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GeneralIntergrowth texture?

7th Feb 2018 21:02 UTCKyle Beucke 🌟

01143270015244381428872.jpg
Hello,


Here are two backscattered images of goldfieldite (or its oxidation products) (=dark gray) and a bismuth-selenium mineral (lightest gray, almost white = unoxidized and slightly darker gray=oxidized).

01430110015652932598517.jpg



I am trying to decide if this represents a contemporaneous intergrowth, or if the bismuth-selenium mineral came in later than the goldfieldite. Both images show "islands" of goldfieldite in the bismuth-selenium phase, which seems to suggest that the bismuth-selenium phase is later.


Another thing: Do bismuth minerals weather more rapidly (in general) than copper sulfosalts?


Thank you,


Kyle

8th Feb 2018 10:43 UTCDavid Von Bargen Manager

You also should consider symplectite intergrowths (breakdown of unstable phase to two distinct minerals). It can be fairly common in sulfides/sulfosalts.

8th Feb 2018 10:50 UTCUwe Kolitsch Manager

Kyle: this might be interesting for you:

Craig, J. R. (2001): Ore-mineral textures and the tales they tell. Canadian Mineralogist 39, 937-956.


Sulfides/sulfosalts with lower melting points generally crystallise later in a given paragenesis and may envelop or replace earlier crystallised sulfides/sulfosalts.

9th Feb 2018 20:54 UTCKyle Beucke 🌟

Thank you both!


Kyle
 
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