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Basal pinacoid
  
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John Betts




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PostPosted: Nov 15, 2012 13:09    Post subject: Basal pinacoid  

Isn't the term "basal pinacoid" redundant? When describing the termination face of the C-axis would "basal" suffice?
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gemlover




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PostPosted: Nov 15, 2012 13:36    Post subject: Re: Basal pinacoid  

Since a "pinacoid" is any pair of parallel crystal faces, basal would describe a particular place/orientation for this pinacoid.

John

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PostPosted: Nov 15, 2012 13:40    Post subject: Re: Basal pinacoid  

Hi John

A pinacoid is not necessarily basal and a "base" could be a pedion for instance and that is not a pinacoid. I'm affraid we need both terms.

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Arturo
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PostPosted: Nov 15, 2012 13:41    Post subject: Re: Basal pinacoid  

Opsss, almost simultaneous answer :-)

(Boths? well it was Both, sorry...)
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PostPosted: Nov 15, 2012 13:59    Post subject: Re: Basal pinacoid  

Thanks.
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Pete Richards
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PostPosted: Nov 15, 2012 15:10    Post subject: Re: Basal pinacoid  

It could be argued that for some symmetry classes the term "basal pinacoid" is redundant. For trigonal bar-3 2/m, the symmetry class of calcite, there is only one pinacoid and it is basal. Hence the term "basal" is unnecessary. But I don't think it really hurts anything to specify it anyway.

Trigonal, hexagonal, and tetragonal symmetry classes that have a mirror plane perpendicular to the unique axis all have this property, that their only pinacoid is basal.

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Antonio Alcaide
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PostPosted: Nov 15, 2012 16:04    Post subject: Re: Basal pinacoid  

Pete Richards wrote:
Trigonal, hexagonal, and tetragonal symmetry classes that have a mirror plane perpendicular to the unique axis all have this property, that their only pinacoid is basal.


Well, I think the trouble for the amateur collector -nearly none of you, who are contributing to this thread- is that we usually forget pinacoid refers to two faces, as John -gemlover- reminded us. This is the reason why I can understand hexagonal symmetry has only one (basal) pinacoid. The tendency -for amateurs I insist- is to consider one of the faces as the pinacoid.

For example, in doubly terminated hanksite crystals -or pyromorphite, mimetite, etc.- I called erroneusly "basal pinacoid" only the face down the crystal. ¿And the other?

I hope to have explained the point well.

Regards.

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