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Stable Isotope Geochemistry

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from bock.ucs.ualberta.ca (bock.ucs.ualberta.ca [129.128.5.214]) by elk.uvm.edu (8.7.3/8.7.3) with SMTP id JAA85720 for <[log in to unmask]>; Thu, 4 Apr 1996 09:57:00 -0500 from maildrop.srv.ualberta.ca by bock.ucs.ualberta.ca with ESMTP (8.6.5/UA3.0.0June95) id HAA24838 for <[log in to unmask]>; Thu, 4 Apr 1996 07:56:56 -0700 from gpu1.srv.ualberta.ca (gpu1.srv.ualberta.ca [129.128.98.10]) by maildrop.srv.ualberta.ca (8.7.1/8.7.1) with SMTP id HAA33412 for <[log in to unmask]>; Thu, 4 Apr 1996 07:56:57 -0700
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Date:
Thu, 4 Apr 1996 07:56:56 -0700 (MST)
Subject:
Re: oxygen isotopes on opal, me too
From:
Karlis Muehlenbachs <[log in to unmask]>
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Dear Zach,

Iam not sure what exchanges.  All I saw was that the delta 18-O increases
several per mille after drying for various times.

Karlis

On Thu, 4 Apr 1996, Zachary Sharp wrote:

> Date: Thu, 04 Apr 1996 14:59:20 +0100
> From: Zachary Sharp <[log in to unmask]>
> Reply-To: [log in to unmask]
> To: [log in to unmask]
> Subject: Re: oxygen isotopes on opal, me too
>
> Dear Karlis,
>
> What actually is exchanging?  Is it the oxygen in the "surface water", the
> oxygen in the "structural water", or the tetrahedrally-bound oxygen?
>
> >Zach
> Zachary Sharp
> Institute of Mineralogy
> University of Lausanne, BFSH-2
> CH-1015 Lausanne
> Switzerland
>
>


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