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Could Zaklodzie be from Mercury?

http://www.space.com/17727-mercury-surface-rare-meteorites.html



Mercury's Surface Resembles Rare Meteorites

by Charles Q. Choi, SPACE.com Contributor
Date: 24 September 2012 Time: 07:26 AM ET

 Mercury has a surface unlike any other planet's in the solar system, instead 
resembling a rare type of meteorite, researchers say.

The finding, based on an analysis of data from NASA's Messenger probe, sheds 
new light on the formation and history of the mysterious innermost planet, 
scientists add.

Mercury, the smallest planet in the solar system, is also one of the least 
understood, having received much less attention from scientific missions than 
Mars, Jupiter and Saturn. NASA set out to change that when it launched the 
Messenger probe a little more than eight years ago. Messenger became the first 
spacecraft to orbit Mercury.

Past research based on Messenger data suggested a vast part of Mercury is 
covered with hardened lava, enough to bury the state of Texas under 4 miles 
(6.4 kilometers) of once-molten rock, scientists said. All in all, these 
mammoth floods of lava cover 6 percent of the planet's surface, an area equal 
to nearly 60 percent of the continental United States. They created Mercury's 
smooth northern plains between 3.5 billion to 4 billion years ago. [Latest 
Photos of Mercury by Messenger Probe]
This view from NASA's Messenger spacecraft orbiting Mercury shows a region of 
smooth, volcanic plains that have been heavily modified by tectonic structures 
termed "wrinkle ridges," low, sinuous features that form when lavas cool and 
subside, causing the
This view from NASA's Messenger spacecraft orbiting Mercury shows a region of 
smooth, volcanic plains that have been heavily modified by tectonic structures 
termed "wrinkle ridges," low, sinuous features that form when lavas cool and 
subside, causing the crust to contract horizontally. Image released Feb. 10, 
2012.
CREDIT: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie 
Institution of Washington

Lava plains are common in the solar system. For instance, young Mars spewed 
lava all across its surface, and it still has the largest volcano in the solar 
system: Olympus Mons is about 370 miles (600 km) in diameter, wide enough to 
cover the entire state of New Mexico, and 16 miles (25 km) high, three times 
taller than Mount Everest.

Now, 205 measurements of Mercury's surface composition, made by the X-ray 
spectrometer onboard Messenger, reveal how much Mercury's surface differs from 
those of other planets in the solar system.

"Being the closest planet to the sun does mean its formation history would be 
different and more extreme than the other terrestrial planets, with hotter 
temperatures and exposure to a stronger gravitational field," says lead study 
author Shoshana Weider, a planetary geologist at the Carnegie Institution of 
Washington.

The surface is dominated by minerals high in magnesium and enriched in sulfur, 
making it similar to partially melted versions of an enstatite chondrite, a 
rare type of meteorite that formed at high temperatures in low-oxygen 
conditions in the inner solar system.

"The similarity between the constituents of these meteorites and Mercury's 
surface leads us to believe that either Mercury formed via the accretion of 
materials somewhat like the enstatite chondrites, or that both enstatite 
chondrites and the Mercury precursors were built from common ancestors," Weider 
said.



The researchers also looked at the areas around the northern volcanic plains. 
These surrounding locales are more pockmarked by craters, suggesting they are 
older, with more time spent getting scarred by meteor impacts.

The older terrain possesses higher ratios of magnesium to silicon, sulfur to 
silicon and calcium to silicon than the northern plains do, but it also has 
lower ratios of aluminum to silicon. These differences suggest the smooth 
plains came from magma sources that were chemically different from the source 
of the material seen in the older regions.

"The chemical differences between the northern plains and the surrounding 
areas, combined with the fact that the northern plains are younger by about 500 
million years, tells us that the volcanic activity which produced the northern 
plains involved melting of different sections of Mercury's mantle, at cooler 
temperatures and at a later stage in the planet's history than the activity 
that would have produced the older surrounding terrains," Weider said.

The scientists will detail their findings in an upcoming issue of the Journal 
of Geophysical Research-Planets.
                                          
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