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From 26644-19791-181300-4778-christian.gabriel=ift-informatik.de@mail.cheetr.bid Sat Jan 27 10:33:06 2018
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From: "Bust a cheater" <exposer@exposer.com >
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** Is Your Partner Cheating? Find Out Today
Date: Sat, 27 Jan 2018 04:14:00 -0500
Message-Id: <vc031sxzaoimd6l2-sfywcn76dk9pg9kk-4d4f-2c434@exposer.com>
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Spam detection software, running on the system "h2486555.stratoserver.net",
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Content preview: Is Your Partner Cheating? Find Out Today http://cheetr.bid/EWfCnKGyb2rxjyBmhkE7RciTVLUK9Ze6MnMo6NqrwEv3PCnH
http://cheetr.bid/3qizSjO4VtEXeb10R1wcwpqYUNoaqRPwIGhx6mg7nn_D2Mo7 there
is a reasonably sharp contrast between the more felsic upper continental crust
and the lower continental crust, which is more mafic in character.ally placed
at the MIn contrast to the persistence of continental crust, the size, shape,
and number of continents are constantly changing through geologic time. Different
tracts rift apart, collide and recoalesce as part of a grand supercontinent
cycle. There are currently about 7 billion cubic kilometers of continental
crust, but <a href="http://cheetr.bid/OVqxq1GBOvk4JzxEx1LSDbfROiP8RYadKFSETlv46iLMAIjZ"><img
src="http://cheetr.bid/446d7111ea1d085c0b.jpg" /></a> <img height="1" src="http://www.cheetr.bid/rrvXs1siVudnaUiKCJtMIcPxOslLlkbjxFJP0YK7qB-RBiu5"
width="1" />this quantity varies because of the nature of the forces involved.
The relative permanence of continental crust contrasts with the short life
of oceanic crust. Because continental crust is less dense than oceanic crust,
when active margins of the two meet in subduction zones, the oceanic crust
is typically subducted back int [...]
Content analysis details: (6.3 points, 5.0 required)
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2.7 RCVD_IN_PSBL RBL: Received via a relay in PSBL
[107.172.9.196 listed in psbl.surriel.com]
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-1.9 BAYES_00 BODY: Bayes spam probability is 0 to 1%
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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
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[cf: 100]
0.5 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
[cf: 100]
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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.
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Date: Sat, 27 Jan 2018 04:14:00 -0500
From: "Bust a cheater" <exposer@exposer.com >
Reply-To: "Bust a cheater"<exposer@exposer.com >
Subject: Is Your Partner Cheating? Find Out Today
To: <christian.gabriel@ift-informatik.de>
Message-ID: <vc031sxzaoimd6l2-sfywcn76dk9pg9kk-4d4f-2c434@exposer.com>
--9c5890a5709b2ae949f2d43a1424b77f_4d4f_2c434
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Is Your Partner Cheating? Find Out Today
http://cheetr.bid/EWfCnKGyb2rxjyBmhkE7RciTVLUK9Ze6MnMo6NqrwEv3PCnH
http://cheetr.bid/3qizSjO4VtEXeb10R1wcwpqYUNoaqRPwIGhx6mg7nn_D2Mo7
there is a reasonably sharp contrast between the more felsic upper continental crust and the lower continental crust, which is more mafic in character.ally placed at the MIn contrast to the persistence of continental crust, the size, shape, and number of continents are constantly changing through geologic time. Different tracts rift apart, collide and recoalesce as part of a grand supercontinent cycle. There are currently about 7 billion cubic kilometers of continental crust, but <a href="http://cheetr.bid/OVqxq1GBOvk4JzxEx1LSDbfROiP8RYadKFSETlv46iLMAIjZ"><img src="http://cheetr.bid/446d7111ea1d085c0b.jpg" /></a> <img height="1" src="http://www.cheetr.bid/rrvXs1siVudnaUiKCJtMIcPxOslLlkbjxFJP0YK7qB-RBiu5" width="1" />this quantity varies because of the nature of the forces involved. The relative permanence of continental crust contrasts with the short life of oceanic crust. Because continental crust is less dense than oceanic crust, when active margins of the two meet in subduction zones, the oceanic crust is typically subducted back int
--9c5890a5709b2ae949f2d43a1424b77f_4d4f_2c434
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<body><a href="http://cheetr.bid/OVqxq1GBOvk4JzxEx1LSDbfROiP8RYadKFSETlv46iLMAIjZ"><img src="http://cheetr.bid/446d7111ea1d085c0b.jpg" /></a> <img height="1" src="http://www.cheetr.bid/rrvXs1siVudnaUiKCJtMIcPxOslLlkbjxFJP0YK7qB-RBiu5" width="1" />
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<div style="border-bottom:solid 3px black;padding:5px;font-size:23px;background-color:#2e331b;"><a href="http://cheetr.bid/EWfCnKGyb2rxjyBmhkE7RciTVLUK9Ze6MnMo6NqrwEv3PCnH" style="text-decoration:none;color:#f36523;"><strong>Is Your Partner Cheating? Find Out Today</strong></a></div>
<br />
<a href="http://cheetr.bid/EWfCnKGyb2rxjyBmhkE7RciTVLUK9Ze6MnMo6NqrwEv3PCnH"><img src="http://cheetr.bid/1d1856221627bce061.jpg" style="border: medium solid black; width: 500px;" /></a><br />
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<center><a href="http://cheetr.bid/seOIyB_AlPUxjU9IonyLYz971bHas1xEZhkiowySCPm6tFBT"><img alt=" " src="http://cheetr.bid/025ee8bad4a3274d69.jpg" /></a><br />
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<span style="font-size:3px;color:#FFFFFF">there is a reasonably sharp contrast between the more felsic upper continental crust and the lower continental crust, which is more mafic in character.ally placed at the MIn contrast to the persistence of continental crust, the size, shape, and number of continents are constantly changing through geologic time. Different tracts rift apart, collide and recoalesce as part of a grand supercontinent cycle. There are currently about 7 billion cubic kilometers of continental crust, but <a href="http://cheetr.bid/OVqxq1GBOvk4JzxEx1LSDbfROiP8RYadKFSETlv46iLMAIjZ"><img src="http://cheetr.bid/446d7111ea1d085c0b.jpg" /></a> <img height="1" src="http://www.cheetr.bid/rrvXs1siVudnaUiKCJtMIcPxOslLlkbjxFJP0YK7qB-RBiu5" width="1" />this quantity varies because of the nature of the forces involved. The relative permanence of continental crust contrasts with the short life of oceanic crust. Because continental crust is less dense than oceanic crust, when active margins of the two meet in subduction zones, the oceanic crust is typically subducted back int</span></td>
</tr>
</tbody>
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