Platinum-group minerals within the Ballantrae Complex, SW Scotland

M. R. Power; D Pirrie

doi:10.1144/sjg40010001

Platinum-group minerals within the Ballantrae Complex, SW Scotland

M. R. Power, D Pirrie

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

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Platinum-group minerals (PGM) are present within the chromitites of the northern serpentinite belt (Pinbain Bridge area) of the ophiolitic Ballantrae Complex. A relatively uncommon but moderately diverse PGM assemblage is dominated by small (

Iaith wreiddiol	Saesneg
Tudalennau (o-i)	1-5
Nifer y tudalennau	5
Cyfnodolyn	Scottish Journal of Geology
Cyfrol	40
Dynodwyr Gwrthrych Digidol (DOIs)	https://doi.org/10.1144/sjg40010001
Statws	Cyhoeddwyd - 2004

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10.1144/sjg40010001Trwydded: CC BY-NC-ND

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@article{1add3652108c491c82a6127c3fd9b1a5,

title = "Platinum-group minerals within the Ballantrae Complex, SW Scotland",

abstract = "Platinum-group minerals (PGM) are present within the chromitites of the northern serpentinite belt (Pinbain Bridge area) of the ophiolitic Ballantrae Complex. A relatively uncommon but moderately diverse PGM assemblage is dominated by small (",

keywords = "OPHIOLITE COMPLEX, PGE, FRACTIONATION, CHROMITITE, MANTLE, ORIGIN, GREECE, RICH",

author = "Power, {M. R.} and D Pirrie",

year = "2004",

doi = "10.1144/sjg40010001",

language = "English",

volume = "40",

pages = "1--5",

journal = "Scottish Journal of Geology",

issn = "0036-9276",

publisher = "GEOLOGICAL SOC PUBL HOUSE",

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TY - JOUR

T1 - Platinum-group minerals within the Ballantrae Complex, SW Scotland

AU - Power, M. R.

AU - Pirrie, D

PY - 2004

Y1 - 2004

N2 - Platinum-group minerals (PGM) are present within the chromitites of the northern serpentinite belt (Pinbain Bridge area) of the ophiolitic Ballantrae Complex. A relatively uncommon but moderately diverse PGM assemblage is dominated by small (

AB - Platinum-group minerals (PGM) are present within the chromitites of the northern serpentinite belt (Pinbain Bridge area) of the ophiolitic Ballantrae Complex. A relatively uncommon but moderately diverse PGM assemblage is dominated by small (

KW - OPHIOLITE COMPLEX

KW - PGE

KW - FRACTIONATION

KW - CHROMITITE

KW - MANTLE

KW - ORIGIN

KW - GREECE

KW - RICH

U2 - 10.1144/sjg40010001

DO - 10.1144/sjg40010001

M3 - Article

VL - 40

SP - 1

EP - 5

JO - Scottish Journal of Geology

JF - Scottish Journal of Geology

SN - 0036-9276

ER -

Platinum-group minerals within the Ballantrae Complex, SW Scotland

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