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Isocubanite Mineral Data
General Isocubanite Information ... Isocubanite Image ... Isocubanite Crystallography...
39k - 6 sec @ 56k
webmineral.com/data/Isocubanite.shtml webmineral.com/data/Isocubanite.shtml
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Isochalcopyrite Mineral Data
General Isochalcopyrite Information ... Deep sea, anoxic sediments. Generally regarded as isocubanite. ... Discredited IMA 2006...
16k - 2 sec @ 56k
webmineral.com/data/Isochalcopyrite.shtml
Isocubanite, a new definition of the cubic polymorph of cubanite ...
Isocubanite is a cubic polymorph ofcubanite CuFezS3, discovered in the submarine ... and iss; the name isocubanite, proposed in order to clarify the ...
rruff.geo.arizona.edu/doclib/mm/vol52/MM52_509.pdf
Isocubanite from sulfide ores of the rainbow hydrothermal field ...
Later, isocubanite was detected in numerous hydrothermal sulfide structures of different ocean regions, and it was always regarded as natural analog of the ...
26k - 4 sec @ 56k
cat.inist.fr/?aModele=afficheN&cpsidt=14678987
Photochemically accelerated surface-diffusion of silver on ...
Automatic download [Begin manual download]. Downloading the PDF version of: Can Mineral Jeppsson 26 (4): 973. (2569K) ...
canmin.geoscienceworld.org/cgi/reprint/26/4/973
Photochemically accelerated surface-diffusion of silver on
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canmin.geoscienceworld.org/cgi/content/abstract/26/4/97... canmin.geoscienceworld.org/cgi/content/abstract/26/4/973
Results and Discussion
in particular the abundance of isocubanite and chalcopyrite was significantly higher in the Deep Copper Zone than had been reported from any part of the massive sulfide body. The massive sulfide at Bent Hill is predominantly pyrite and pyrrhotite, with much lower abundance of sphalerite, chalcopyrite, and magnetite (Fig.
99k - 14 sec @ 56k
www-odp.tamu.edu/publications/169_SR/chap_05/c5_5.htm
Figure F7.
Figure F7. Reflected-light photomicrographs of (A) Sample 169-856H-31R-2, 1-5 cm, from the Deep Copper Zone beneath Bent Hill Massive Sulfide deposit, (B) Sample 169-1035H-19R-1, 58-62 cm, from the Deep Copper Zone beneath ODP Mound, and (C) Section The host mineral is isocubanite, and the lamellae are chalcopyrite.
99k - 14 sec @ 56k
www-odp.tamu.edu/publications/169_SR/chap_05/c5_f7.htm
Teagle et al (PDF File)
Similar styles of alteration are present in both the sills and flows, ... There are steep min-eralogical, chemical, and isotopic alteration gradients from the highly altered basalt-sediment interfaces down to the less altered flow interiors, suggesting the channeling of hydrothermal fluids along the ... (87Sr/86Sr = 0.7046).
319k - 46 sec @ 56k
www.segweb.org/EG/papers/Abs99-3_files/07Teagle.pdf
http://www.maden.hacettepe.edu.tr/dmmrt/dmmrt295.html
Next page Previous page ... a. A sandstone in which the quartz grains have been enlarged by deposition of silica so that the grains show regenerated crystal facets and sometimes nearly perfect quartz euhedra. ... An orthorhombic mineral, CuFe2 S3 ; dimorphous with isocubanite. Formerly called chalmersite.
76k - 11 sec @ 56k
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www.maden.hacettepe.edu.tr/dmmrt/dmmrt295.html
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