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

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

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 (

Original language	English
Pages (from-to)	1-5
Number of pages	5
Journal	Scottish Journal of Geology
Volume	40
DOIs	https://doi.org/10.1144/sjg40010001
Publication status	Published - 2004

Keywords

OPHIOLITE COMPLEX
PGE
FRACTIONATION
CHROMITITE
MANTLE
ORIGIN
GREECE
RICH

Access to Document

10.1144/sjg40010001Licence: CC BY-NC-ND

Cite this

@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",

}

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

Abstract

Keywords

Access to Document

Fingerprint

Cite this