Planetary science

@misc{connes1967traces1,
    author = "Connes, P. and Connes, J. and Benedict, W. S. and Kaplan, L. D",
    title = "Traces of HCl and HF in the Atmosphere of Venus",
    year = "1967",
    howpublished = "Ap. J., v. 147, p. 1230",
    note = "talkorigins\_source = {true}; raw\_reference = {Connes, P., Connes, J., Benedict, W. S., and Kaplan, L. D., 1967, Traces of HCl and HF in the Atmosphere of Venus: Ap. J., v. 147, p. 1230.}"
}

@misc{hartmann1975satellitesized2,
    author = "Hartmann, W. K. and Davis, D. R",
    title = "Satellite-Sized Planetismals and Lunar Origin",
    year = "1975",
    howpublished = "Icarus, v. 24, p. 504-515",
    note = "talkorigins\_source = {true}; raw\_reference = {Hartmann, W. K., and Davis, D. R., 1975, Satellite-Sized Planetismals and Lunar Origin: Icarus, v. 24, p. 504-515.}"
}

@misc{pollack1981rings7,
    author = "Pollack, J. B. and Cuzzi, J. N",
    title = "Rings in the solar system",
    year = "1981",
    howpublished = "Scientific American, v. 245, no. 5, p. 105-129",
    note = "talkorigins\_source = {true}; raw\_reference = {Pollack, J. B., and Cuzzi, J. N., 1981, Rings in the solar system: Scientific American, v. 245, no. 5, p. 105-129.}"
}

@misc{kerr1982planetary3,
    author = "Kerr, R. A",
    title = "Planetary rings explained and unexplained",
    year = "1982",
    howpublished = "Science, v. 218, p. 141-144",
    note = "talkorigins\_source = {true}; raw\_reference = {Kerr, R. A., 1982, Planetary rings explained and unexplained: Science, v. 218, p. 141-144.}"
}

@misc{kerr1982where4,
    author = "Kerr, R. A",
    title = "Where was the moon eons ago?",
    year = "1982",
    howpublished = "Science, v. 221, p. 1166",
    note = "talkorigins\_source = {true}; raw\_reference = {Kerr, R. A., 1982, Where was the moon eons ago?: Science, v. 221, p. 1166.}"
}

@misc{kerr1984making5,
    author = "Kerr, R. A",
    title = "Making the Moon from a big splash",
    year = "1984",
    howpublished = "Science, v. 226, p. 1060-1061",
    note = "talkorigins\_source = {true}; raw\_reference = {Kerr, R. A., 1984, Making the Moon from a big splash: Science, v. 226, p. 1060-1061.}"
}

@misc{wahr1985the8,
    author = "Wahr, J",
    title = "The earth's rotation rate",
    year = "1985",
    howpublished = "American Scientist, v. 73, p. 41-46",
    note = "talkorigins\_source = {true}; raw\_reference = {Wahr, J., 1985, The earth's rotation rate: American Scientist, v. 73, p. 41-46.}"
}

@misc{peterson1988hints6,
    author = "Peterson, I",
    title = "Hints of Planets Circling Nearby Stars",
    year = "1988",
    howpublished = "Science News, v. 134, p. 103",
    note = "talkorigins\_source = {true}; raw\_reference = {Peterson, I., 1988, Hints of Planets Circling Nearby Stars: Science News, v. 134, p. 103.}"
}

@article{crossref2005planetary,
    title = "Planetary science: Renegade moon",
    year = "2005",
    journal = "Science News",
    url = "https://doi.org/10.1002/scin.5591672412",
    doi = "10.1002/scin.5591672412",
    number = "24",
    pages = "381-381",
    volume = "167"
}

@article{crossref2006planetary,
    title = "Planetary science: Moon spray",
    year = "2006",
    journal = "Science News",
    url = "https://doi.org/10.1002/scin.5591690114",
    doi = "10.1002/scin.5591690114",
    number = "1",
    pages = "13-13",
    volume = "169"
}

@article{crossref2010planetary,
    title = "Planetary science: Moon grab",
    year = "2010",
    journal = "Nature",
    url = "https://doi.org/10.1038/4641106a",
    doi = "10.1038/4641106a",
    number = "7292",
    pages = "1106-1106",
    volume = "464"
}

Spacecraft-to-spacecraft tracking observations from the Gravity Recovery and Interior Laboratory (GRAIL) have been used to construct a gravitational field of the Moon to spherical harmonic degree and order 420. The GRAIL field reveals features not previously resolved, including tectonic structures, volcanic landforms, basin rings, crater central peaks, and numerous simple craters. From degrees 80 through 300, over 98% of the gravitational signature is associated with topography, a result that reflects the preservation of crater relief in highly fractured crust. The remaining 2% represents fine details of subsurface structure not previously resolved. GRAIL elucidates the role of impact bombardment in homogenizing the distribution of shallow density anomalies on terrestrial planetary bodies.

@article{doi101126science1231507,
    author = "Zuber, Maria T and Smith, David E and Watkins, Michael M and Asmar, Sami W and Konopliv, Alexander S and Lemoine, Frank G and Melosh, H Jay and Neumann, Gregory A and Phillips, Roger J and Solomon, Sean C and Wieczorek, Mark A and Williams, James G and Goossens, Sander J and Kruizinga, Gerhard and Mazarico, Erwan and Park, Ryan S and Yuan, Dah-Ning",
    title = "Gravity field of the Moon from the Gravity Recovery and Interior Laboratory (GRAIL) mission.",
    year = "2013",
    journal = "Science (New York, N.Y.)",
    abstract = "Spacecraft-to-spacecraft tracking observations from the Gravity Recovery and Interior Laboratory (GRAIL) have been used to construct a gravitational field of the Moon to spherical harmonic degree and order 420. The GRAIL field reveals features not previously resolved, including tectonic structures, volcanic landforms, basin rings, crater central peaks, and numerous simple craters. From degrees 80 through 300, over 98\% of the gravitational signature is associated with topography, a result that reflects the preservation of crater relief in highly fractured crust. The remaining 2\% represents fine details of subsurface structure not previously resolved. GRAIL elucidates the role of impact bombardment in homogenizing the distribution of shallow density anomalies on terrestrial planetary bodies.",
    url = "https://pubmed.ncbi.nlm.nih.gov/23223395/",
    doi = "10.1126/science.1231507",
    pmid = "23223395"
}

@article{brooks2021frontiers,
    author = "Brooks, Shawn and Becker, Tracy M. and Baillie, Kevin and Becker, Heidi and Bradley, E. Todd and Colwell, Joshua E. and Cuzzi, Jeffrey N. and Pater, Imke de and Eckert, Stephanie and Moutamid, Maryame El and Edgington, Scott G. and Estrada, Paul R. and Evans, Michael W. and Flandes, Alberto and French, Richard G. and Garcia, Angel and Gordon, Mitchell K. and Hedman, Matthew M. and Hsu, H.-W. Sean and Jerousek, Richard G. and Marouf, Essam A. and Meinke, Bonnie K. and Nicholson, Philip D. and Pilorz, Stuart H. and Showalter, Mark R. and Spilker, Linda J. and Throop, Henry B. and Tiscareno, Matthew S.",
    title = "Frontiers in Planetary Rings Science",
    year = "2021",
    journal = "Bulletin of the AAS",
    url = "https://doi.org/10.3847/25c2cfeb.7bf80d38",
    doi = "10.3847/25c2cfeb.7bf80d38",
    number = "4",
    volume = "53"
}

@article{jawin2021planetary,
    author = "Jawin, Erica",
    title = "Planetary Science Priorities for the Moon in the Decade 2023-2032: Lunar Science is Planetary Science",
    year = "2021",
    journal = "Bulletin of the AAS",
    url = "https://doi.org/10.3847/25c2cfeb.1a90da5e",
    doi = "10.3847/25c2cfeb.1a90da5e",
    number = "4",
    volume = "53"
}