Daliranite occurs as hair-like crystals, in appearance similar to ludlockite. This beautiful new species is a new sulfosalt from the Zarshouran Au-As deposit, Iran, published in late 2009. Only a small number of these pieces were recovered and then studied. This is one of the largest extant specimens and is co-type material, which I obtained by exchange from the collection of Dr. Werner Paar of the University of Salzburg. Dr. Paar is lead author on the publication of the species (Mineralogical Magazine, Oct. 2009, vol. 73 #5.) Daliranite occurs as very rich orange-red crystals, eye visible but sub-mm in size, easily seen on this contrasting matrix specimen of quartz. It is associated with orpiment and other related species (he has identified both galkhaite and cinnabar as present on this piece). This specimen is a large, display-worthy piece. The orpiment veins and crystals make this an attractive piece, overall. These specimens were found in 1998-2002 and studied only later, in Germany. Return trips by the authors in 2005, to the dumps, were unsuccessful at finding more daliranite and it remains today a fairly rare species, thus. Originally, and erroneously, reported as ludlockite from Zarehehuran, Takap, Takht-e-Suleiman massif, Azerbaijan. Apparently, it was rather difficult to analyze and presented a fair challenge to the crystallographers. Type and only locality material. Co-type material.
Omistamine: Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
Tohid:
jagada – teost kopeerida, levitada ja edastada
kohandada – valmistada muudetud teoseid
Järgmistel tingimustel:
omistamine – Pead materjali sobival viisil autorile omistama, tooma ära litsentsi lingi ja märkima ära, kas on tehtud muudatusi. Sobib, kui teed seda mõistlikul viisil, kuid seejuures ei tohi jääda muljet, et litsentsiandja tõstab esile sind või seda, et sina materjali kasutad.
sarnaselt jagamine – Kui töötled, kujundad ümber või arendad materjali edasi, siis pead oma töö levitamiseks kasutama sama litsentsi, mille all on algupärand, või ühilduvat litsentsi.
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