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GEO-METAMORPHISM  July 2011

GEO-METAMORPHISM July 2011

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Subject:

Re: cataclasites and albitites

From:

Tamoghna Saha <[log in to unmask]>

Reply-To:

Metamorphic Studies Group <[log in to unmask]>

Date:

Mon, 11 Jul 2011 13:04:56 +0530

Content-Type:

text/plain

Parts/Attachments:

Parts/Attachments

text/plain (55 lines)

Sir, I think I am not the guy you wanted to mail to. I am by the way,
a student of metamorphic petrology and work under guidance of Dr S
Karmakar in Jadavpur University, Kolkata, India. So, please
rectification of your sent mail address needed. Thanking you.

                           Yours Faithfully,

                            Tamoghna Saha

On Mon, Jul 11, 2011 at 10:46 AM, Bottrill, Ralph (DIER)
<[log in to unmask]> wrote:
> We have been working on the metamorphic rocks hosting the Savage River
> magnetite deposits, and have found some disagreement about the interpretation
> of some albite-rich cataclastic rocks in the footwall. The metamorphics are
> mostly metamafics, quartzites, dolostones/magnesitestones, amphibolites and
> various muscovite and chlorite schists and skarns.
>
> The albitites have a variety of textures. Some are very fine grained
> and grains are mostly simply twinned or untwinned, typical of metamorphic albite
> (e.g.  photo 1). Some have coarse grains in a fine matrix (eg. fig 2), which
> some have interpreted as porphyritic felsic volcanics, and others as sheared
> porphyroblasts or disaggregated veins. The immobile elements Ti/Zr etc suggest
> an origin from sodic alteration of associated pelites and other metasediments.
>
> But there are also some small (<1m wide) cross-cutting coarse zones,
> interpreted by some as granitoids, which are more Zr-rich - these
> typically contain some quartz and show myrmekitic textures (fig. 3).
> Some of the coarse plagioclase in these bodies shows microcline-like
> Twinning (Fig. 4), suggested by some to be plagioclase replacing microcline(?)
> I have wondered if these coarse zones could be be zones of recrystallised
> cataclasites or zones of partial melting? With remobilised Zr? The rocks
> locally contain calcic to sodic amphiboles and diopside, with maximum
> temperatures to about 600-700oC (magnetite-ilmenite).
>
>
> Has anyone seen similar textures in cataclasites, or have any other thoughts on the origins
> of these rocks?
>
>
> regards
> Ralph Bottrill
> Senior Geologist, Mineralogist and Petrologist
> Metallic Minerals & Geochemistry
> Mineral Resources Tasmania
> PO Box 56, Rosny Park TAS 7018
> Phone: 61 3 6233 8359, Fax:  61 3 6233 8338
> Email: [log in to unmask]  or: [log in to unmask]
>
>
>
>
> CONFIDENTIALITY NOTICE AND DISCLAIMER
> The information in this transmission may be confidential and/or protected by legal professional privilege, and is intended only for the person or persons to whom it is addressed.  If you are not such a person, you are warned that any disclosure, copying or dissemination of the information is unauthorised.  If you have received the transmission in error, please immediately contact this office by telephone, fax or email, to inform us of the error and to enable arrangements to be made for the destruction of the transmission, or its return at our cost.  No liability is accepted for any unauthorised use of the information contained in this transmission.
>

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