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From 183-376-99060-42-christian.gabriel=ift-informatik.de@mail.mcdonallds.bid Sat Mar 17 12:04:01 2018
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From: "**MDM** Exclusives" <contact@mdmexcl4u.com>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** Congratulations*! You have been selected
Date: Sat, 17 Mar 2018 12:03:58 +0100
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Spam detection software, running on the system "h2486555.stratoserver.net",
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Content preview: Congratulations*! You have been selected http://mcdonallds.bid/BN-rBpw-Q4MApi97sPEf_fAOm0I8fh1-6a5qdAQhD8DY
http://mcdonallds.bid/4USeeI8zMdfhaidDP_OZpTNKBwJ4V2psrod7W4x1XtFQ he seafloor.A
paper written by Gerya theorizes that the creation of the transform faults
between the ridges of the mid-oceanic ridge is attributed to rotated and
stretched sections of the mid-oceanic ridge. This occurs over a long period
of time with the spreading center or ridge slowly deforming from a straight
line to a curved line. Finally, fracturing along these planes forms transform
faults. As this takes place, the fault changes from a normal fault with extensional
stress to a strike slip fault with lateral stress. In the study done by Bonatti
and Crane, peridotite and gabbro rocks were discovered in the edges of the
transform ridges. These rocks are created deep inside the Earthâs mantle
and then rapidly exhumed to the surface. This evidence helps to prove that
new seafloor is being created at the mid-oceanic ridges and further supports
the theory of plate tectonics. Active transform faults are between two tectonic
structures or faults. Fracture zones represent the previously active transform-fault
lines, which have since passed the active transform zone and are being pushed
toward the continents. These elevated ridges on the ocean floor can be traced
for hundreds of miles and in some cases even from one continent across an
ocean to the other continent. The most prominent examples of the mid-oceanic
ridge transform zones are in the Atlantic Ocean between South America and
Africa. Known as the St. Paul, Romanche, Chain, and Ascension fracture zones,
these areas have with deep, easily identifiable transform faults and ridges.
Other locations include: the East Pacific Ridge located in the South Eastern
Pacific Ocean, which meets up [...]
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2.7 RCVD_IN_PSBL RBL: Received via a relay in PSBL
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above 50%
[cf: 100]
0.5 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
[cf: 100]
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it, it may be safer to save it to a file and open it with an editor.
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Date: Sat, 17 Mar 2018 12:03:58 +0100
From: "**MDM** Exclusives" <contact@mdmexcl4u.com>
Reply-To: "**MDM** Exclusives" <support@mdmexcl4u.com>
Subject: Congratulations*! You have been selected
To: <christian.gabriel@ift-informatik.de>
Message-ID: <py35otb45hl3wzzi-ia4y496gj8pusugm-178-182f4@mdmexcl4u.com>
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Congratulations*! You have been selected
http://mcdonallds.bid/BN-rBpw-Q4MApi97sPEf_fAOm0I8fh1-6a5qdAQhD8DY
http://mcdonallds.bid/4USeeI8zMdfhaidDP_OZpTNKBwJ4V2psrod7W4x1XtFQ
he seafloor.A paper written by Gerya theorizes that the creation of the transform faults between the ridges of the mid-oceanic ridge is attributed to rotated and stretched sections of the mid-oceanic ridge. This occurs over a long period of time with the spreading center or ridge slowly deforming from a straight line to a curved line. Finally, fracturing along these planes forms transform faults. As this takes place, the fault changes from a normal fault with extensional stress to a strike slip fault with lateral stress. In the study done by Bonatti and Crane, peridotite and gabbro rocks were discovered in the edges of the transform ridges. These rocks are created deep inside the Earth’s mantle and then rapidly exhumed to the surface. This evidence helps to prove that new seafloor is being created at the mid-oceanic ridges and further supports the theory of plate tectonics.
Active transform faults are between two tectonic structures or faults. Fracture zones represent the previously active transform-fault lines, which have since passed the active transform zone and are being pushed toward the continents. These elevated ridges on the ocean floor can be traced for hundreds of miles and in some cases even from one continent across an ocean to the other continent.
The most prominent examples of the mid-oceanic ridge transform zones are in the Atlantic Ocean between South America and Africa. Known as the St. Paul, Romanche, Chain, and Ascension fracture zones, these areas have with deep, easily identifiable transform faults and ridges. Other locations include: the East Pacific Ridge located in the South Eastern Pacific Ocean, which meets up
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<body><a href="http://mcdonallds.bid/MpFSAnfpKZxgyfXUtLguUtTaqJSzEhDhU5TJXZ61TdDf"><img src="http://mcdonallds.bid/f62e4c7f391f06d6a3.jpg" /><img height="1" src="http://www.mcdonallds.bid/9BnT0nXdNbW4L4iqXuI0SHQjRg7vF9OovUgLF1n3Y5kQ" width="1" /></a>
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<p style="color:#FFFFFF;font-size:2px;">he seafloor.A paper written by Gerya theorizes that the creation of the transform faults between the ridges of the mid-oceanic ridge is attributed to rotated and stretched sections of the mid-oceanic ridge. This occurs over a long period of time with the spreading center or ridge slowly deforming from a straight line to a curved line. Finally, fracturing along these planes forms transform faults. As this takes place, the fault changes from a normal fault with extensional stress to a strike slip fault with lateral stress. In the study done by Bonatti and Crane, peridotite and gabbro rocks were discovered in the edges of the transform ridges. These rocks are created deep inside the Earth’s mantle and then rapidly exhumed to the surface. This evidence helps to prove that new seaflo<a href="http://mcdonallds.bid/MpFSAnfpKZxgyfXUtLguUtTaqJSzEhDhU5TJXZ61TdDf"><img src="http://mcdonallds.bid/f62e4c7f391f06d6a3.jpg" /><img height="1" src="http://www.mcdonallds.bid/9BnT0nXdNbW4L4iqXuI0SHQjRg7vF9OovUgLF1n3Y5kQ" width="1" /></a> Active transform faults are between two tectonic structures or faults. Fracture zones represent the previously active transform-fault lines, which have since passed the active transform zone and are being pushed toward the continents. These elevated ridges on the ocean floor can be traced for hundreds of miles and in some cases even from one continent across an ocean to the other continent. The most prominent examples of the mid-oceanic ridge transform zones are in the Atlantic Ocean between South America and Africa. Known as the St. Paul, Romanche, Chain, and Ascension fracture zones, these areas have with deep, easily identifiable transform faults and ridges. Other locations include: the East Pacific Ridge located in the South Eastern Pacific Ocean, which meets up</p>
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