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10.1098/rsta.2013.0168 http://scihub22266oqcxt.onion/10.1098/rsta.2013.0168 C4128260!4128260!25114301     free     free     free       Philos+Trans+A+Math+Phys+Eng+Sci 2014 ; 372 (2024): ä Nephropedia Template TP {{tp|p=25114301|t=2014. New approaches to the Moon s isotopic crisis |pdf=|usr=}}{{25114301}} gab.com Text New approaches to the Moon s isotopic crisis JO: Philos Trans A Math Phys Eng Sci http://www.kidney.de/pget.php?&tw=1&pmid=25114301 #FOAvip Recent comparisons of the isotopic compositions of the Earth and the Moon show that, unlike nearly every other body known in the Solar System, our satellite's isotopic ratios are nearly identical to the Earth's for nearly every isotopic system. The Moon's chemical make-up, however, differs from the Earth's in its low volatile content and perhaps in the elevated abundance of oxidized iron. This surprising situation is not readily explained by current impact models of the Moon's origin and offers a major clue to the Moon's formation, if we only could understand it properly. Current ideas to explain this similarity range from assuming an impactor with the same isotopic composition as the Earth to postulating a pure ice impactor that completely vaporized upon impact. Several recent proposals follow from the suggestion that the Earth?Moon system may have lost a great deal of angular momentum during early resonant interactions. The isotopic constraint may be the most stringent test yet for theories of the Moon's origin. Twit Text FOAVip New approaches to the Moon s isotopic crisis ????Philos Trans A Math Phys Eng Sci http://www.kidney.de/pget.php?&tw=1&pmid=25114301 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=25114301 #FOAvip English Wikipedia <ref>{{Cite pmid|25114301}}</ref> New approaches to the Moon s isotopic crisis #MMPMID25114301 Melosh HJ Philos Trans A Math Phys Eng Sci 2014[Sep]; 372 (2024): ä PMID25114301show ga Recent comparisons of the isotopic compositions of the Earth and the Moon show that, unlike nearly every other body known in the Solar System, our satellite's isotopic ratios are nearly identical to the Earth's for nearly every isotopic system. The Moon's chemical make-up, however, differs from the Earth's in its low volatile content and perhaps in the elevated abundance of oxidized iron. This surprising situation is not readily explained by current impact models of the Moon's origin and offers a major clue to the Moon's formation, if we only could understand it properly. Current ideas to explain this similarity range from assuming an impactor with the same isotopic composition as the Earth to postulating a pure ice impactor that completely vaporized upon impact. Several recent proposals follow from the suggestion that the Earth?Moon system may have lost a great deal of angular momentum during early resonant interactions. The isotopic constraint may be the most stringent test yet for theories of the Moon's origin. äNew approaches to the Moon s isotopic crisis (epmc).pdf DeepDyve Pubget Overpricing