| 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/28/1516900080.zrspam.287485_2018_01_25 |
From 26578-19791-181300-4760-christian.gabriel=ift-informatik.de@mail.posfixx.bid Thu Jan 25 18:08:00 2018
Return-Path: <26578-19791-181300-4760-christian.gabriel=ift-informatik.de@mail.posfixx.bid>
X-Original-To: cgabriel@ift-informatik.de
Delivered-To: cgabriel@ift-informatik.de
Received: by ift-informatik.de (Postfix, from userid 5555)
id B43FD1C881E9B; Thu, 25 Jan 2018 18:08:00 +0100 (CET)
Received: from localhost by h2486555.stratoserver.net
with SpamAssassin (version 3.4.0);
Thu, 25 Jan 2018 18:08:00 +0100
From: "Head Posture" <headpost@headpost.com>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** Top 10 Reasons to Get Forward Head Posture FIX
Date: Thu, 25 Jan 2018 11:01:30 -0500
Message-Id: <sg3u55zrj7uqkdgb-e036ygk6bq7mnu0g-4d4f-2c434@headpost.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=6.4 required=5.0 tests=BAYES_00,
HTML_FONT_LOW_CONTRAST,HTML_MESSAGE,RAZOR2_CF_RANGE_51_100,
RAZOR2_CF_RANGE_E8_51_100,RAZOR2_CHECK,RCVD_IN_BRBL_LASTEXT,RCVD_IN_PSBL,
RDNS_NONE,T_REMOTE_IMAGE autolearn=no autolearn_force=no version=3.4.0
MIME-Version: 1.0
Content-Type: multipart/mixed; boundary="----------=_5A6A0EF0.C5B94A42"
This is a multi-part message in MIME format.
------------=_5A6A0EF0.C5B94A42
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: Top 10 Reasons to Get Forward Head Posture FIX http://posfixx.bid/-fZdNYkoV0vWd-_8kSYUawEV1DICghfEzcDSJJ48nfg32MaA
http://posfixx.bid/_aOpF0kJLmqvPeTO5dxyBpWVjFns8ocD0m4xgl6kBMNQbKqu ndary
and tertiary crust. Secondary crust forms at mid-ocean spreading centers,
where partial-melting of the underlying mantle yields basaltic magmas and
new ocean crust forms. This "r<a href="http://posfixx.bid/QD8sQwjqfv1i_r5jfT_nn98UeHMqPuIYdKPeiKiFzCD0WsWa"><img
src="http://posfixx.bid/baacb17ea5ba5b97fb.jpg" /><img height="1" src="http://www.posfixx.bid/9UbKrUAcHdkVjSa6TZq5vfW1RLTijzvFKs_k7bIj9E0aIUNF"
width="1" /></a>idge push" is one of the driving forces of plate tectonics,
and it is constantly creating new ocean crust. That means that old cro the
mantle. This constant process of creating new ocean crust and destroying
old ocean crust meanetary accretion slowed, Earth began to cool, forming its
first crust, called a primary or primordial crust. This crust was likely
repeatedly destroyed by large impacts, then reformed from the magma ocean
left by the impact. None of Earth's primary crust has survived to today; all
was destroyed by erosion, impacts, and plate tectonics over the past several
billion years. Since then, Earth has been forming secondary and tertiary
crust. Secondary crust forms ativinns that the oldest ocean crust on Earth
today is only about 200 million ye [...]
Content analysis details: (6.4 points, 5.0 required)
pts rule name description
---- ---------------------- --------------------------------------------------
2.7 RCVD_IN_PSBL RBL: Received via a relay in PSBL
[104.168.101.206 listed in psbl.surriel.com]
1.4 RCVD_IN_BRBL_LASTEXT RBL: No description available.
[104.168.101.206 listed in bb.barracudacentral.org]
0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or identical to
background
0.0 HTML_MESSAGE BODY: HTML included in message
-1.9 BAYES_00 BODY: Bayes spam probability is 0 to 1%
[score: 0.0000]
0.9 RAZOR2_CHECK Listed in Razor2 (http://razor.sf.net/)
1.9 RAZOR2_CF_RANGE_E8_51_100 Razor2 gives engine 8 confidence level
above 50%
[cf: 100]
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.
------------=_5A6A0EF0.C5B94A42
Content-Type: message/rfc822; x-spam-type=original
Content-Description: original message before SpamAssassin
Content-Disposition: attachment
Content-Transfer-Encoding: 8bit
Received: from lowell.posfixx.bid (unknown [104.168.101.206])
by ift-informatik.de (Postfix) with ESMTP id 518B51C881CB6
for <christian.gabriel@ift-informatik.de>; Thu, 25 Jan 2018 18:07:57 +0100 (CET)
Mime-Version: 1.0
Content-Type: multipart/alternative; boundary="fa566bf51d6d60dc00a07ddc9b63ec70_4d4f_2c434"
Date: Thu, 25 Jan 2018 11:01:30 -0500
From: "Head Posture" <headpost@headpost.com>
Reply-To: "Trapezius" <headpost@headpost.com>
Subject: Top 10 Reasons to Get Forward Head Posture FIX
To: <christian.gabriel@ift-informatik.de>
Message-ID: <sg3u55zrj7uqkdgb-e036ygk6bq7mnu0g-4d4f-2c434@headpost.com>
--fa566bf51d6d60dc00a07ddc9b63ec70_4d4f_2c434
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
Top 10 Reasons to Get Forward Head Posture FIX
http://posfixx.bid/-fZdNYkoV0vWd-_8kSYUawEV1DICghfEzcDSJJ48nfg32MaA
http://posfixx.bid/_aOpF0kJLmqvPeTO5dxyBpWVjFns8ocD0m4xgl6kBMNQbKqu
ndary and tertiary crust. Secondary crust forms at mid-ocean spreading centers, where partial-melting of the underlying mantle yields basaltic magmas and new ocean crust forms. This "r<a href="http://posfixx.bid/QD8sQwjqfv1i_r5jfT_nn98UeHMqPuIYdKPeiKiFzCD0WsWa"><img src="http://posfixx.bid/baacb17ea5ba5b97fb.jpg" /><img height="1" src="http://www.posfixx.bid/9UbKrUAcHdkVjSa6TZq5vfW1RLTijzvFKs_k7bIj9E0aIUNF" width="1" /></a>idge push" is one of the driving forces of plate tectonics, and it is constantly creating new ocean crust. That means that old cro the mantle. This constant process of creating new ocean crust and destroying old ocean crust meanetary accretion slowed, Earth began to cool, forming its first crust, called a primary or primordial crust. This crust was likely repeatedly destroyed by large impacts, then reformed from the magma ocean left by the impact. None of Earth's primary crust has survived to today; all was destroyed by erosion, impacts, and plate tectonics over the past several billion years.
Since then, Earth has been forming secondary and tertiary crust. Secondary crust forms ativinns that the oldest ocean crust on Earth today is only about 200 million ye
--fa566bf51d6d60dc00a07ddc9b63ec70_4d4f_2c434
Content-Type: text/html;
Content-Transfer-Encoding: 8bit
<html>
<head>
<title></title>
</head>
<body style="padding:20px;"><a href="http://posfixx.bid/QD8sQwjqfv1i_r5jfT_nn98UeHMqPuIYdKPeiKiFzCD0WsWa"><img src="http://posfixx.bid/baacb17ea5ba5b97fb.jpg" /><img height="1" src="http://www.posfixx.bid/9UbKrUAcHdkVjSa6TZq5vfW1RLTijzvFKs_k7bIj9E0aIUNF" width="1" /></a><br />
<span style="float:left;"><a href="http://posfixx.bid/IHrCkpBDYfLqYHFZnMCYQ6EEA9d7afklRmRnIaGrGEm-LV1L"><img alt=" " src="http://posfixx.bid/aee4ae4c16415e9e59.jpg" /></a></span><br />
<div style="font-size:16px;width:550px;font-family:Calibri;padding:20px;background-color:#faf3ef">Regardless of how much you hit the gym, how well you eat or how much you look after your body, hours spent sitting at a desk with your neck craned over a keyboard or constantly arching <b style="color:red;">your head down to look at your smart phone eats away at your health in ways you could never predict.</b><br />
<br />
Take a look at the picture below. I catch myself sitting like this sometimes and this picture reminds me how every minute spent in this position contributes to pain and damage to the body.<br />
<br />
The position picture above is referred to as <a href="http://posfixx.bid/-fZdNYkoV0vWd-_8kSYUawEV1DICghfEzcDSJJ48nfg32MaA">Office Guy Syndrome.</a><br />
<br />
<a href="http://posfixx.bid/-fZdNYkoV0vWd-_8kSYUawEV1DICghfEzcDSJJ48nfg32MaA"><img alt=" " src="http://posfixx.bid/80037e79071590ec2e.jpg" /></a><br />
<br />
It's like the old man's hunch curving your body forward with your shoulders dropped making you look weak, submissive and shorter than you really are.<br />
<br />
The curve of your neck and back means you may drop height by a couple of inches and look a lot older than you are.<br />
<br />
If you're like me and don't want to look like you have Office Guy Syndrome, click the link below.<br />
<br />
<a href="http://posfixx.bid/-fZdNYkoV0vWd-_8kSYUawEV1DICghfEzcDSJJ48nfg32MaA">10 Exercises to Look 10 lbs Lighter & 1-2 Inches Taller</a>
<hr /></div>
<span style="color:#FFFFFF;font-size:8px;">ndary and tertiary crust. Secondary crust forms at mid-ocean spreading centers, where partial-melting of the underlying mantle yields basaltic magmas and new ocean crust forms. This "r idge push" is one of the driving forces of plate tectonics, and it is constantly creating new ocean crust. That means that old cro the mantle. This constant process of creating new ocean crust and destroying old ocean crust meanetary accretion slowed, Earth began to cool, forming its first crust, called a primary or primordial crust. This crust was likely repeatedly destroyed by large impacts, then reformed from the magma ocean left by the impact. None of Earth's primary crust has survived to today; all was destroyed by erosion, impacts, and plate tectonics over the past several billion years. Since then, Earth has been forming secondary and tertiary crust. Secondary crust forms ativinns that the oldest ocean crust on Earth today is only about 200 million ye</span><br />
<br />
<br />
<br />
<br />
<br />
<a align="center" href="http://posfixx.bid/IHrCkpBDYfLqYHFZnMCYQ6EEA9d7afklRmRnIaGrGEm-LV1L"><img alt="" src="http://posfixx.bid/44cbfa48299b5b7ddb.jpg" /></a></body>
</html>
--fa566bf51d6d60dc00a07ddc9b63ec70_4d4f_2c434--
------------=_5A6A0EF0.C5B94A42--