation - Complete official name of the organization, and complete postal address, including zip code, city and country. The author shall indicate all affiliations related to the study. For contact with the authors also indicate email address. Summary - (100-180 words) to build so that readers without going to the full text of received ideas about the subject and level of published results.
Keywords - up to 7 words.
Text of the article - without figures and tables.
Bibliographic references
Funding - It is required to specify all sources of funding for the study.
Acknowledgments

Tables (each on a separate page)
Figures (each on a separate page)
Figure captions (on a separate page)

IV. MANUSCRIPT FORMAT GUIDELINES

  • Text

Text page set-up: A4, Microsoft Word, double interval spacing, Times New Roman (Size 12), 2 cm margins all round, justified alignment. Each paragraph shall be indented by 1.25 cm. No hyphenation. Page numbers in the lower right corner.
No abbreviations are allowable in the text, except the standard ones complying with the International System of Units. Decimal separator: period (i.e. point, or dot).
Mathematical formulas: Microsoft Word (depending on the version).
You can use subheadings to structure your article. They stand out in bold and lowercase letters. Subtitle Separated from Text spaces, no dot at the end of the subtitle.

  • Tables

Tables shall be in the editable text format (not as a scan or a drawing). Large tables shall be given in separate pages in the text format.
A table header shall include its number and name, no dot at the end of the table header. Notes and footnotes to tables should be printed directly below them (Times New Roman (size 8-10 pt).
Tables shall be numbered in Arabic numerals through the text. If the text contains only one table, this table shall not be assigned any number. References to the tables: e.g., «Table 1 gives…», «It is noted that ... (see Table 2)».

  • Illustrations

Each figure should be in good quality and needs to have a figure caption. Full-colour illustrations, as well as extended explanations for the figures (as part of the figure captions) are welcome.
Vector graphics: CorelDRAW. Submit in CorelDRAW or InDesign formats etc.
Raster graphics (photographs, scanned materials): TIFF or JPEG format (JPEG format of maximum or high quality). Resolution: min 600 dpi for black-and-white figures (Bitmap); min 300 dpi for photos. The scale and direction of the "top-bottom" should be indicated on the photographs.
Required elements of a figure caption: figure number and its title. Figure numbers should be Arabic. If the manuscript contains only one figure, no number should be assigned to this figure. References to the figures: «Figure 3 shows that… «; «It is indicated that ... (fig. 3)».

  • References

References to the cited literature shall be given in the text in brackets: e.g. one author – (Smith, 1999), two authors - [Smith, Jones, 1999], more than two authors - [Smith et al., 1999].
A list of references shall be compiled in the alphabetical order. It shall be separated from the text by a blank line. Names of all the authors shall be given and printed in italics. Full names of journals cited shall be given.
References in the text shall strictly correspond to the list of references. Should the authors fail to meet this requirement, the Editorial Board reserves the right to correct references in the text and, if required, delete a reference from the list.
Journals Nekrylov, N. A., Popov, D. V., Plechov, P. Y., Shcherbakov, V. D., Danyushevsky, L. V., and Dirksen, O. V., 2018, Garnet-Pyroxenite-Derived End-Member Magma Type in Kamchatka: Evidence from Composition of Olivine and Olivine-Hosted Melt Inclusions in Holocene Rocks of Kekuknaisky Volcano. Petrology, v. 26, p. 329-350.
Books Magnus Wangen, 2010. Principles of Sedimentary Basin Analysis. Cambridge University Press, Cambridge, 527 p.
Articles/chapters in books Sun S.S., McDonough W.F., 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: A.D. Sounders, M.J. Norry (Eds), Magmatism in the ocean basins. Geological Society Special Publication, vol. 42, p. 313–345.
Electronic resources/sources: International Seismological Centre, On-line Bulletin, 2012. Available from: http://www.isc.ac.uk (last accessed 27.08.2012).

Register article in edition only carried out subject to the rules for authors. In case of a substantial revision of Article date of its receipt is the date of the submission of a corrected version. According to the actual content of materials, precision bibliographic references, quotations, writing geographical names and proper names liable authors of the manuscript.

Editorial office: 119071 Moscow, Leninsky Prospekt 18, Building 2, tel. +7(495)952-0067, mineral@fmm.ru.