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Article
Peer-Review Record

Geochemistry and Mineralogy of the Clay-Type Ni-Laterite Deposit of San Felipe (Camagüey, Cuba)

Minerals 2023, 13(10), 1281; https://doi.org/10.3390/min13101281
by Esperança Tauler 1,*, Salvador Galí 1, Cristina Villanova-de-Benavent 1, Alfonso Chang-Rodríguez 2, Kenya Núñez-Cambra 3, Giorgi Khazaradze 4 and Joaquín Antonio Proenza 1
Reviewer 2:
Reviewer 3:
Reviewer 4:
Minerals 2023, 13(10), 1281; https://doi.org/10.3390/min13101281
Submission received: 1 August 2023 / Revised: 19 September 2023 / Accepted: 21 September 2023 / Published: 29 September 2023
(This article belongs to the Special Issue Geochemistry and Mineralogy of Ni-Co Laterite Deposits)

Round 1

Reviewer 1 Report

The authors should improve the readability and overall quality of this article (particularly in the introduction, geology, and methodology parts) before considering it for publication in your journal. My comments and suggestions are attached to above

Please refer to all comments shown in the attached annotated file

Comments for author File: Comments.pdf

Author Response

Please see the attachment

Author Response File: Author Response.docx

Reviewer 2 Report


Comments for author File: Comments.pdf

Author Response

Please see the attachment

Author Response File: Author Response.docx

Reviewer 3 Report

1. Some figures can be further improved (The font size in Figure 1 should be uniform).

2.The conclusion can be further condensed.

In Line 20 and Line 21, please check the unit statement.

Author Response

Please see the attachment

Author Response File: Author Response.docx

Reviewer 4 Report

Dear authors,

 

This is a nice paper on the mineralogy and geochemistry of the smectite-rich Ni-laterite at San Felipe and I enjoyed reading the manuscript. I understand that this is a quite exploratory work and I appreciate the effort made for comparing with other known clay-type Ni-laterites. Apart from a few minor comments, I believe that the manuscript could benefit from a more extensive discussion regarding the timing of mineralisation, the influence of geomorphology and mineralogy/geochemistry of the parent rock, and the origin of amorphous or poorly crystaline silica. It is too bad that you only have XRF geochemistry on major/minor elements, I would have loved to see some Sc concentrations ! Indeed with such a pyroxene-rich protolith (before serpentinisation), we might expect some elevated Sc concentrations, though the behaviour of Sc during smectitisation remains to be further constrained. Please see the comments made in the pdf file.

 

Regards,

 

Comments for author File: Comments.pdf

Author Response

Please see the attachment

Author Response File: Author Response.docx

Round 2

Reviewer 1 Report

Despite some comments, the authors addressed them well enough for the paper to be accepted for publication

best wishes

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