Universities Space Research Association

Lunar science and techSubcontractor to 4
Lunar obligations
$107M
as prime
Lunar awards
19
as prime
Its subcontractors
21
$5.2M reported
Primes it works for
4
$739K in subawards

Who it subcontracts to

  1. HOSTING, MAINTENANCE AND TECHNICAL SUPPORT OF THE NEXSS WEBSITE AND MEETING SUPPORT

  2. PSI WILL LEAD THE EFFORT ON DESIGN, DATA COLLECTION AND ANALYSIS OF PLANETARY SME NEEDS ASSESSMENT (2021)

  3. ANALYSES OF APOLLO AND LUNAR-RELATED MATERIALS TO DETERMINE THE AMOUNT OF VOLATILE ELEMENTS IN THEM AND THEIR SOURCE REGIONS, IN AN EFFORT TO CHARACTERIZE THE VOLATILE CYCLE OF THE MOON. THESE ACTIVITIES WILL BE INTEGRATED WITH THOSE OF OTHER TEAM INVESTIGATORS WHO ARE STUDYING ADDITIONAL PETROLOGICAL, GEOCHEMICAL, AND ISOTOPIC ATTRIBUTES OF THE SAMPLES AND/OR ARE INVESTIGATING RELATED LUNAR AND ASTEROID SCIENCE ISSUES AS PART OF THE CENTER FOR LUNAR SCIENCE AND EXPLORATION (CLSE) ACTIVITIES. WILL CONTRIBUTE TO THE INTELLECTUAL DISCUSSION OF THE TEAM AND WORK WITH THE TEAM TO EXPLORE THE SCIENCE PRIORITIES IDENTIFIED AND, WHEN WARRANTED AND APPROVED BY THE PI, FOLLOW NEW LEADS THAT THE WORK REVEALS. WILL PARTICIPATE IN TEAM MEETINGS, USING TELE-CONFERENCING TOOLS. WILL PROVIDE STUDENTS AN OPPORTUNITY TO INTERACT WITH OTHER SENIOR CLSE SCIENTISTS AND MEET PEERS ON THE TEAM.

  4. CSTL WILL WORK WITH THE PLANETARY REACH TEAM TO PLAN CONFERENCE PRESENTATIONS AND PUBLIC ENGAGEMENT INSTITUTES. CSTL WILL CO-FACILITATE AT LEAST ONE CONFERENCE PRESENTATION AND UP TO THREE WORKSHOPS AND PUBLIC ENGAGEMENT DAYS ACROSS THE COUNTRY PER YEAR. THE WORKSHOPS WILL ENABLE PARTICIPANTS TO UTILIZE THE MATERIALS, AND UNDERSTAND AUDIENCE NEEDS TO SUPPORT BETTER CONNECTIONS.

  5. WILL PROVIDE HIGHLY SIDEROPHILE ELEMENT ANALYSES AND OSMIUM AND MOLYBDENUM ISOTOPE ANALYSIS OF IMPACT LITHOLOGIES AND REGOLITH SAMPLES TO IDENTIFY IMPACT PROJECTILES. THEY WILL ALSO PROVIDE ANALYSES OF EXPERIMENTAL SAMPLES TO DETERMINE IF LUNAR SIDEROPHILE ELEMENTS IN MAGMATIC SOURCE REGIONS ARE THE RESULT OF INTERNAL PROCESSES OR THE DELIVERY OF A LATE VENEER OF THOSE ELEMENTS. THESE ACTIVITIES WILL BE INTEGRATED WITH THOSE OF OTHER TEAM INVESTIGATORS WHO ARE STUDYING ADDITIONAL PETROLOGICAL, GEOCHEMICAL, AND ISOTOPIC ATTRIBUTES OF THE SAMPLES AND/OR ARE INVESTIGATING RELATED LUNAR SCIENCE ISSUES AS PART OF THE CENTER FOR LUNAR SCIENCE AND EXPLORATION ACTIVITIES. UMD PARTICIPANTS WILL CONTRIBUTE TO THE INTELLECTUAL DISCUSSION OF THE TEAM AND WORK WITH THE TEAM TO EXPLORE THE SCIENCE PRIORITIES IDENTIFIED IN THE PROPOSAL AND, WHEN WARRANTED AND APPROVED, FOLLOW NEW LEADS THAT THE WORK REVEALS. BECAUSE THIS IS A TEAM EFFORT THAT HAS A STRONG INTEREST IN TRAINING YOUNG INVESTIGATORS, THE CO-I AND STUDENT(S) WILL PARTICIPATE IN TEAM MEETINGS USING TELE-CONFERENCING TOOLS PROVIDING THE STUDENT(S) AN OPPORTUNITY TO INTERACT WITH OTHER SENIOR CLSE SCIENTISTS AND MEET HIS/HER PEERS ON TEH TEAM.

  6. LEADS EVALUATION EFFORTS FOR PLANETARY REACH

  7. WORK WITH THE PLANETARY REACH TEAM TO PLAN CONFERENCE PRESENTATIONS AND PUBLIC ENGAGEMENT INSTITUTES. SUBRECIPIENT WILL CO-FACILITATE AT LEAST ONE SCIENCE CONFERENCE PRESENTATION/WORKSHOP (FOR INSTANCE, AT DPS OR AGU OR GSA) AND AT LEAST ONE PUBLIC ENGAGEMENT INSTITUTE ACROSS THE COUNTRY PER YEAR. EACH INSTITUTE PLUS THE TIME FOR CONDUCTING A PUBLIC EVENT AT THE END WILL INCLUDE 4 DAYS.

  8. PROVIDE PETROLOGIC, GEOCHEMICAL, ISOTOPIC ANALYSES OF LUNAR AND METEORITIC MATERIAL TO HELP EVALUATE THE COLLISIONAL EVOLUTION OF THE SOLAR SYSTEM.

  9. PROVIDE NOBLE GAS ANALYSES AND, IN PARTICULAR, AR-AR ISOTOPE ANALYSIS, TO DETERMINE THE CHRONOLOGY OF LUNAR AND METEORITIC IMPACT LITHOLOGIES.

  10. DR. NOVAK WILL " INPUT FOR MONTHLY QUAD-CHART REPORTS FOR NASA SCIENCE ACTIVATION " ANNUAL ACTIVITY REPORTS " PARTICIPATE IN TEAM MEETINGS AT LPI IN 2021, 2023, AND 2025 (ANTICIPATE 2.5 DAYS PLUS TRAVEL TIME) " PARTICIPATES IN ONLINE TEAM MEETINGS AS NEEDED

  11. PROVIDE PETROLOGIC AND GEOCHEMICAL ANALYSES OF APOLLO AND LUNAR-RELATED MATERIALS TO DETERMINE THE AMOUNT OF VOLATILE ELEMENTS IN THEM AND THEIR SOURCE REGIONS, IN AN EFFORT TO CHARACTERIZE THE VOLATILE-CYCLE OF THE MOON.

  12. WORK WITH LPI E/PO STAFF TO REVIEW E/PO AND INSTITUTE EFFORTS AND IDENTIFY THOSE THAT CAN BE FURTHER ENHANCED BY THE USE OF/MORE EFFECTIVE USE OF NEW MEDIA TOOLS AND APPROACHES (E.G., ENHANCING FOR TRAINED EDUCATORS, CAMPAIGNS TO BROADENING REACH OF PUBLIC OUTREACH EFFORTS). IDENTIFY SYNERGISTIC ACTIVITIES BETWEEN LPI'S AND NMC'S E/PO AND INSTITUTE EFFORTS. MAKE RECOMMENDATIONS TO THE LPI E/PO TEAM AND INSTITUTE PERSONNEL FOR THE STRATEGIC USE OF NEW MEDIA TOOLS AND APPROACHES IN LPI/S E/PO AND INSTITUTE PROGRAMS AND IN COLLABORATION WITH NMC. WORK WITH LPI AND ITS EVALUATOR TO SELECT THE MOST STRATEGIC INVESTMENTS, DESIGN RECOMMENDED ACTIVITIES, IDENTIFY IDEAL OUTCOMES, AND REVIEW EVALUATION TOOLS TO MEASURE IMPACT. WORK WITH LPI TO IMPLEMENT SYNERGISTIC ACTIVITIES AS FUNDING PERMITS. MEET WITH LPI E/PO AND INSTITUTE PERSONNEL QUARTERLY TO REVIEW ACTIVITY PROGRESS AND MAKE RECOMMENDATIONS FOR CHANGES BASED ON EVALUATION DATA.

  13. RESPONSIBLE FOR USING VIMS DATA TO INFER THE DISTRIBUTION OF ICE AGES OVER 30 CRATERS ON THE SURFACES OF TETHYS, DIONE, AND RHEA. USING SUCH DATA, THE CO-L WILL RESOLVE THE FORMATION AGE OF THESE YOUNG CRATERS. SETI WILL ADDITIONALLY AIDE IN THE INTERPRETATION OF THE MODELING RESULTS AND IN MANUSCRIPT PREPARATION. SETI WILL WORK WITH CO-LS TO DEVELOP A LIST OF CRATERS WITH THE BEST DATA TO STUDY BOTH ICE PHASE DISTRIBUTION AND CRATERING STATISTICS. THE CO-L WILL ALSO SUPERVISE 2 SUMMER UNDERGRADUATE STUDENTS PER PROPOSED YEAR

  14. REVISE STEM ENHANCEMENT IN EARTH SCIENCE (SEES) RESOURCES DEVELOPED UNDER SCIACT TO ADJUST FOR USE BY INFORMAL EDUCATORS AND PUBLIC, AND REDESIGN FOR SPECIFIC COMMUNITIES.

  15. 1) PROVIDE INPUT FOR ROSES EXOBIOLOGY AND EVOLUTIONARY BIOLOGY SOLICITATION ANNUALLY & ANY UPDATES AS NEEDED THROUGHOUT THE YEAR. 2) ORGANIZE & MANAGE REVIEW PANELS: SET DATES & LOCATIONS, OVERSEE RECRUITING ALL PANELISTS & NON-PANEL REVIEWERS, CONDUCT THE REVIEW, & REVIEW PANEL EVALUATIONS. 3) COMMUNICATE WITH PROPOSERS REGARDING THE PROGRESS OF THEIR REVIEW & SELECTION DECISIONS, & EVALUATE REQUESTS FOR RECONSIDERATION. 4) PREPARE & PRESENT TO THE SELECTING OFFICIAL THE SELECTION REQUIREMENTS PACKAGE AND THE SELECTION DECISION DOCUMENT. 5) INTERFACE WITH HGAO, NSSC, AND THE PROGRAM SUPPORT SPECIALIST, & RESOURCE ANALYSTS TO FACILITATE TIMELY RELEASE OF FUNDING. 6) COMMUNICATE WITH PRIOR AWARD RECIPIENTS REGARDING THE PROGRESS OF THEIR RESEARCH AND THE ACCEPTABILITY OF THEIR ANNUAL REPORTS. 7) INTERFACE WITH HGAO, NSSC, THE PROGRAM SUPPORT SPECIALIST, & RESOURCE ANALYSTS TO FACILITATE TIMELY RELEASE OF CONTINUATION FUNDS. 8) PROVIDE RECOMMENDATIONS FOR RELATED FUNDING ACTIONS ON ANY REQUESTS FOR PI TRANSFERS, AUGMENTATIONS, & EXTENSIONS OF EXISTING AWARDS. 9) SET REVIEW SCHEDULE TO ENABLE ANNOUNCEMENT OF SELECTION DECISIONS WITHIN 180 DAYS OF PROPOSAL RECEIPT. SELECTION DECISIONS WILL BE ANNOUNCED WITHIN 180 DAYS OF PROPOSAL RECEIPT OR WITHIN 4 WEEKS OF MANAGEMENT COMMITMENT TO PROGRAM BUDGETS, WHICHEVER IS LATER. 10) PROVIDE INPUT TO THE ANNUAL GPRA REPORT.

Who it works for

  1. STATEMENT OF WORK JULIE STOPAR, PH.D WILL SERVE AS INSTITUTIONAL PL AND A MEMBER OF THE CASA MOON SCIENCE TEAM, INCLUDING RESEARCH AND MISSION OPERATIONS AND SUPPORT ROLES AS NEEDED IN THE FOLLOWING AREAS: • ESTABLISHING LINKAGES BETWEEN EXISTING ORBITAL DATA, SAMPLES, FUTURE EXPLORATION SITES, AND UPCOMING DATA SETS • CONNECTING SAMPLE CHRONOLOGY, GEOCHEMISTRY, AND MINERALOGY TO ORBITAL REMOTE SENSING DATA FOR LUNAR PYROCLASTIC AND OTHER VOLCANIC DEPOSITS • INVESTIGATING THE COMPOSITIONAL DIVERSITY OF PYROCLASTIC MATERIALS AND UNDERSTANDING HOW THEY RELATE TO THE EVOLUTION OF VOLCANISM AND THE LUNAR INTERIOR • PARTICIPATE IN REGULAR MEETINGS/TELECONFERENCE CALLS, AS NEEDED • ATTEND THE KICKOFF MEETING • PREPARE AND PRESENT PAPERS AND PUBLICATIONS AS NEEDED • SUPPORT PUBLIC ENGAGEMENT ACTIVITIES FOR BROADENING IMPACT AND ACCESSIBILITY OF RESEARCH • ORGANIZE SCIENCE TEAM THEME GROUPS AND MEETINGS AS NEEDED DR. STOPAR WILL PROVIDE THE FOLLOWING DELIVERABLES: • PROVIDE ACTIVITY SUMMARIES MONTHLY/ANNUALLY • CONFERENCE PRESENTATIONS AND ABSTRACTS • RESEARCH PUBLICATIONS • CONTRIBUTIONS TO AND SUPPORT OF MISSION WEB AND MEDIA CONTENT • SUPPORT THE INCLUSION PLAN

  2. SCOPE OF WORK " CO-I STOPAR THE PRIMARY PROPOSED TASK IS TO PERFORM MODELING OF WATER-REGOLITH REACTIONS. THE MODELING WILL SUPPORT AND COMPLEMENT OTHER PROPOSED TASKS INCLUDING ALTERATION EXPERIMENTS ON LUNAR REGOLITH SIMULANTS AND CURATION CONSIDERATIONS. TO CONSTRAIN HOW LONG IT TAKES FOR SPECIFIC MINERAL REACTIONS IN THE PRESENCE OF LIQUID WATER OR GAS, RATE EQUATIONS WILL BE USED TO DETERMINE THE VOLUME OF MATERIAL THAT WOULD BE ALTERED AT DIFFERENT TIME-STEPS FOLLOWING THE ONSET OF HEATING. THUS, FOR EXAMPLE, THE TIME IT WOULD BE EXPECTED TO TAKE FOR 10% OF THE ANORTHITE TO ALTER IN A SOIL WITH 1 MM GRAINS, 30% ANORTHITE, AND 5% H2O BY MASS AT A DEPTH OF 35 CM (OR CONFINING PRESSURE OF 6 MBARS) WILL BE CONSTRAINED BY THE MODELS. FACTORS TO BE CONSIDERED: PRESENCE OF LIQUID WATER AT DIFFERENT TEMPERATURES, PRESSURES, VARIOUS REGOLITH AND SIMULANT MINERAL COMPONENTS (PYROXENE, PLAGIOCLASE, GLASS, OLIVINE, FE-METAL, AGGLUTINATES), REGOLITH MINERAL COMPONENTS OF VARYING DIMENSIONS, AND CURATION SETTING OR GEOLOGIC SETTING. PUBLICATIONS(S) WILL SUMMARIZE RESULTS OF THE MODELS AND THEIR RELEVANCE FOR OTHER CONSORTIUM RESEARCH.

  3. DEPUTY PI RAPETTI WILL CO-LEAD THEORETICAL AND OBSERVATIONAL RESEARCH ON RADIO PLANET MAGNETOSPHERES AND 21-CM COSMOLOGY USING BOTH EXISTING AND FUTURE OBSERVATIONS, INCLUDING GROUND AND SPACE-BASED INSTRUMENTS AS USEFUL, AND LEAD DATA ANALYSIS PIPELINE DEVELOPMENTS FOR RADIO EXOPLANETS AND 21-CM COSMOLOGY STUDIES TOWARDS OPTIMIZING THE DESIGN OF FUTURE EXPERIMENTS AND HIGH-QUALITY MEASUREMENTS. THE STATE-OF-THE-ART PIPELINE DEVELOPED FOR LOW RADIO FREQUENCY OBSERVATIONS CONTAINING THE GLOBALLY AVERAGED SPIN-FLIP 21-CM BACKGROUND WILL BE EXTENDED AND ADAPTED TO INCORPORATE SUCH AN AUGMENTED FRAMEWORK. TO EFFECTIVELY OPTIMIZE THE DESIGN OF LUNAR RADIO TELESCOPES, RAPETTI WILL ALSO SUPPORT POTENTIAL LUNARLAB EFFORTS TO LEVERAGE SYNERGIES WITH OTHER ASTROPHYSICAL PROBES, AS WELL AS PIPELINE AUGMENTATIONS FOR THEORETICAL MODELING AIMED AT PLANNING FOR FUTURE LUNAR RADIO TELESCOPES. KEY EXTENSIONS OF THE PIPELINE WILL AIM AT MAXIMIZING THE SCIENTIFIC YIELD OF LUNAR-BASED INTERFEROMETERS STUDIED BY LUNARLAB SUCH AS FARSIDE AND FARVIEW, WHICH WILL MEASURE FLUCTUATIONS IN THE SPIN-FLIP BACKGROUND, BOTH ACROSS THE SKY AND IN THE RADIAL DIRECTION. STATISTICAL MEASUREMENTS OF THE 21-CM LINE PLACE STRINGENT REQUIREMENTS ON THE SPECTRAL CHARACTERISTICS OF THE ANALOG AND DIGITAL HARDWARE. TO LEVERAGE THE PIPELINE TO JOINTLY STUDY MULTIPLE ASPECTS OF THE TRADE-OFFS BETWEEN INSTRUMENT DESIGN AND SCIENTIFIC POTENTIAL, DEPUTY PI RAPETTI WILL LEAD OTHER TEAM MEMBERS AND POTENTIAL COLLABORATORS IN AN EFFORT TOWARDS EXPANDING THE PIPELINE TO INCLUDE SPATIAL FLUCTUATIONS, AS MEASURED BY INTERFEROMETERS OVER A RANGE OF SCALES, AND USING IT TO TEST FOR THE EXTRACTION OF THE POWER SPECTRUM SIGNAL FROM SYSTEMATICS WITH LUNAR RADIO TELESCOPE DESIGNS TO MAXIMIZE SCIENCE RETURNS. DEPUTY PI RAPETTI WILL ALSO ASSIST PI BURNS IN THE CONSTRUCTION OF TEAM REPORTS AND IN CONTRIBUTING TO PRESENTATIONS ON LUNARLAB AT EC MEETINGS AT THE REDUCED LEVEL PERMITTED BY SSERVI BASED ON THE LIMITED TEAM SIZE.

  4. CO-I RIVERA-VALENTIN WILL WORK WITHIN THEME 2 (INVESTIGATIONS OF FINE-GRAINED MATERIALS ON THE LUNAR SURFACE) OF THE PROPOSED WORK TO PERFORM SIMULATIONS OF IMPACT-INDUCED MIXING TO UNDERSTAND THE ORIGIN OF MINERALS THAT ARE THOUGHT TO ARISE FROM DEPTH ON THE MOON.

Lunar awards as prime

AwardDescriptionPeriodObligated
NNX08AC28ASTEPHEN MACKWELL / UNIVERSITIES SPACE RESEARCH ASSOCIATIONOPERATION OF THE LUNAR AND PLANETARY INSTI2007-12-20 → ?$36M
NNX15AL12ATHE UNIVERSITIES SPACE RESEARCH ASSOCIATION PROPOSES TO OPERATE THE LUNAR AND PLANETARY INSTITUTE AT ITS HOUSTON FACILITY ADJACENT TO NASA JOHNSON SP2015-05-19 → 2021-07-21$27M
80NSSC20M0173SINCE ITS INCEPTION MORE THAN FIVE DECADES AGO THE LPI HAS PLAYED A UNIQUE ROLE IN THE LUNAR AND PLANETARY SCIENCE COMMUNITY PROVIDING A MEANS FOR COOPERATION AMONG NASA UNIVERSITIES AND OTHER RESEARCH ORGANIZATIONS TO ADVANCE NASA S OBJECTIVES IN PLANETARY SCIENCE. THE LPI S SUCCESS IS DUE TO THE BREADTH OF ITS ACTIVITIES THE ACTIVE SYNERGIES AMONG THEM AND CRUCIALLY THE INFUSION OF SCIENCE INTO EVERYTHING WE DO. THE LPI ALSO HAS A LONG HISTORY OF FRUITFUL COLLABORATION WITH THE ASTROMATERIALS DIVISION AT NASA S JOHNSON SPACE CENTER (JSC) FACILITATED BY THE CLOSE PROXIMITY OF OUR TWO ORGANIZATIONS.2020-09-09 → 2025-09-30$22M
NNA14AB07AFPDS BASE DESCRIPTION MULTIPLE YEAR AWARD&INCREMENTAL FUNDING FOR YEARS ONE TO FIVE. THIS PROPOSAL IS ENTITLED "INNER SOLAR SYSTEM IMPACT PROCESSES: AN INTEGRATED ANALYSIS USING EXTRATERRESTRIAL SAMPLES ASTRONOMICAL OBSERVATIONS AND MODELING." THIS IS AWARDED IN RESPONSE TO COOPERATIVE AGREEMENT NOTICE (CAN) NO. NNH13ZDA006C SOLAR SYSTEM EXPLORATION RESEARCH VIRTUAL INSTITUTE (SSERVI) CYCLE TWO. THE PRINCIPAL INVESTIGATOR IS DR. DAVID A. KRING WITH UNIVERSITIES SPACE RESEARCH ASSOCIATION (USRA). PROJECT SUMMARY: LUNAR SAMPLES AND METEORITIC SAMPLES OF NEAR-EARTH ASTEROIDS WILL BE ANALYZED TO BETTER ADDRESS THE COLLISIONAL EVOLUTION OF THE INNER SOLAR SYSTEM RANGING IN THE TIME FROM THE EARLIEST STAGES OF PLANETARY ACCRETION TO THE PROCESSES THAT CREATED THE SURFACES WE SEE TODAY. THESE DATA WILL PROVIDE THE FUEL TO CATALYZE AND CONSTRAIN MAJOR SOLAR SYSTEM HYPOTHESES LIKE THE INNER SOLAR SYSTEM IMPACT CATACLYSM&ITS IMPLICATIONS FOR THE ORBITAL EVOLUTION OF OUTER SOLAR SYSTEM PLANETS. SAMPLE ANALYSES WILL BE INTEGRATED WITH ASTRONOMICAL OBSERVATIONS OF NEAR-EARTH ASTEROIDS AND A GEOLOGIC ASSESSMENT OF THEIR SURFACES. MODELS OF ASTEROIDS&THE IMPACTS THEY PRODUCE WILL THEN BE USED TO DETERMINE THE HISTORICAL FLUX OF IMPACT EVENTS THEIR CONSEQUENCES &POTENTIAL FUTURE HAZARDS. LPI&JSC ARE LEADING A TEAM THAT WILL HELP GROW AN INTEGRATED SCIENCE&EXPLORATION COMMUNITY THROUGH COLLABORATIONS WITH RESEARCHERS AT SEVERAL INSTITUTIONS. THE RESEARCH PROVIDES THE FOUNDATION FOR A RICH TRAINING EDUCATIONAL&PUBLIC OUTREACH (E/PO) PROGRAM. THE TEAM WILL WORK WITH A CONSORTIUM OF NATIONALLY-DISTRIBUTED UNIVERSITIES AND COMMUNITY COLLEGES INCLUDING SEVERAL MINORITY-SERVING INSTITUTIONS TO INCREASE EXPOSURE OF UNDERGRADUATE&GRADUATE STUDENTS TO SPACE SCIENCE&EXPLORATION. WE WILL EXPAND OUR CURRENT SUITE OF LUNAR E/PO PROGRAMS TO INCLUDE ADDITIONAL LUNAR AND NEAR-EARTH ASTEROID SCIENCE EXPERIENCES FOR HIGH SCHOOL STUDENTS TRAVELING EXHIBITS FOR LIBRARIES AND MUSEUMS AN ON-LINE GALLERY OF SOLAR SYSTEM IMAGES AND A PUBLIC ENGAGEMENT WEBSITE. ALL OF THESE ACTIVITIES ARE DESIGNED WITH AN INTERFACE BETWEEN THE SCIENCE&EXPLORATION COMMUNITIES&WILL DEVELOP CONTENT THAT CAN BE USED TO DEVELOP FUTURE ROBOTIC&HUMAN MISSIONS.2014-03-04 → ?$5.3M
80NSSC22K0176THE UNIVERSITIES SPACE RESEARCH ASSOCIATION (USRA)-LUNAR AND PLANETARY INSTITUTE (LPI) PROPOSES TO PLAN AND IMPLEMENT ANNUAL MEETINGS AND PROVIDE TRAVEL AND SALARY SUPPORT FOR NASA S PROGRAM ANALYSIS (OR ASSESSMENT) GROUPS (PAGS). THE EIGHT PLANETARY2021-10-26 → 2027-04-25$3.9M
80NSSC17M0004THE UNIVERSITIES SPACE RESEARCH ASSOCIATION (USRA) ACTING BY AND THROUGH THE LUNAR AND PLANETARY INSTITUTE (REFERRED TO THROUGHOUT THE DOCUMENT AS THE INSTITUTE OR LPI) IS PROPOSING A SCIENCE COLLABORATION TO FACILITATE THE EFFORTS OF THE ASTROMATERIALS RESEARCH AND EXPLORATION SCIENCE (ARES) DIVISION BY PROVIDING SCIENTIFIC ANALYSIS AND EXPERTISE TO COMPLEMENT AND EXTEND THE EXISTING CAPABILITIES IN ARES. AS A TOP QUALITY WORLD RENOWNED SCIENCE INSTITUTE THE LPI IS UNIQUELY POSITIONED TO PROVIDE TECHNICAL PERSONNEL WITH STRONG RESEARCH CREDENTIALS THAT WOULD PROVIDE A FORUM FOR DEVELOPING RESEARCH IDEAS IN LUNAR AND PLANETARY SCIENCE. LPI S EXPERIENCE IN DEALING WITH NASA BADGING AND VISAS FOR FOREIGN NATIONALS BRINGS A UNIQUE RESOURCE TO THE ARES DIVISION. ADDITIONALLY THE LPI WILL PROVIDE USE OF THE FACILITIES AT THE INSTITUTE INCLUDING BUT NOT LIMITED TO MEETING FACILITIES OUTSIDE THE JSC FENCE TO FACILITATE CONVERSATIONS WITH COLLABORATORS; IT RESOURCES AND STAFF THAT PROVIDE COMPLEMENTARY RESOURCES TO THOSE AT JSC; A LUNAR AND PLANETARY SCIENCE LIBRARY COLLECTION THAT EXCEEDS 62 000 BOOKS JOURNALS AND ARCHIVED NASA DOCUMENTS; THE ENTIRE APOLLO IMAGE COLLECTION HOUSED AT THE INSTITUTE S REGIONAL PLANETARY IMAGE FACILITY (RPIF); AND ACCESS TO SCHOLARS AND STUDENTS TO ADDRESS KEY PLANETARY SCIENCE QUESTIONS.2017-08-01 → ?$3.8M
80NSSC20M0016ANALYSES OF LUNAR SAMPLES EXPERIMENTAL ANALOGUES AND METEORITIC REMNANTS OF COLLISIONAL RESERVOIRS WILL BE USED TO ASSESS THE ACCRETION AND SUBSEQUENT BOMBARDMENT OF THE EARTH-MOON SYSTEM WITH A SPECIFIC FOCUS ON THE DELIVERY AND PROCESSING OF VOLA2020-01-17 → 2026-10-14$3.3M
80NSSC21M0003PLANETARY EXPLORATION IS AMONG THE MOST EXCITING AND ACCESSIBLE OF THE SCIENCE ACTIVITIES FUNDED BY NASA OR ANY GOVERNMENT AGENCY. THE LUNAR AND PLANETARY INSTITUTE AND PARTNERS PROPOSE PLANETARY RESOURCES AND CONTENT HEROES (REACH) A PROCESS OR2021-01-01 → ?$2.8M
NNX17AG01GSATURN S RECENT CRATER FLUX AS CONSTRAINED BY CASSINI VIMS BACKGROUND: THE CRATERING FLUX FOR THE INNER SOLAR SYSTEM IS PARTIALLY CONSTRAINED BY GEOCHRONOLOGICAL MEASUREMENTS OF RETURNED LUNAR SAMPLES AND MARTIAN METEORITES COMBINED WITH CRATERING STUDIES; HOWEVER THE FLUX FOR THE OUTER SOLAR SYSTEM DOES NOT HAVE SUCH CONSTRAINTS. AT PRESENT THE PRIMARY METHOD OF UNDERSTANDING THE CRATERING HISTORY OF THE OUTER SOLAR SYSTEM IS VIA DYNAMICAL SIMULATIONS AND CRATERING STUDIES. THE ICY NATURE OF THE SATURNIAN MOONS THOUGH PROVIDES AN AS-OF-YET UNEXPLORED MEANS TO DATE YOUNG CRATERS. AN IMPACT ONTO AN ICY MOON WILL MELT A SHALLOW QUASI-SPHERICAL REGION. CRYSTALLINE ICE FORMS FROM THE FLASH HEATING OF SURFACE ICE AND SUBSEQUENT COOLING OF THE EXPOSED MELT. OVER TIME BOMBARDMENT BY IONS DISRUPTS THE CRYSTALLINE STRUCTURE PRODUCING AMORPHOUS ICE AT A KNOWN RATE ALLOWING FOR AN ESTIMATE OF FORMATION AGE. HERE WE PROPOSE TO USE VISIBLE AND INFRARED MAPPING SPECTROMETER (VIMS) DATA TO STUDY THE DISTRIBUTION OF ICE PHASES WITHIN AND SURROUNDING YOUNG CRATERS ON MIMAS TETHYS DIONE AND RHEA ALONG WITH CRATER COUNTS ON THESE CRATERS' FLOORS IN ORDER TO ESTIMATE THE RECENT CRATER FLUX EXPERIENCED BY THESE MOONS. SCIENCE GOALS AND OBJECTIVES: THE SCIENCE QUESTIONS WE PROPOSE ARE MOTIVATED BY RECENT SPACECRAFT DATA ANALYSIS AND ADVANCEMENTS IN SPECTROSCOPIC STUDIES OF ICE. WE SEEK TO ANSWER: 1) WHAT IS THE DISTRIBUTION OF ICE PHASES WITHIN AND SURROUNDING YOUNG CRATERS ON MIMAS TETHYS DIONE AND RHEA? 2) WHAT IS THE PREDICTED FORMATION AGE FOR THE STUDIED CRATERS USING THE KNOWN TRANSITION TIME BETWEEN CRYSTALLINE AND AMORPHOUS ICE? 3) WHAT IS THE DEGRADATION STATE OF THE OBSERVED CRATERS AND DOES THIS SUPPORT THE INFERRED AGE FROM OUR VIMS STUDY? 4) HOW HAS THE CRATER FLUX CHANGED OVER THE PAST FEW GA AND DOES IT VARY BETWEEN THE STUDIED MOONS? 5) HOW RECENTLY WERE THE GEOLOGICALLY YOUNG TERRAINS OF THE MID-SIZED MOONS OF SATURN FORMED? SUMMARY OF METHODOLOGY: WE WILL USE THE 2 M SPECTRAL BAND ASYMMETRY TO DETERMINE THE FRACTION OF CRYSTALLINE TO AMORPHOUS ICE ON THE SURFACE. THE MAIN ADVANTAGE OF APPLYING THE 2 M TECHNIQUE DEVELOPED BY CO-I DALLE ORE IS THAT IT IS INDEPENDENT OF THE SPECTRUM RESOLUTION AND IS STABLE EVEN IN THE CASE OF FAIRLY NOISY DATA. WE WILL USE TOPOGRAPHIC DATA OF THE MID-SIZED MOONS TO DETERMINE THE SLOPE OF THE CRATER WALLS FOR EACH STUDIED CRATER AND USE CASSINI IMAGING SCIENCE SUBSYSTEM (ISS) GEOLOGIC CONTEXT IMAGERY TO INFER STRATIGRAPHIC RELATIONSHIPS. THIS WILL ALLOW US TO ESTIMATE THE DEGRADATION STATE OF EACH CRATER WHICH WILL BE COMPARED WITH THE VIMS INFERRED CRATER AGE. ISS IMAGERY WILL ALSO BE USED TO CONDUCT CRATER STATISTICAL ANALYSIS OF THE FLOORS OF EVERY STUDIED CRATER IN ORDER TO QUANTIFY THE CRATER DENSITY ACCUMULATED AFTER FORMATION. VIA OUR FULLY THREE-DIMENSIONAL MONTE CARLO CRATERING MODEL WE WILL RELATE CRATER DENSITIES TO BOMBARDMENT MASSES. FINALLY GIVEN OUR DERIVED FORMATION AGES AND THE MEASURED CUMULATIVE BOMBARDMENT MASS EXPERIENCED WE WILL DEVELOP A CRATER FLUX FOR SATURN S MID-SIZED MOONS WHICH CAN INFORM DYNAMICAL MODELS OF THE OUTER SOLAR SYSTEM CRATERING HISTORY. RELEVANCE TO CDAP OBJECTIVES: THE PROPOSED WORK WOULD ENHANCE THE SCIENTIFIC RETURN OF THE CASSINI MISSION BY PRODUCING MAPS OF ICE PHASES WITHIN AND SURROUNDING CRATERS ON THE SATURNIAN MOONS USING CASSINI VIMS DATA. THE PROPOSED WORK WOULD MAKE USE OF PRODUCED HIGHER ORDER DATA PRODUCTS RESULTING FROM CASSINI ISS IN ORDER TO STUDY THE CRATERING HISTORY OF SATURN S MOONS. THE PROPOSED TASKS INCORPORATE BOTH DATA ANALYSIS AND NONDATA-ANALYSIS TASKS THAT ARE NECESSARY TO ANALYZE AND INTERPRET THE PROPOSED ANALYSIS. BY COMBINING SPECTROSCOPIC DATA THE OBSERVED CRATERING OF THE MID-SIZED MOONS ALONG WITH THEORY AND MODELING THE PROPOSED WORK WOULD HELP UNRAVEL THE RECENT CRATER FLUX OF THE SATURN SYSTEM AND SHED LIGHT ON THE DYNAMICAL HISTORY OF THE OUTER SOLAR SYSTEM.2017-02-07 → 2023-02-06$595K
80NSSC20K0762THE LUNAR AND PLANETARY INSTITUTE (LPI) PROPOSES TO PLAN IMPLEMENT AND SUPPORT A THREE-DAY WORKSHOP AND ASSOCIATED PUBLICATION ACTIVITIES FOR THE NASA HEADQUARTERS HELIOPHYSICS DIVISION (HPD).2020-03-11 → 2022-12-31$500K
80NSSC25K7020EXECUTE A BALANCED SCIENCE PROGRAM BASED ON DISCIPLINE-SPECIFIC GUIDANCE FROM THE NATIONAL ACADEMIES OF SCIENCES ENGINEERING AND MEDICINE ADMINISTRATION PRIORITIES AND DIRECTION FROM CONGRESS. PARTICIPATE AS A KEY PARTNER AND ENABLER IN THE AGENCY S EXPLORATION INITIATIVE FOCUSING ON SCIENTIFIC RESEARCH OF ON AND FROM THE MOON LUNAR ORBIT MARS AND BEYOND. ADVANCE DISCOVERY IN EMERGING FIELDS BY IDENTIFYING AND EXPLOITING CROSS-DISCIPLINARY OPPORTUNITIES BETWEEN TRADITIONAL SCIENCE DISCIPLINES DEVELOP A DIRECTORATE-WIDE TARGET-USER FOCUSED APPROACH TO APPLIED PROGRAMS INCLUDING EARTH SCIENCE APPLICATIONS SPACE WEATHER PLANETARY DEFENSE AND SPACE SITUATIONAL AWARENESS.2024-10-07 → 2027-10-06$375K
80NSSC25K7212EXECUTE A BALANCED SCIENCE PROGRAM BASED ON DISCIPLINE-SPECIFIC GUIDANCE FROM THE NATIONAL ACADEMIES OF SCIENCES ENGINEERING AND MEDICINE ADMINISTRATION PRIORITIES AND DIRECTION FROM CONGRESS. PARTICIPATE AS A KEY PARTNER AND ENABLER IN THE AGENCY S EXPLORATION INITIATIVE FOCUSING ON SCIENTIFIC RESEARCH OF ON AND FROM THE MOON LUNAR ORBIT MARS AND BEYOND. ADVANCE DISCOVERY IN EMERGING FIELDS BY IDENTIFYING AND EXPLOITING CROSS-DISCIPLINARY OPPORTUNITIES BETWEEN TRADITIONAL SCIENCE DISCIPLINES DEVELOP A DIRECTORATE-WIDE TARGET-USER FOCUSED APPROACH TO APPLIED PROGRAMS INCLUDING EARTH SCIENCE APPLICATIONS SPACE WEATHER PLANETARY DEFENSE AND SPACE SITUATIONAL AWARENESS.2024-10-18 → 2027-10-17$331K
80NSSC18K0711WE PROPOSE TO USE COINCIDENT OBSERVATIONS AS WELL AS BACK-FORWARD TRAJECTORIES TO VALIDATE SAGE-III/ISS SOLAR AND LUNAR OCCULTATION PROFILES OF AEROSOLS OZONE NITROGEN DIOXIDE AND WATER VAPOR AGAINST NON-COINCIDENT OBSERVATIONS OF THESE TRACE SPECIES FROM SATELLITE PLATFORMS SUCH AS MLS OSIRIS CALIPSO AND OMPS LP BALLOONSONDE NETWORKS (SHADOZ WOUDC AND NDACC OZONE AEROSOL AND WATER VAPOR) AND OTHER AVAILABLE AIR AND GROUND-BASED MEASUREMENT SYSTEMS. OUR APPROACH IS A VARIANT OF THE TECHNIQUE DESCRIBED IN SCHOEBERL ET AL. [2015] WHICH HAS BEEN USED TO VALIDATE ATTREX AND POSIDON DATA AGAINST MLS RETRIEVALS. A CHEMISTRY MODEL WHICH INCLUDES DIURNAL CHANGES IN PRODUCTION AND LOSS WILL BE USED TO RECONCILE OZONE NO2 AND WATER VAPOR MEASUREMENTS TAKEN BY SAGE III AT SUNRISE AND SUNSET AND DURING LUNAR OCCULTATIONS WE WILL THEN EXPLOIT THE ~1 KM RESOLUTION OF THE VALIDATED SAGE-III OBSERVATIONS TO CHARACTERIZE OF THE STRUCTURE AND SEASONAL VARIABILITY OF OZONE AEROSOLS AND WATER VAPOR IN THE UPPER TROPOSPHERE AND LOWER-TO-MIDDLE STRATOSPHERE.2018-06-01 → ?$289K
80NSSC19K0904IN THE LAST DECADE NEW MISSIONS TO THE MOON HAVE RETURNED A FLOOD OF NEW HIGH-RESOLUTION IMAGING SPECTROSCOPY TOPOGRAPHY AND GRAVITY DATA THAT HAVE TRIGGERED MAJOR ADVANCES IN OUR KNOWLEDGE OF THAT BODY'S ORIGIN STRUCTURE AND EVOLUTION. ONE MAJOR DEVELOPMENT IS THE IDENTIFICATION OF SEVERAL LARGE MARE PROVINCES (BASALT-COVERED PLAINS) THAT LACK A CLEAR ASSOCIATION WITH THE INTERIORS OF LARGE IMPACT BASINS. THESE INCLUDE THE BROAD BUT NARROW MARE FRIGORIS NORTH OF THE IMBRIUM AND SERENTIATIS BASINS AND MARE TRANQUILLITATIS WHICH OCCUPIES THE CENTER OF A TRIANGULAR REGION DELINEATED BY THE SERENTIATIS CRISIUM AND NECTARIS BASINS (HERE TERMED THE "SCN TRIANGLE"). FRIGORIS AND THE WESTERN MARGIN OF TRANQUILLITATIS COINCIDE WITH THE PROPOSED VOLCANO-TECTONIC BOUNDARY STRUCTURES OF THE PROCELLARUM REGION (ANDREWS-HANNA ET AL. 2014) BUT A SEARCH FOR GRAVITATIONAL SIGNALS OF BASINS (NEUMANN ET AL. 2015) REVEALED EVIDENCE FOR ONLY ONE SMALL BASIN IN WESTERN TRANQUILLITATIS AND NONE IN THE REMAINDER OF TRANQUILLITATIS OR FRIGORIS. THESE OBSERVATIONS CLEARLY SHOW THAT THE STANDARD PARADIGM FOR CREATING MARIA WITH BASALTIC MELT ASCENDING FROM AN ANOMALOUSLY WARM (AND PRESUMABLY IMPACT-HEATED) MANTLE REGION BENEATH AN IMPACT BASIN TO FILL THE BASIN IS INSUFFICIENT TO EXPLAIN THESE REGIONS. ..HERE WE PROPOSE TWO DISTINCT BUT INTERDEPENDENT TASKS AIMED AT 1) CHARACTERIZING THE GEOCHEMICAL PETROLOGIC AND GEOPHYSICAL RECORDS OF THESE REGIONS AS REVEALED BY REMOTELY SENSED DATA (AND INFORMED BY THE LUNAR SAMPLE COLLECTION) AND 2) CONSTRAINING THEIR VOLCANIC AND TECTONIC STRUCTURE VIA SOPHISTICATED NUMERICAL MODELING OF LITHOSPHERIC STRESS DEFORMATION AND GRAVITATIONAL SIGNATURE. ..TASK 1 WILL USE IMAGING AND SPECTROSCOPIC DATA FROM MISSIONS SUCH AS CLEMENTINE LUNAR PROSPECTOR KAGUYA CHANDRAYAAN-1 AND LUNAR RECONNAISSANCE ORBITER (LRO) TO CHARACTERIZE THE COMPOSITIONS AND ERUPTIVE HISTORIES OF VOLCANIC UNITS. FOR EXAMPLE FEO AND TIO2 ABUNDANCES DERIVED FROM CLEMENTINE AND KAGUYA VISIBLE AND NEAR-INFRARED DATA AND MINERALOGY DETERMINED FROM MOON MINERALOGY MAPPER DATA WILL BE USED TO CREATE MAPS OF COMPOSITIONAL/GEOLOGIC UNITS IN THE ENTIRE SCN TRIANGLE REGION. SUCH MAPS WILL PROVIDE INFORMATION NOT ONLY ON THE SURFACE UNITS BUT ALSO ON DEEPER ONES BY ANALYZING MATERIAL EXPOSED IN THE RIMS AND EJECTA OF SMALL IMMATURE CRATERS. THIS INFORMATION WILL CONSTRAIN POSSIBLE SCENARIOS FOR MAGMA GENERATION AND EMPLACEMENT IN TASK 2. TASK 2 WILL APPLY FINITE ELEMENT MODELS (USING THE COMSOL MULTIPHYSICS CODE) OF STRESS AND DEFORMATION OF THE LITHOSPHERE AND OF GRAVITATIONAL SIGNALS FROM TOPOGRAPHY AND INTERNAL DENSITY CONTRASTS TO EVALUATE SCENARIOS FOR LOAD EMPLACEMENT (E.G. EXTRUSIVE OR INTRUSIVE BASALTIC UNITS) THAT ARE CONSISTENT WITH GEOPHYSICAL OBSERVABLES (TOPOGRAPHY FROM LRO/LOLA AND GRAVITY FROM GRAIL) AND THE GEOLOGIC AND TECTONIC RECORDS. MODEL SCALES WILL VARY AS REQUIRED FROM SMALL-SCALE EDIFICES AND MAGMA BODIES (10S OF KM) TO REGIONAL-SCALE EMPLACEMENT OF MARE UNITS AND VOLCANIC EDIFICES (100S OF KM) TO PLANET-SCALE MODELS OF RIFTS (>1000 KM IN SPHERICAL GEOMETRY). ..THESE TASKS BUILD ON PREVIOUS WORK OF TEAM MEMBERS IN CHARACTERIZING FRIGORIS FROM THE SPECTROSCOPY/MAPPING PERSPECTIVE AND THE SCN TRIANGLE REGION FROM THE GEOPHYSICAL/LITHOSPHERIC PERSPECTIVE. THE PROPOSED WORK OFFERS INSIGHTS THAT MAY REACH BACK TO PRIMORDIAL EVENTS ON THE MOON (E.G. MAGMA OCEAN SOLIDIFICATION AND ESTABLISHMENT OF THE PROCELLARUM KREEP TERRANE) AND THE SUBSEQUENT HISTORY OF THE PROPOSED PROCELLARUM BOUNDARY RIFTS AND EMPLACEMENT OF BASALT UNITS IN THE TRIANGLE BASINS AND ENCOMPASSED REGION. ..THE PROPOSED WORK FULFILLS THE LDAP PROGRAM OBJECTIVE OF ENHANCING SCIENTIFIC RETURN FROM MISSIONS TO THE MOON BY EXPLOITING DATA FROM INSTRUMENTS OF MISSIONS SUCH AS CLEMENTINE KAGUYA CHANDRAYAAN-1 LRO AND GRAIL AND ADDRESSES NASA GOALS OF BETTER UNDERSTANDING THE VOLCANIC TECTONIC AND THERMAL HISTORY OF THE MOON. .2019-05-17 → 2025-04-30$285K
NNX17AC64GLUNAR PYROCLASTIC DEPOSITS: WINDOWS TO THE LUNAR INTERIORS THE GOAL OF THIS NEW, 3-YEAR RESEARCH PROGRAM IS TO ADVANCE OUR UNDERSTANDING OF THE NUMB2016-11-28 → 2023-11-27$156K
80NSSC17K0275MULTI-RING IMPACT BASINS ARE THE LARGEST IMPACTS AND FORM IN THE EARLIEST HISTORY OF THE TERRESTRIAL PLANETS. THE MOON HAS OVER 40 OF THESE LARGE IMPACT FEATURES IN VARYING STATES OF PRESERVATION. BECAUSE THESE LARGE IMPACTS EXCAVATE MANY KILOMETERS OF CRUST DURING FORMATION STUDY OF BASIN EJECTA ALLOWS US TO MAKE INFERENCES ABOUT THE CRUSTAL COMPOSITION AND STRUCTURE AT EACH BASIN SITE. IN THE PAST WORK ON THESE FEATURES HAS BEEN HAMPERED BY INCOMPLETE COVERAGE AND IMPRECISE POOR QUALITY DATA. THE NEW GLOBAL DATA FOR THE MOON OBTAINED BY LUNAR RECONNAISSANCE ORBITER (LRO) AND OTHER RECENT MISSIONS ALLOW US TO EXAMINE THE EJECTA DEPOSITS OF LUNAR BASINS IN HIGH RESOLUTION WITH A VARIETY OF SENSING TECHNIQUES INCLUDING DETERMINATION OF THEIR CHEMICAL MINERALOGICAL AND PHYSICAL PROPERTIES. I PROPOSE TO STUDY THE MORPHOLOGY AND COMPOSITION OF BASIN EJECTA DEPOSITS ON THE MOON USING THESE NEW DATA SETS. NEW IMAGE AND TOPOGRAPHIC DATA FROM LRO PERMITS GEOLOGICAL MAPPING OF THE DISTRIBUTION OF BASIN EJECTA AND THEIR STRATIGRAPHIC RELATIONS TO OTHER UNITS. BUILDING ON MY PREVIOUS STUDIES OF LUNAR BASINS I WILL RE-MAP THE GEOLOGICAL UNITS OF SEVERAL BASINS INCLUDING THE IMBRIUM HUMORUM MOSCOVIENSE AND HUMBOLDTIANUM BASINS USING LRO IMAGES AND TOPOGRAPHIC DATA TO ELUCIDATE THE DISTRIBUTION AND OCCURRENCE OF BASIN EJECTA. THE NEW GEOLOGICAL MAPS WILL BE USED IN CONJUNCTION WITH ELEMENTAL AND MINERAL MAPS FROM THE CLEMENTINE AND LUNAR PROSPECTOR MISSIONS AND DETERMINE THE COMPOSITION OF INDIVIDUAL EJECTA UNITS. GEOLOGICAL MAPPING HAS IDENTIFIED PROBABLE DEPOSITS OF BASIN IMPACT MELT ON THE BASIS OF MORPHOLOGY OCCURRENCE AND COMPOSITION FOR THE ORIENTALE IMBRIUM AND CRISIUM BASINS. IN THE COURSE OF THIS STUDY I WILL SEARCH FOR ADDITIONAL DEPOSITS OF IMPACT MELT AT THESE AND OTHER BASINS OCCURRING BOTH AS REMNANTS OF THE INTERIOR MELT SHEET AND AS ISOLATED EJECTED MELT DEPOSITS. THE NEW GEOLOGICAL MAPPING AND COMPOSITIONAL INFORMATION WILL PERMIT ASSESSMENT OF THE HYPOTHESIS THAT VERY LARGE IMPACT MELT BODIES PRODUCED BY BASIN-FORMING IMPACTS MIGHT DIFFERENTIATE IN PLACE PRODUCING A SEQUENCE OF ROCKS THAT COULD BE MISTAKEN AS PRODUCTS FROM AN ENDOGENOUSLY PRODUCED MAGMA. FINDING BASIN IMPACT MELT IS IMPORTANT TO CHARACTERIZE THE STRUCTURE AND COMPOSITION OF THE LUNAR CRUST. IN ADDITION IMPACT MELTS ARE THE ONLY MATERIALS SUITABLE FOR THE DETERMINATION OF ABSOLUTE AGES FOR THE BASIN-FORMING IMPACTS AND THUS THESE SITES ARE HIGH-PRIORITY FOR FUTURE EXPLORATION INCLUDING ROBOTIC AND HUMAN SAMPLE RETURN MISSIONS. STUDY OF BASIN MELT AND EJECTA USING REMOTE SENSING DATA WILL SHED LIGHT ON THE PROCESSES OF LARGE-BODY IMPACTS AND THE SUBSEQUENT GEOLOGICAL EVOLUTION OF THE LUNAR CRUST. AS LARGE BASINS FORMED IN THE EARLY HISTORY OF BODIES OF THE SOLAR SYSTEM THIS WORK WILL SHED LIGHT ON THE EARLY GEOLOGICAL EVOLUTION OF ALL TERRESTRIAL PLANETS. DATA TO BE USED IN THIS WORK (CLEMENTINE MULTISPECTRAL IMAGES LUNAR PROSPECTOR ELEMENTAL MAPS KAGUYA AND LRO LASER ALTIMETRY AND LRO WAC DTM AND NAC IMAGES) ARE ALL AVAILABLE THROUGH THE PDS SYSTEM.2017-07-24 → ?$81K
80NSSC26K1114THE PROPOSAL'S PURPOSE IS TO ENABLE THE PI (USRA/LUNAR AND PLANETARY INSTITUTE) TO SERVE AS A MEMBER OF NASA'S LUNAR MAPPING PROGRAM (LMAP) TEAM. HER ROLE IS TO SUPPORT A TEAM-BASED CAMPAIGN-STYLE EFFORT TO PRODUCE HIGH-QUALITY INTERNALLY CONSISTENT GEOLOGIC MAPS OF SELECTED REGIONS OF THE MOON.2026-09-15 → 2027-09-14$45K
80NSSC23PC468SUPPORT FOR LUNAR RECONNAISSANCE2023-09-12 → 2026-03-14$30K
80NSSC20P1289ANDREW SHANER'S SUPPORT OF INTERNATIONAL OBSERVE THE MOON NIGHT'S NATIONAL PARTNERS.2020-06-09 → 2022-09-30$23K

Source: USAspending.gov prime award and subaward data (public domain), refreshed daily; last refreshed 2026-10-19 06:18 UTC.

Amounts are obligated to date, not contract ceilings. An award counts as lunar when its published description is about the Moon, and programs are tagged from that text; repeated or impossible subaward reports are shown but not summed. Subawards are only as complete as primes report them.

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