Dear Andrew,
What I have received is a bit different.
I had also the text/plain and html parts but I have another one too. This
was an attachment called READER_DIGEST_LETTER.txt.pif .
If decoded and opened it starts spreading in the WINDOWS directory. Now I
have the report of the AntiVirus, it is W95.MTX which has also a warm
component infected with the same virus that spreads through e-mail. It also
patches WSOCK32.DLL.
I am still running after it instead of seeing of my work. I am terribly
upset upon this incident because threatens my recent data deposited on this
computer.
Yours,
Cris
> Hi Cris,
>
> > Are you sure? In my computer it triggered the Norton AntiVirus which
> > identified copies of something called Win95MTX (I do not remember the
> exact
> > name; I am still shivering) in many files under C:\windows
>
> I'm 100% sure that I didn't receive anything resembling any virus. It was
> a two part message, part one is text/plain and the second is text/html.
> Standard format for Outlook Express 5. I've inserted the decoded text at
> the bottom of this message to asuage any doubts. There is no Javascript,
> DirectX or actually anything which isn't just a text email message.
>
> My mail server may have stripped an attachment if it thought it was
> infected, but there's no sign of any message to this effect in the body or
> headers of the message.
>
> Cheers,
>
> Andrew
>
> =====Part 1=====
>
> Dear Dr. Mayer,
>
> There is a calculated fractionation factor by me for the siderite-water
> system in Geochem. J. 33:109-126 (1999), but it is essentially identical
> to the experimental data of Carothers et al. (1988).
>
> The large variation in d13C but a constant d18O value for your siderite
> may result from a large variation in sedimentary environment (particularly
> CO2 input), whereas the oxygen isotope ratios of carbonate is
> predominantly governed by H2O which is of a great amount relative to CO2.
>
> Sincerely,
> Yong-Fei Zheng
>
> **************************************************************************
> **********
> Dr. Yong-Fei Zheng
> Professor and Chairman
> Department of Earth and Space Sciences
> University of Science and Technology of China
> Hefei 230026, PR China
> Tel.: (+86) 551 3603384 Fax: (+86) 551 3603554
> Email: [log in to unmask]
> **************************************************************************
> **********
>
>
> ----- Original Message -----
> 发件人: Bernhard Mayer
> 收件人: [log in to unmask]
> 发送时紒E 2000膩E1月14日 6:23
> 主虂E Oxygen isotope ratios of siderite
>
>
> Dear colleagues:
>
> Is there anything known about the temperature dependence of the
> equilibrium
> isotope exchange between oxygen in water and oxygen in siderite (FeCO3)?
> I
> consulted Friedman & O'Neil (1977) without success.
>
> Background: I have recently analyzed the carbon and oxygen isotope
> ratios of
> siderites from laminated lake sediments of early Holocene age. The
> siderites
> are believed to be a primary formation under reducing conditions at the
> water/sediment interface of a Fe-rich, Ca-poor freshwater lake. The
> shifts
> in carbon isotope ratios of the siderites from the lake sediment
> sequence
> agree nicely with known climatic and paleoenvironmental changes at the
> time.
> However, the oxygen isotope ratios in the siderites do not.
>
> Any suggestions would be welcome.
>
> Cheers,
>
> Bernhard
>
> Bernhard Mayer
> Associate Professor
> University of Calgary
> Departments of Physics and Astronomy
> and Geology and Geophysics
> 2500 University Drive NW
> Calgary, Alberta
> Canada T2N 1N4
> phone (403) 220-5389
> fax (403) 220-7773
> e-mail: [log in to unmask]
>
>
> =====Part 2=====
>
> <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN">
> <HTML><HEAD>
> <META content="text/html; charset=gb2312" http-equiv=Content-Type>
> <META content="MSHTML 5.00.2919.6307" name=GENERATOR>
> <STYLE></STYLE>
> </HEAD>
> <BODY bgColor=#ffffff>
> <DIV><FONT face="Times New Roman" size=4>Dear Dr. Mayer,</FONT></DIV>
> <DIV> </DIV>
> <DIV><FONT face="Times New Roman" size=4>There is a calculated
> fractionation
> factor by me for the siderite-water system in Geochem. J. 33:109-126
> (1999), but
> it is essentially identical to the experimental data of Carothers et al.
> (1988).
> </FONT></DIV>
> <DIV> </DIV>
> <DIV><FONT face="Times New Roman" size=4>The large variation in
> d13C but a
> constant d18O value for your siderite may result from a large variation in
> sedimentary environment (particularly CO2 input), whereas the oxygen
> isotope
> ratios of carbonate is predominantly governed by H2O which is of a great
> amount
> relative to CO2.</FONT></DIV>
> <DIV> </DIV>
> <DIV><FONT face="Times New Roman" size=4>Sincerely,</FONT></DIV>
> <DIV><FONT face="Times New Roman" size=4>Yong-Fei Zheng</FONT></DIV>
> <DIV> </DIV>
> <DIV>*********************************************************************
> ***************<BR>Dr.
> Yong-Fei Zheng<BR>Professor and Chairman<BR>Department of Earth and Space
> Sciences<BR>University of Science and Technology of China<BR>Hefei 230026,
> PR
> China<BR>Tel.: (+86) 551 3603384
> Fax:
> (+86) 551 3603554<BR>Email: <A
> href="mailto:[log in to unmask]">[log in to unmask]</A><BR>*************
> ***********************************************************************</D
> IV>
> <DIV> </DIV>
> <DIV> </DIV>
> <BLOCKQUOTE
> style="BORDER-LEFT: #000000 2px solid; MARGIN-LEFT: 5px; MARGIN-RIGHT:
> 0px; PADDING-LEFT: 5px; PADDING-RIGHT: 0px">
> <DIV style="FONT: 10pt 宋虂E>----- Original Message ----- </DIV>
> <DIV style="BACKGROUND: #e4e4e4; FONT: 10pt 宋虂E font-color:
> black"><B>发件人:</B>
> <A href="mailto:[log in to unmask]"
> [log in to unmask]>Bernhard Mayer</A> </DIV>
> <DIV style="FONT: 10pt 宋虂E><B>收件人:</B> <A
> href="mailto:[log in to unmask]"
> [log in to unmask]>[log in to unmask]</A> </DIV>
> <DIV style="FONT: 10pt 宋虂E><B>发送时紒E</B> 2000膩E1月14日 6:23</DIV>
> <DIV style="FONT: 10pt 宋虂E><B>主虂E</B> Oxygen isotope ratios of
> siderite</DIV>
> <DIV><BR></DIV>Dear colleagues:<BR><BR>Is there anything known about the
> temperature dependence of the equilibrium<BR>isotope exchange between
> oxygen
> in water and oxygen in siderite (FeCO3)? I<BR>consulted Friedman &
> O'Neil
> (1977) without success.<BR><BR>Background: I have recently analyzed the
> carbon
> and oxygen isotope ratios of<BR>siderites from laminated lake sediments
> of
> early Holocene age. The siderites<BR>are believed to be a primary
> formation
> under reducing conditions at the<BR>water/sediment interface of a
> Fe-rich,
> Ca-poor freshwater lake. The shifts<BR>in carbon isotope ratios of the
> siderites from the lake sediment sequence<BR>agree nicely with known
> climatic
> and paleoenvironmental changes at the time.<BR>However, the oxygen
> isotope
> ratios in the siderites do not.<BR><BR>Any suggestions would be
> welcome.<BR><BR>Cheers,<BR><BR>Bernhard<BR><BR>Bernhard
> Mayer<BR>Associate
> Professor<BR>University of Calgary<BR>Departments of Physics and
> Astronomy<BR>and Geology and Geophysics<BR>2500 University Drive
> NW<BR>Calgary, Alberta<BR>Canada T2N 1N4<BR>phone (403) 220-5389<BR>fax
> (403)
> 220-7773<BR>e-mail: <A
>
> href="mailto:[log in to unmask]">[log in to unmask]
> a</A><BR></BLOCKQUOTE></BODY></HTML>
>
>
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