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The New Massadou Diamondiferous Kimberlite Field in Guinea. / Afanasiev, V. P.; Nikolenko, E. I.; Glushkova, N. V. et al.

In: Geology of Ore Deposits, Vol. 61, No. 4, 01.07.2019, p. 381-390.

Research output: Contribution to journal › Article › peer-review

Harvard

Afanasiev, VP, Nikolenko, EI, Glushkova, NV & Zolnikov, ID 2019, 'The New Massadou Diamondiferous Kimberlite Field in Guinea', Geology of Ore Deposits, vol. 61, no. 4, pp. 381-390. https://doi.org/10.1134/S1075701519030024

APA

Afanasiev, V. P., Nikolenko, E. I., Glushkova, N. V., & Zolnikov, I. D. (2019). The New Massadou Diamondiferous Kimberlite Field in Guinea. Geology of Ore Deposits, 61(4), 381-390. https://doi.org/10.1134/S1075701519030024

Vancouver

Afanasiev VP, Nikolenko EI, Glushkova NV, Zolnikov ID. The New Massadou Diamondiferous Kimberlite Field in Guinea. Geology of Ore Deposits. 2019 Jul 1;61(4):381-390. doi: 10.1134/S1075701519030024

Author

Afanasiev, V. P. ; Nikolenko, E. I. ; Glushkova, N. V. et al. / The New Massadou Diamondiferous Kimberlite Field in Guinea. In: Geology of Ore Deposits. 2019 ; Vol. 61, No. 4. pp. 381-390.

BibTeX

@article{59a3dc629cff4672ab7da8a5a13e4b4f,
title = "The New Massadou Diamondiferous Kimberlite Field in Guinea",
abstract = "Abstract: A new Massadou kimberlite field, was discovered in southeastern Guinea, near the town of Macenta. It consists of 16 poorly diamondiferous kimberlite dikes, ~1 m thick on average. The ore-controlling zone has a width of around 600 m, its orientation corresponds to the K-4 trend after S. Haggerty, and it is quite well detectable in satellite images. A thick laterite weathering profile has developed on the kimberlites. The main indicator minerals are pyrope, chromite, and ilmenite. Ilmenite grains have a zoned structure with a high-Fe core (hemoilmenite) overgrown by a parallel-columnar aggregate of Mg-ilmente rim resulting from interaction of the core phase with kimberlitic melt. The age of kimberlites is estimated as 140–145 Ma by analogy with those in adjacent areas. Dikes occur as an independent form of kimberlite magmatism in the Guinean–Liberian shield, rather than being roots of kimberlite pipes; therefore, the erosion cutout is relatively small and large-scale diamond placers should not be expected.",
keywords = "diamond, Guinean–Liberian shield, kimberlite, kimberlite indicator minerals, tectonic control of kimberlites, Guinean-Liberian shield",
author = "Afanasiev, {V. P.} and Nikolenko, {E. I.} and Glushkova, {N. V.} and Zolnikov, {I. D.}",
year = "2019",
month = jul,
day = "1",
doi = "10.1134/S1075701519030024",
language = "English",
volume = "61",
pages = "381--390",
journal = "Geology of Ore Deposits",
issn = "1075-7015",
publisher = "Maik Nauka-Interperiodica Publishing",
number = "4",

}

RIS

TY - JOUR

T1 - The New Massadou Diamondiferous Kimberlite Field in Guinea

AU - Afanasiev, V. P.

AU - Nikolenko, E. I.

AU - Glushkova, N. V.

AU - Zolnikov, I. D.

PY - 2019/7/1

Y1 - 2019/7/1

N2 - Abstract: A new Massadou kimberlite field, was discovered in southeastern Guinea, near the town of Macenta. It consists of 16 poorly diamondiferous kimberlite dikes, ~1 m thick on average. The ore-controlling zone has a width of around 600 m, its orientation corresponds to the K-4 trend after S. Haggerty, and it is quite well detectable in satellite images. A thick laterite weathering profile has developed on the kimberlites. The main indicator minerals are pyrope, chromite, and ilmenite. Ilmenite grains have a zoned structure with a high-Fe core (hemoilmenite) overgrown by a parallel-columnar aggregate of Mg-ilmente rim resulting from interaction of the core phase with kimberlitic melt. The age of kimberlites is estimated as 140–145 Ma by analogy with those in adjacent areas. Dikes occur as an independent form of kimberlite magmatism in the Guinean–Liberian shield, rather than being roots of kimberlite pipes; therefore, the erosion cutout is relatively small and large-scale diamond placers should not be expected.

AB - Abstract: A new Massadou kimberlite field, was discovered in southeastern Guinea, near the town of Macenta. It consists of 16 poorly diamondiferous kimberlite dikes, ~1 m thick on average. The ore-controlling zone has a width of around 600 m, its orientation corresponds to the K-4 trend after S. Haggerty, and it is quite well detectable in satellite images. A thick laterite weathering profile has developed on the kimberlites. The main indicator minerals are pyrope, chromite, and ilmenite. Ilmenite grains have a zoned structure with a high-Fe core (hemoilmenite) overgrown by a parallel-columnar aggregate of Mg-ilmente rim resulting from interaction of the core phase with kimberlitic melt. The age of kimberlites is estimated as 140–145 Ma by analogy with those in adjacent areas. Dikes occur as an independent form of kimberlite magmatism in the Guinean–Liberian shield, rather than being roots of kimberlite pipes; therefore, the erosion cutout is relatively small and large-scale diamond placers should not be expected.

KW - diamond

KW - Guinean–Liberian shield

KW - kimberlite

KW - kimberlite indicator minerals

KW - tectonic control of kimberlites

KW - Guinean-Liberian shield

UR - http://www.scopus.com/inward/record.url?scp=85071993765&partnerID=8YFLogxK

U2 - 10.1134/S1075701519030024

DO - 10.1134/S1075701519030024

M3 - Article

AN - SCOPUS:85071993765

VL - 61

SP - 381

EP - 390

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 4

ER -

ID: 21472605