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  • 1
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    Mining and beneficiation of lunar ores (1979)
    In:  CASI
    Details
    Publication Date: 2006-01-12
    Description: The beneficiation of lunar plagioclase and ilmenite ores to feedstock grade permits a rapid growth of the space manufacturing economy by maximizing the production rate of metals and oxygen. A beneficiation scheme based on electrostatic and magnetic separation is preferred over conventional schemes, but such a scheme cannot be completely modeled because beneficiation processes are empirical and because some properties of lunar minerals have not been measured. To meet anticipated shipping and processing needs, the peak lunar mining rate will exceed 1000 tons/hr by the fifth year of operation. Such capabilities will be best obtained by automated mining vehicles and conveyor systems rather than trucks. It may be possible to extract about 40 kg of volatiles (60 percent H2O) by thermally processing the less than 20 micron ilmenite concentrate extracted from 130 tons of ilmenite ore. A thermodynamic analysis of an extraction process is presented.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Space Resources and Space Settlements; p 275-288
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  • 2
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    A geologic assessment of potential lunar ores (1979)
    In:  CASI
    Details
    Publication Date: 2006-01-12
    Description: Although bulk lunar soil is not a suitable feedstock for extracting metals, certain minerals such as anorthite and ilmenite can be separated and concentrated. These minerals can be considered as potential ores of aluminum, silicon, titanium, andiron. A separation and metal extraction plant could also extract large amounts of oxygen and perhaps hydrogen from these minerals. Anorthie containing 19 percent aluminum and 20 percent silicon can be concentrated from some highland soils where it is present in amounts up to 60 percent. Ilmenite containing 32 percent titanium and 37 percent iron can be concentrated from some mare soils where it is present in amounts up to 10 percent. The ideal mining site would be located at the boundary between a high-titanium mare and a high-aluminum highlands. Such area may exist around the rims of some eastern maria, particularly Tranquilitatis. A location on Earth with raw materials as described above would be considered an economically valuable ore deposit if conventional terrestrial resources were not available.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: NASA. Ames Res. Center Space Resources and Space Settlements; p 243-255
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  • 3
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    A refractory glass chondrule in the Vigarano chondrite (1974)
    In:  Other Sources
    Details
    Publication Date: 2011-08-16
    Description: Vigarano, a type 3 carbonaceous chondrite, contains a chondrule composed of highly refractory Ca- and Al-rich glass with minor spinel. The chondrule formed from material similar to the Ca-, Al-, Ti-rich aggregates that are common in Vigarano and other type 3 chondrites and formation of these refractory aggregates must predate formation of some Vigarano chondrules. Experiments with synthetic analogs and a comparison with studies in the system CaO-MgO-Al2O3-SiO2 indicate a temperature for formation of the chondrule at or above 1700 C followed by very rapid cooling.
    Keywords: SPACE SCIENCES
    Type: Meteoritics; 9; Mar. 30
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  • 4
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    The lithification and metamorphism of lunar breccias. (1972)
    In:  Other Sources
    Details
    Publication Date: 2011-08-16
    Description: Investigations regarding the textural and mineralogical classification of Apollo 14 breccias are considered together with some related experimental studies. The experiments can be used to construct a temperature scale which may be called the 'petrogenetic line' for lunar breccias. A model for the Fra Mauro formation is also discussed. The most interesting facts revealed by the discussion are the intensity of heating involved and the short times necessary to develop the physical properties of the Apollo 14 breccias. The purpose of the studies is to construct a scale of lunar metamorphic temperatures which is consistent with experimentally determined conditions necessary for the acquisition of certain properties by the lunar breccias.
    Keywords: SPACE SCIENCES
    Type: Earth and Planetary Science Letters; 16; Oct. 197
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  • 5
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    The origin and stability of lunar goethite, hematite and magnetite. (1972)
    In:  Other Sources
    Details
    Publication Date: 2011-08-16
    Description: Extra-lunar contamination, fumarolic activity, and exposure to oxidizing gases from comet or carbonaceous meteorite impacts have been previously proposed as the causes of magnetite, hematite, and goethite in lunar materials. However, these minerals can occur in the stable low-temperature gas-solid equilibrium assemblages of lunar rocks. Below 600 C magnetite is in equilibrium with C-O-H gases with compositions compatible with high-temperature equilibrium with metallic iron; below 150 C hematite is stable in these same gases. Goethite is not stable in carbonaceous gases at low total pressure, and thus gases from impacting carbonaceous material cannot have produced it. Goethite is stable at low temperatures and pressures in almost pure H2-H2O gases. Its minimum stability against hematite is 2 bars total pressure at 130 C and 0.001 bars at 30 C for H2 to H2O ratios compatible with the high-temperature redox state of lunar materials. Thus the traces of magnetite, hematite, and goethite in lunar materials may be the result of normal low-temperature processes indigenous to the moon and not special processes.
    Keywords: SPACE SCIENCES
    Type: Earth and Planetary Science Letters; 17; Dec. 197
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  • 6
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    Report of Workshop on Methodology for Evaluating Potential Lunar Resources Sites (1981)
    In:  CASI
    Details
    Publication Date: 2019-06-28
    Description: The type and quantity of lunar materials needed to support a space power satellite program was used to define the type and quality of geological information required to certify a site for exploitation. The existing geological, geochemical, and geophysical data are summarized. The difference between these data and the required data for exploitation is used to define program requirements. Most of these requirements involve linear extensions of existing capabilities, fuller utilization of existing data, or expanded use of automated systems.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: NASA-TM-58235 , JSC-17058 , Houston, TX; United States
    Format: application/pdf
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  • 7
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    Handbook of lunar materials (1980)
    In:  CASI
    Details
    Publication Date: 2019-06-27
    Description: The physical, chemical, thermodynamic, and geologic data on lunar rocks, minerals, and processes are summarized, and a set of data metals that might be extracted from lunar materials is presented.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: NASA-RP-1057
    Format: application/pdf
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  • 8
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    Equilibrium temperatures, pressures, and oxygen fugacities of the equilibrated chondrites (1971)
    In:  Other Sources
    Details
    Publication Date: 2019-06-27
    Description: Equilibrium temperatures, pressures and oxygen fugacities of equilibrated chondrites in meteorites
    Keywords: SPACE SCIENCES
    Type: ; OMBUSTION IN A FLOW
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  • 9
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    Experimentally reproduced textures and mineral chemistries of high-titanium mare basalts (1975)
    In:  Other Sources
    Details
    Publication Date: 2019-07-13
    Description: Many of the textures, morphologies, and mineral chemistries of the high-titanium mare basalts have been experimentally duplicated using single-stage cooling histories. Lunar high-titanium mare basalts are modeled in a 1 m thick gravitationally differentiating flow based on cooling rates, thermal models, and modal olivine contents. The low-pressure equilibrium phase relations of a synthetic high-titanium basalt composition were investigated as a function of oxygen fugacity, and petrographic criteria are developed for the recognition of phenocrysts which were present in the liquid at the time of eruption.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Lunar Science Conference; Mar 17, 1975 - Mar 21, 1975; Houston, TX
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  • 10
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    The system anorthite-forsterite-fayalite-silica to 2 kbar with lunar petrologic applications (1975)
    In:  Other Sources
    Details
    Publication Date: 2019-07-13
    Description: Near-liquidus phase relations in the magnesium-rich portion of the system anorthite-forsterite-fayalite-silica have been determined from synthesis experiments at 1 atm and 2 kbar at oxygen fugacities near the iron-wuestite buffer. The major-element chemistries of KREEP basalts are similar to peritectic liquids, L/ol,px,an/, produced experimentally. The reaction L/ol,px,an/ is well-located at low pressures. It intersects the join anorthite-enstatite-ferrosilite at Fe/(Fe+Mg) equals 0.45 (atomic ratio), and is peritectic only for Fe/(Fe+Mg) not greater than 0.45. Although positions of the equilibria, L/an,ol/ and L/ol,px/, differ significantly at 1 atm from their positions at 2 kbar, the position of the piercing point, L/ol,px,an/, on the anorthite-enstatite-ferrosilite join is not sensitive to pressure. The composition of liquids produced by partial melting of troctolites and pyroxenites in the lunar crustal environment will be affected by pressure, whereas liquids derived from gabbroic assemblages will not.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Lunar Science Conference; Mar 17, 1975 - Mar 21, 1975; Houston, TX
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