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Capture of Phobos and Deimos, Paper AAAS - 57725 by Geoffrey Landis
nprev
post May 24 2009, 01:19 AM
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What's interesting about Mars wrt tidal dynamics is that it has one pronounced bump: the Tharsis Bulge. It's apparently a fairly recent feature (<1 By), but it would be useful to understand its effect on the planet's Milankovitch cycles as well as on the orbital evolution of Phobos & Deimos.


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vk3ukf
post May 24 2009, 11:13 AM
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Could the grooves on Phobos be fracture marks from actually being shattered by the Stickney impact but only gently moving apart a little only to meld back together?
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Hungry4info
post May 24 2009, 04:37 PM
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Full inline quote removed

I'm no expert, but I would say it is possible.

Some of the newer images of Phobos show that the lines appear to be composed of several small craters. Or at least that my interpretation of it.


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Shaka
post May 24 2009, 10:29 PM
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craters or sinkholes?


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JohnVV
post Sep 8 2009, 09:46 PM
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QUOTE
Some of the newer images of Phobos show that the lines appear to be composed of several small craters


they don't look like strings of craters to me .More like stress fractures
an isis remapped image of ( PSP_007769_9015_BG13.cub ) to the shape model i am working on

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Floyd
post Sep 8 2009, 10:42 PM
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Welcome JohnVV! Really impressive first post. It is interesting that the groves in the top half of your projection run horizontally (east-west??) and those in the lower half run perpendicular/vertically. Almost seems like the bottom half of Phobos got rotated 90 degrees.


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JohnVV
post Oct 1 2009, 05:10 AM
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QUOTE
and those in the lower half run perpendicular/vertically. Almost seems like the bottom half of Phobos got rotated 90 degrees.


that is just from the shape model in ISIS3 that i made " ShapeModel = $base/dems/PhobosShapeNew.cub "
using the default lat/long from spiceinit

here it is without the "ShapeModel = Null ", and lat/long corrected with "qtie"

not mapped


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sgendreau
post Oct 25 2009, 08:52 PM
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QUOTE (john_s @ Mar 29 2009, 11:30 AM) *
A harder question for the capture hypothesis, I think, is why the inclination of the orbits is so low (1.1 and 1.8 degrees for Phobos and Deimos respectively).

John.


Could the large changes in obliquity be a factor? I've read that Earth's obliquity varies little because the Moon acts as an anchor -- so does the reverse hold as well?
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remcook
post Dec 11 2009, 11:52 AM
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never mind
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