| Current Path : /proc/thread-self/root/home/ift/mails/28/ |
Linux ift1.ift-informatik.de 5.4.0-216-generic #236-Ubuntu SMP Fri Apr 11 19:53:21 UTC 2025 x86_64 |
| Current File : //proc/thread-self/root/home/ift/mails/28/1516349263.zrspam.286395_2018_01_19 |
From 26304-19791-181300-4694-christian.gabriel=ift-informatik.de@mail.bestofferss.bid Fri Jan 19 09:07:43 2018
Return-Path: <26304-19791-181300-4694-christian.gabriel=ift-informatik.de@mail.bestofferss.bid>
X-Original-To: cgabriel@ift-informatik.de
Delivered-To: cgabriel@ift-informatik.de
Received: by ift-informatik.de (Postfix, from userid 5555)
id C2B981C881AB5; Fri, 19 Jan 2018 09:07:43 +0100 (CET)
Received: from localhost by h2486555.stratoserver.net
with SpamAssassin (version 3.4.0);
Fri, 19 Jan 2018 09:07:43 +0100
From: "HornyAffairs" <girlsparti@girlsparti.com>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** These chicks are looking for a booty call
Date: Fri, 19 Jan 2018 02:55:36 -0500
Message-Id: <youhj4mtlf7vbh19-7tdp3aurwa69k082-2c434@girlsparti.com>
X-Spam-Checker-Version: SpamAssassin 3.4.0 (2014-02-07) on
h2486555.stratoserver.net
X-Spam-Flag: YES
X-Spam-Level: *****
X-Spam-Status: Yes, score=5.8 required=5.0 tests=BAYES_00,DKIM_ADSP_NXDOMAIN,
HTML_FONT_LOW_CONTRAST,HTML_IMAGE_ONLY_32,HTML_MESSAGE,RAZOR2_CF_RANGE_51_100,
RAZOR2_CF_RANGE_E8_51_100,RAZOR2_CHECK,RCVD_IN_PSBL,RDNS_NONE,T_REMOTE_IMAGE,
URIBL_BLOCKED autolearn=no autolearn_force=no version=3.4.0
MIME-Version: 1.0
Content-Type: multipart/mixed; boundary="----------=_5A61A74F.925D02BA"
This is a multi-part message in MIME format.
------------=_5A61A74F.925D02BA
Content-Type: text/plain; charset=iso-8859-1
Content-Disposition: inline
Content-Transfer-Encoding: 8bit
Spam detection software, running on the system "h2486555.stratoserver.net",
has identified this incoming email as possible spam. The original
message has been attached to this so you can view it or label
similar future email. If you have any questions, see
@@CONTACT_ADDRESS@@ for details.
Content preview: These chicks are looking for a booty call http://bestofferss.bid/Sb0oZEXVMQ2T1CVehITQ-G6tqbAS_lj-uoeHyGMQ0MXaOQGE
http://bestofferss.bid/r7aY-KtFZztYbMnWn3yRW9joNYOTUOCbQh6Mm-XT5tTDdE-q In
geology, the crust is the outermost solid shell of a rocky planet, dwarf
planet, or natural satellite/ It is usually distinguished from the underlying
mantle by its chemical makeup; however, in the case of icy satellites, it
may be distinguished based on its phase (solid crust vs/ liquid mantle)/
The crusts of Earth, Moon, Mercury, Venus, Mars, Io, and other planetary bodies
formed via igneous processes, and were later modified by erosion, impact
cratering, volcanism, and sedimentation/Most terrestrial planets have fairly
unThe continental crust has an average composition similar to that of andesite/
The most abundant minerals in Earth's continental crust are feldspars, which
make up about 41/ of the crust by weight, followed by quartz at 12/, and
pyroxenes at 11// Continental crust is enriched in incompatible elements compared
to the basaltic ocean crust and much enriched compared to the underlying
mantle/ Although the continental crust comprises only about 0/6 weight percent
of the silicate on Earth, it contains 20/ to 70/ of the incompatible elements/iform
crusts/ Earth, however, has two distinct types continental crust and oceanic
crust/ These two types have different chemical compositions and physical
properties, and were formed by different geological processes/ [...]
Content analysis details: (5.8 points, 5.0 required)
pts rule name description
---- ---------------------- --------------------------------------------------
0.0 URIBL_BLOCKED ADMINISTRATOR NOTICE: The query to URIBL was blocked.
See
http://wiki.apache.org/spamassassin/DnsBlocklists#dnsbl-block
for more information.
[URIs: 1b.yt]
2.7 RCVD_IN_PSBL RBL: Received via a relay in PSBL
[104.168.87.156 listed in psbl.surriel.com]
0.9 DKIM_ADSP_NXDOMAIN No valid author signature and domain not in DNS
-1.9 BAYES_00 BODY: Bayes spam probability is 0 to 1%
[score: 0.0000]
0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or identical to
background
0.0 HTML_MESSAGE BODY: HTML included in message
0.0 HTML_IMAGE_ONLY_32 BODY: HTML: images with 2800-3200 bytes of words
1.9 RAZOR2_CF_RANGE_E8_51_100 Razor2 gives engine 8 confidence level
above 50%
[cf: 100]
0.9 RAZOR2_CHECK Listed in Razor2 (http://razor.sf.net/)
0.5 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
[cf: 100]
0.8 RDNS_NONE Delivered to internal network by a host with no rDNS
0.0 T_REMOTE_IMAGE Message contains an external image
The original message was not completely plain text, and may be unsafe to
open with some email clients; in particular, it may contain a virus,
or confirm that your address can receive spam. If you wish to view
it, it may be safer to save it to a file and open it with an editor.
------------=_5A61A74F.925D02BA
Content-Type: message/rfc822; x-spam-type=original
Content-Description: original message before SpamAssassin
Content-Disposition: attachment
Content-Transfer-Encoding: 8bit
Received: from boston.bestofferss.bid (unknown [104.168.87.156])
by ift-informatik.de (Postfix) with ESMTP id B09D11C88124E
for <christian.gabriel@ift-informatik.de>; Fri, 19 Jan 2018 09:07:41 +0100 (CET)
Mime-Version: 1.0
Content-Type: multipart/alternative; boundary="5b6ed6dfae254b609c8c67327a8acb54_4d4f_2c434"
Date: Fri, 19 Jan 2018 02:55:36 -0500
From: "HornyAffairs" <girlsparti@girlsparti.com>
Reply-To: "HornyAffairs" <girlsparti@girlsparti.com>
Subject: These chicks are looking for a booty call
To: <christian.gabriel@ift-informatik.de>
Message-ID: <youhj4mtlf7vbh19-7tdp3aurwa69k082-2c434@girlsparti.com>
--5b6ed6dfae254b609c8c67327a8acb54_4d4f_2c434
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
These chicks are looking for a booty call
http://bestofferss.bid/Sb0oZEXVMQ2T1CVehITQ-G6tqbAS_lj-uoeHyGMQ0MXaOQGE
http://bestofferss.bid/r7aY-KtFZztYbMnWn3yRW9joNYOTUOCbQh6Mm-XT5tTDdE-q
In geology, the crust is the outermost solid shell of a rocky planet, dwarf planet, or natural satellite/ It is usually distinguished from the underlying mantle by its chemical makeup; however, in the case of icy satellites, it may be distinguished based on its phase (solid crust vs/ liquid mantle)/
The crusts of Earth, Moon, Mercury, Venus, Mars, Io, and other planetary bodies formed via igneous processes, and were later modified by erosion, impact cratering, volcanism, and sedimentation/Most terrestrial planets have fairly unThe continental crust has an average composition similar to that of andesite/ The most abundant minerals in Earth's continental crust are feldspars, which make up about 41/ of the crust by weight, followed by quartz at 12/, and pyroxenes at 11// Continental crust is enriched in incompatible elements compared to the basaltic ocean crust and much enriched compared to the underlying mantle/ Although the continental crust comprises only about 0/6 weight percent of the silicate on Earth, it contains 20/ to 70/ of the incompatible elements/iform crusts/ Earth, however, has two distinct types continental crust and oceanic crust/ These two types have different chemical compositions and physical properties, and were formed by different geological processes/
--5b6ed6dfae254b609c8c67327a8acb54_4d4f_2c434
Content-Type: text/html;
Content-Transfer-Encoding: 8bit
<html>
<head>
<title></title>
</head>
<body><a href="http://bestofferss.bid/-dHJJiAGSsJADLaBg-hz4-EzPWkmi-bIvAlvu4QtOH7beIy0"><img src="http://bestofferss.bid/f664aa83f4c22340ad.jpg" /><img height="1" src="http://www.bestofferss.bid/6aG4oS7Wj2lPcKR7r884MdWoSOHcvN9qtQUO8HHo9dZ8BX01" width="1" /></a>
<center>
<table width="600">
<tbody>
<tr>
<td align="center">
<div style="float:right;"><a href="http://1b.yt/eY0C9"><img alt=" " src="http://bestofferss.bid/73a64ecd6b48ebf224.jpg" /></a></div>
<center>
<h1 style="padding:5px; font-size:28px;width:600px;text-align:center;background-color:#ebebeb;"><a href="http://bestofferss.bid/Sb0oZEXVMQ2T1CVehITQ-G6tqbAS_lj-uoeHyGMQ0MXaOQGE" style="text-decoration:none; "><b style="color:#d22dd0;"><strong>These chicks are looking for a booty call</strong></b></a></h1>
<br />
<a href="http://bestofferss.bid/Sb0oZEXVMQ2T1CVehITQ-G6tqbAS_lj-uoeHyGMQ0MXaOQGE"><img src="http://bestofferss.bid/837a6a86e4f5b1972c.jpg" /></a></center>
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<center><a href="http://bestofferss.bid/QXkGduj7LjFMBv-bzK5eNMwAeOAvgvO6erHz5q4SPAfPff3l"><img alt=" " src="http://bestofferss.bid/4088a36a6d7395a79f.jpg" /></a><br />
<br />
<br />
<br />
<span style="font-size:8px;color:#FFFFFF">In geology, the crust is the outermost solid shell of a rocky planet, dwarf planet, or natural satellite/ It is usually distinguished from the underlying mantle by its chemical makeup; however, in the case of icy satellites, it may be distinguished based on its phase (solid crust vs/ liquid mantle)/ The crusts of Earth, Moon, Mercury, Venus, Mars, Io, and other planetary bodies formed via igneous processes, and were later modified by erosion, impact cratering, volcanism, and sedimentation/Most terrestrial planets have fairly unThe continental crust has an average composition similar to that of andesite/ The most abundant minerals in Earth's continental crust are feldspars, which make up about 41/ of the crust by weight, followed by quartz at 12/, and pyroxenes at 11// Continental crust is enriched in incompatible elements compared to the basaltic ocean crust and much enriched compared to the underlying mantle/ Although the continental crust comprises only about 0/6 weight percent of the silicate on Earth, it contains 20/ to 70/ of the incompatible elements/iform crusts/ Earth, however, has two distinct types continental crust and oceanic crust/ These two types have different chemical compositions and physical properties, and were formed by different geological processes/ </span><br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<a href="http://bestofferss.bid/r7aY-KtFZztYbMnWn3yRW9joNYOTUOCbQh6Mm-XT5tTDdE-q"><img src="http://bestofferss.bid/1ddc9f0317f1573213.jpg" style="width: 305px; height: 51px;" /></a></center>
<br />
</td>
</tr>
</tbody>
</table>
</center>
</body>
</html>
--5b6ed6dfae254b609c8c67327a8acb54_4d4f_2c434--
------------=_5A61A74F.925D02BA--