NIELSENITE, PdCu3, A NEW PLATINUM-GROUP INTERMETALLIC MINERAL SPECIES FROM THE SKAERGAARD INTRUSION, GREENLAND

2008 ◽  
Vol 46 (3) ◽  
pp. 709-716 ◽  
Author(s):  
A. M. McDonald ◽  
L. J. Cabri ◽  
N. S. Rudashevsky ◽  
C. J. Stanley ◽  
V. N. Rudashevsky ◽  
...  
Keyword(s):  
Mineral Species ◽  
Skaergaard Intrusion ◽  
Platinum Group

scholarly journals MENSHIKOVITE, Pd3Ni2As3, A NEW PLATINUM-GROUP MINERAL SPECIES FROM TWO LAYERED COMPLEXES, RUSSIA

2002 ◽  
Vol 40 (2) ◽  
pp. 679-692 ◽  
Author(s):  
A. Y. Barkov ◽  
R. F. Martin ◽  
Y. A. Pakhomovsky ◽  
N. D. Tolstykh ◽  
A. P. Krivenko
Keyword(s):  
Platinum Group Mineral ◽  
Mineral Species ◽  
Group Mineral ◽  
Platinum Group

PASAVAITE, Pd3Pb2Te2, A NEW PLATINUM-GROUP MINERAL SPECIES FROM THE NORIL'SK-TALNAKH Ni-Cu CAMP, RUSSIA

2009 ◽  
Vol 47 (1) ◽  
pp. 53-62 ◽  
Author(s):  
A. Vymazalova ◽  
F. Laufek ◽  
M. Drabek ◽  
J. Haloda ◽  
T. Sidorinova ◽  
...  
Keyword(s):  
Platinum Group Mineral ◽  
Mineral Species ◽  
Group Mineral ◽  
Platinum Group

LAFLAMMEITE, Pd3Pb2S2, A NEW PLATINUM-GROUP MINERAL SPECIES FROM THE PENIKAT LAYERED COMPLEX, FINLAND

2002 ◽  
Vol 40 (2) ◽  
pp. 671-678 ◽  
Author(s):  
A. Y. Barkov ◽  
R. F. Martin ◽  
T. A.A. Halkoaho ◽  
A. J. Criddle
Keyword(s):  
Platinum Group Mineral ◽  
Mineral Species ◽  
Group Mineral ◽  
Platinum Group ◽  
Layered Complex

JACUTINGAITE, Pt2HgSe3, A NEW PLATINUM-GROUP MINERAL SPECIES FROM THE CAUE IRON-ORE DEPOSIT, ITABIRA DISTRICT, MINAS GERAIS, BRAZIL

2012 ◽  
Vol 50 (2) ◽  
pp. 431-440 ◽  
Author(s):  
A. Vymazalova ◽  
F. Laufek ◽  
M. Drabek ◽  
A. R. Cabral ◽  
J. Haloda ◽  
...  
Keyword(s):  
Iron Ore ◽  
Minas Gerais ◽  
Platinum Group Mineral ◽  
Mineral Species ◽  
Ore Deposit ◽  
Group Mineral ◽  
Platinum Group ◽  
Iron Ore Deposit

scholarly journals Gold and platinum group metal mineralisation in the Skaergaard intrusion, southern East Greenland

1990 ◽  
Vol 148 ◽  
pp. 101-103
Author(s):  
T.F.D Nielsen ◽  
H.K Schønwandt
Keyword(s):  
Trace Element ◽  
Platinum Group Metal ◽  
Platinum Metal ◽  
Middle Zone ◽  
Skaergaard Intrusion ◽  
East Greenland ◽  
Group Metal ◽  
Platinum Group

A stratabound gold and platinum metal mineralisation has been located in the Tertiary Skaergaard intrusion of the Kangerdlugssuaq area 68°N in East Greenland. The mineralisation is located in the upper part of the Middle Zone (MZ) of the layered gabbros and appears continuous over c. 40 km2. The mineralisation is 2–5 m thick with gold concentrations up to 5.6 g/t, Pd up to 3.5 g/t and Pt up to 1.5 g/t. Major and trace element distributions indicate that the gold is concentrated in the less mafic layers in the mineralised horizon. It is also concluded that previously reported TiO2 contents of the gabbros and the TiO2 enrichment in the evolving liquids of the intrusion have been underestimated by a factor of 2–3.

A Note on the Origin of Ophitic Texture in the Chilled Olivine Gabbro of the Skaergaard Intrusion

1961 ◽  
Vol 98 (5) ◽  
pp. 353-366 ◽  
Author(s):  
L. R. Wager
Keyword(s):  
Northern Ireland ◽  
Mineral Species ◽  
Olivine Gabbro ◽  
Skaergaard Intrusion ◽  
Magma Type ◽  
Cooling Conditions

AbstractThe textures of the chilled marginal gabbro of the Skaergaard intrusion and of the coarser marginal gabbros 25 yards further in are described and related to counts of the number of separate crystals of the chief mineral species per cubic centimetre of the rock. An explanation of the textures and number of crystal individuals is attempted in terms of various degrees of supersaturation in the magma. In the chilled rock abundant nucleation of plagioclase and olivine, presumably at the middle labile stage of supersaturation, is inferred. This is followed by ophitic or poikilitic crystallization of pyroxene and ilmenite about scarce nuclei, produced at lower temperatures, presumably during the early labile stage of supersaturation for these two minerals. The coarser gabbro, further in from the margin, has about half the number of plagioclase crystals per cm.3 compared with the chilled rock and only one twenty-fifth the number of olivine crystals, and these have a tendency to be ophitic in texture. Under these slower cooling conditions, supersaturation apparently still reached into the middle labile region for plagioclase, giving many nuclei, while olivine, like pyroxene, separated under early labile supersaturation conditions and only relatively few nuclei formed. The contrasting textures of the plateau magma-type basalts of Mull and the tholeiitic basalts of Northern Ireland are explained along similar lines.

scholarly journals Platinum-group mineralization at the margin of the Skaergaard intrusion, East Greenland

2017 ◽  
Vol 52 (6) ◽  
pp. 929-942 ◽  
Author(s):  
Jens C. Ø. Andersen ◽  
Gavyn K. Rollinson ◽  
Iain McDonald ◽  
Christian Tegner ◽  
Charles E. Lesher
Keyword(s):  
Skaergaard Intrusion ◽  
East Greenland ◽  
Platinum Group
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