TY - JOUR
T1 - Diamonds from the Nassau Mountains, Suriname
AU - Naipal, Renoesha
AU - Zwaan, J. C. H.
AU - Kroonenberg, Salomon B.
AU - Kriegsman, Leo M.
AU - Mason, Paul R.D.
PY - 2020
Y1 - 2020
N2 - Alluvial diamonds have been found in Suriname since the late 19th century, but to date the details of their origin remain unclear. Here we describe diamonds from Paramaka Creek (Nassau Mountains area) in the Marowijne greenstone belt, Guiana Shield, north-eastern Suriname. Thirteen samples were studied, consisting mainly of euhedral crystals with dominant octahedral and dodecahedral habits. They had colourless to brown to slightly greenish body colours, and some showed green or (less commonly) brown irradiation spots. Surface features showed evidence of late-stage resorption that occurred during their transport to the earth's surface. The studied diamonds were predominantly type IaAB, with nitrogen as both A and B aggregates. In the DiamondView most samples displayed blue and/or green luminescence and concentric growth patterns. Their mineral inclusion assemblages (forsterite and enstatite) indicate a peridotitic (possibly harzburgitic) paragenesis.
AB - Alluvial diamonds have been found in Suriname since the late 19th century, but to date the details of their origin remain unclear. Here we describe diamonds from Paramaka Creek (Nassau Mountains area) in the Marowijne greenstone belt, Guiana Shield, north-eastern Suriname. Thirteen samples were studied, consisting mainly of euhedral crystals with dominant octahedral and dodecahedral habits. They had colourless to brown to slightly greenish body colours, and some showed green or (less commonly) brown irradiation spots. Surface features showed evidence of late-stage resorption that occurred during their transport to the earth's surface. The studied diamonds were predominantly type IaAB, with nitrogen as both A and B aggregates. In the DiamondView most samples displayed blue and/or green luminescence and concentric growth patterns. Their mineral inclusion assemblages (forsterite and enstatite) indicate a peridotitic (possibly harzburgitic) paragenesis.
UR - http://www.scopus.com/inward/record.url?scp=85098122089&partnerID=8YFLogxK
U2 - 10.15506/jog.2020.37.2.180
DO - 10.15506/jog.2020.37.2.180
M3 - Article
AN - SCOPUS:85098122089
SN - 1355-4565
VL - 37
SP - 180
EP - 191
JO - Journal of Gemmology
JF - Journal of Gemmology
IS - 2
ER -