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Browsing LPI Contributions by Title

Browsing LPI Contributions by Title

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  • Silicate petrography, classification, and origin of the mesosiderites: Review and new observations 
    Floran, R. J. (Pergamon Press, 1978)
    The classification of mesosiderites proposed by Powell (1971) is modified and expanded to include impact melts. A petrographic study of all 20 mesosiderites reveals that most contain a complex assemblage of mineral, lithic, ...
  • Site M0077: Introduction 
    Gulick, Sean P. S.; Morgan, Joanna V.; Mellett, Claire L.; Green, S. L.; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282 (International Ocean Discovery Program, 2017-12-30)
    During International Ocean Discovery Program Expedition 364, open-hole drilling occurred from the seafloor to ~500 m drilling depth below seafloor (DSF) and core was recovered between 505.70 and 1334.69 meters below seafloor ...
  • Site M0077: Lower Peak Ring 
    Morgan, Joanna V.; Gulick, Sean P. S.; Mellett, Claire L.; Green, S. L.; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282 (International Ocean Discovery Program, 2017-12-30)
    From 747.02 meters below seafloor (mbsf) to the base of Hole M0077A at 1334.69 mbsf, granitoids intruded by pre-impact mafic and felsic dikes were recovered, interspersed with suevite and impact melt rock (Core 95R-3, 117 ...
  • Site M0077: microbiology 
    Morgan, Joanna V.; Gulick, Sean P. S.; Mellett, Claire L.; Green, S. L.; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282 (International Ocean Discovery Program, 2017-12-30)
    Asteroid and comet impacts are known to cause severe disruption to surface biota, as is the case for Chicxulub, but what is their effect on the present and ancient deep biosphere, where a large proportion of the Earth's ...
  • Site M0077: Open Hole 
    Gulick, Sean P. S.; Morgan, Joanna V.; Mellett, Claire L.; Green, S. L.; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282 (International Ocean Discovery Program, 2017-12-30)
    The upper part of Hole M0077A, the Open Hole interval, was drilled without coring to maximize the potential to reach the target drilling depth. A rotary drill was used for open-hole drilling from the seabed to 505.7 m ...
  • Site M0077: Post-Impact Sedimentary Rocks 
    Gulick, Sean P. S.; Morgan, Joanna V.; Mellett, Claire L.; Green, S. L.; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282 (International Ocean Discovery Program, 2017-12-30)
    In the uppermost part of the cored interval in Hole M0077A, a succession of post-impact sedimentary rocks was recovered between 505.7 and 617.33 meters below seafloor (mbsf) (Core 1R to Section 40R-1, 109.4 cm). The following ...
  • Site M0077: Upper Peak Ring 
    Morgan, Joanna V.; Gulick, Sean P. S.; Mellett, Claire L.; Green, S. L.; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282 (International Ocean Discovery Program, 2017-12-30)
    In Hole M0077A, the Upper Peak Ring interval is composed of suevite and impact melt rock between 617.33 and 747.02 meters below seafloor (mbsf) (Sections 40R-1, 109.4 cm, to 95R-3, 117 cm). The following sections detail ...
  • Sixth International Conference on Mars : July 20-25, 2003, Pasadena, California 
    Albee, Arden; Kieffer, Hugh (Lunar and Planetary Institute, 2003)
  • The Sixth International Conference on Mars Polar Science and Exploration : September 5-9, 2016, Reykjavik, Iceland 
    Smith, Isaac; Calvin, Wendy; https://orcid.org/0000-0002-6097-9586 (Lunar and Planetary Institute, 2016)
    The conference is designed to pull together the current state of Mars polar research from many fields, including geology, atmospheric, and climate sciences.
  • SkyTellers 
    Moroney, Lynn; Manning, James G. (Lunar and Planetary Institute, 2005)
    Each topic begins with a story and is followed by the scientific explanation. The story video is only a star field, to allow visualization by the children. The accompanying text includes an activity, discussion, and further ...
  • Slope Map between Shackleton and de Gerlache Craters, Lunar South Pole 
    Harish; Animireddi, Venkata Satya Kumar; Barrett, Natasha; https://orcid.org/0000-0002-4964-1138; Boazman, Sarah; Gawronska, Aleksandra; Gilmour, Cosette; https://orcid.org/0000-0002-4978-530X; Halim, Samuel; McCanaan, Kathryn; Shah, Jahnavi; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282; https://orcid.org/0000-0003-3150-6787 (Center for Lunar Science and Exploration, Lunar and Planetary Institute, 2019)
    This map is based on data collected by the Lunar Orbiter Laser Altimeter (LOLA) onboard the Lunar Reconnaissance Orbiter (LRO). The map shows slopes derived from the LOLA 5-m elevation product (NASA Goddard Space Flight ...
  • Slope Map between Shackleton and de Gerlache Craters, Lunar South Pole 
    Harish; Animireddi, Venkata Satya Kumar; Barrett, Natasha; https://orcid.org/0000-0002-4964-1138; Boazman, Sarah; Gawronska, Aleksandra; Gilmour, Cosette; https://orcid.org/0000-0002-4978-530X; Halim, Samuel; McCanaan, Kathryn; Shah, Jahnavi; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282; https://orcid.org/0000-0003-3150-6787 (Center for Lunar Science and Exploration, Lunar and Planetary Institute, 2020)
    This map is based on data collected by the Lunar Orbiter Laser Altimeter (LOLA) onboard the Lunar Reconnaissance Orbiter (LRO). The map shows slopes derived from the LOLA 10-m elevation product (NASA Goddard Space Flight ...
  • Slope Map between Shackleton and de Gerlache Craters, Lunar South Pole 
    Harish; Animireddi, Venkata Satya Kumar; Barrett, Natasha; https://orcid.org/0000-0002-4964-1138; Boazman, Sarah; Gawronska, Aleksandra; Gilmour, Cosette; https://orcid.org/0000-0002-4978-530X; Halim, Samuel; McCanaan, Kathryn; Shah, Jahnavi; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282; https://orcid.org/0000-0003-3150-6787 (Center for Lunar Science and Exploration, Lunar and Planetary Institute, 2019)
    This map is based on data collected by the Lunar Orbiter Laser Altimeter (LOLA) onboard the Lunar Reconnaissance Orbiter (LRO). The map shows slopes derived from the LOLA 5-m elevation product (NASA Goddard Space Flight ...
  • Slope Map of the Moon's South Pole (85°S to Pole) 
    Harish; Animireddi, Venkata Satya Kumar; Barrett, Natasha; https://orcid.org/0000-0002-4964-1138; Boazman, Sarah; Gawronska, Aleksandra; Gilmour, Cosette; https://orcid.org/0000-0002-4978-530X; Halim, Samuel; McCanaan, Kathryn; Shah, Jahnavi; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282; https://orcid.org/0000-0003-3150-6787 (Center for Lunar Science and Exploration, Lunar and Planetary Institute, 2019)
    This map is based on data collected by the Lunar Orbiter Laser Altimeter (LOLA) onboard the Lunar Reconnaissance Orbiter (LRO). The map shows slopes derived from the LOLA 10-m elevation product (NASA Goddard Space Flight ...
  • Slope Map of the Moon's South Pole (85°S to Pole) 
    Harish; Animireddi, Venkata Satya Kumar; Barrett, Natasha; https://orcid.org/0000-0002-4964-1138; Boazman, Sarah; Gawronska, Aleksandra; Gilmour, Cosette; https://orcid.org/0000-0002-4978-530X; Halim, Samuel; McCanaan, Kathryn; Shah, Jahnavi; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282; https://orcid.org/0000-0003-3150-6787 (Center for Lunar Science and Exploration, Lunar and Planetary Institute, 2019)
    This map is based on data collected by the Lunar Orbiter Laser Altimeter (LOLA) onboard the Lunar Reconnaissance Orbiter (LRO). The map shows slopes derived from the LOLA 10-m elevation product (NASA Goddard Space Flight ...
  • Slope Map of the Moon's South Pole (85°S to Pole) 
    Harish; Animireddi, Venkata Satya Kumar; Barrett, Natasha; https://orcid.org/0000-0002-4964-1138; Boazman, Sarah; Gawronska, Aleksandra; Gilmour, Cosette; https://orcid.org/0000-0002-4978-530X; Halim, Samuel; McCanaan, Kathryn; Shah, Jahnavi; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282; https://orcid.org/0000-0003-3150-6787 (Lunar and Planetary Institute, 2019)
    This map is based on data collected by the Lunar Orbiter Laser Altimeter (LOLA) onboard the Lunar Reconnaissance Orbiter (LRO). The map shows slopes derived from the LOLA 10-m elevation product (NASA Goddard Space Flight ...
  • Slope Map of the Moon's South Pole Ridge 
    McCanaan, Kathryn; Animireddi, Venkata Satya Kumar; Barrett, Natasha; https://orcid.org/0000-0002-4964-1138; Boazman, Sarah; Gawronska, Aleksandra; Gilmour, Cosette; https://orcid.org/0000-0002-4978-530X; Halim, Samuel; Harish; Shah, Jahnavi; Kring, David A. (David Allen); https://orcid.org/0000-0002-3440-6282; https://orcid.org/0000-0003-3150-6787 (Center for Lunar Science and Exploration, Lunar and Planetary Institute, 2019)
    Lunar Reconnaissance Orbiter Lunar Orbiter Laser Altimeter (LOLA) 5-m elevation product over derived hillshade with solar azimuth 45° and solar elevation 45°. High elevation: red and orange; Low elevation: purple and white.
  • Small Bodies Tell the Story of the Solar System: A Scientific Rationale for a Multi-Target Small Body Sample Return Program including the Earth-based Laboratory Analysis of Returned Samples 
    Jacobson, Seth; Bose, Maitrayee; Bodewits, Dennis; Fries, Marc D.; Jha, Devanshu; Mane, Prajkta; Nittler, Larry R., 1969-; Sandford, Scott; Thompson, Michelle (2020)
    A White Paper submitted to the Planetary Science and Astrobiology Decadal Survey 2023-2032
  • SNC meteorites: Igneous rocks from Mars? 
    Wood, Charles A.; Ashwal, Lewis D.; https://orcid.org/0000-0001-7277-9007 (Pergamon Press, 1981)
    All dated meteorites have formation ages of 4.4 to 4.6 b.y. (Sears, 1978), except for nine achondrites which crystallized 1.3 b.y. ago (Table 1). These meteorites-shergottites, nakhlites, and chassignites (SNC)-also differ ...
  • Solar System fact finder 
    Chapman, Clark R.; Matson, Dennis L.; Newburn, R. L. (Ray L.); Orton, Glenn; Scott, Edward R. D.; Zeller, Ben (Lunar and Planetary Institute, 1979-11)
    Tables show data on planetary atmospheres, planets, planetary satellites, asteroids, comets, and meteorites.

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