The hydrothermal Waterberg platinum deposit, Mookgophong (Naboomspruit), South Africa. Part 2 – Quartz chemistry, fluid inclusions and geochronology

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The hydrothermal Waterberg platinum deposit, Mookgophong (Naboomspruit), South Africa. Part 2 – Quartz chemistry, fluid inclusions and geochronology. / Alfons, van den Kerkhof; Sosa, Graciela M.; Oberthür, Thomas et al.
in: Mineralogical Magazine, Jahrgang 82, Nr. 3, 01.08.2018, S. 751-778.

Publikationen: Beitrag in FachzeitschriftArtikelForschung(peer-reviewed)

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Author

Alfons, van den Kerkhof ; Sosa, Graciela M. ; Oberthür, Thomas et al. / The hydrothermal Waterberg platinum deposit, Mookgophong (Naboomspruit), South Africa. Part 2 – Quartz chemistry, fluid inclusions and geochronology. in: Mineralogical Magazine. 2018 ; Jahrgang 82, Nr. 3. S. 751-778.

Bibtex - Download

@article{bc4d79f22e4f456c877819c8599893f5,
title = "The hydrothermal Waterberg platinum deposit, Mookgophong (Naboomspruit), South Africa. Part 2 – Quartz chemistry, fluid inclusions and geochronology",
author = "Alfons, {van den Kerkhof} and Sosa, {Graciela M.} and Thomas Oberth{\"u}r and Frank Melcher and Tobias Fusswinkel and Andreas Kronz and Klaus Simon and Istv{\'a}n Dunkl",
year = "2018",
month = aug,
day = "1",
doi = "10.1180/mgm.2018.80",
language = "English",
volume = "82",
pages = "751--778",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "3",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - The hydrothermal Waterberg platinum deposit, Mookgophong (Naboomspruit), South Africa. Part 2 – Quartz chemistry, fluid inclusions and geochronology

AU - Alfons, van den Kerkhof

AU - Sosa, Graciela M.

AU - Oberthür, Thomas

AU - Melcher, Frank

AU - Fusswinkel, Tobias

AU - Kronz, Andreas

AU - Simon, Klaus

AU - Dunkl, István

PY - 2018/8/1

Y1 - 2018/8/1

U2 - 10.1180/mgm.2018.80

DO - 10.1180/mgm.2018.80

M3 - Article

VL - 82

SP - 751

EP - 778

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 3

ER -