Exotic armalcolite and the origin of Apollo 11 ilmenite basalts
Armalcolite and ilmenite basalt in Apollo 11 lunar samples, discussing formation process of titanium, potassium and silicon oxides
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Armalcolite and ilmenite basalt in Apollo 11 lunar samples, discussing formation process of titanium, potassium and silicon oxides
The liquidus-solidus behavior of Apollo 11 lunar fines and the evolution characteristics of CO, nitrogen, He, Ne, and Ar were investigated by use of the combined techniques of high-vacuum differential thermal analysis (DTA) and mass spectrometry between 100 and 1500 C. The DTA thermogram has shown that the lunar fines undergo partial melting over a broad range of temperature from about 915 to 1300 C, with a significant initial melting of glassy and crystalline components within the fines at about 1140 C. The lunar material becomes a homogeneous melt at about 1300 C.
Historical film footage of Apollo 11 is shown. The pre-flight, launch, module docking, lunar orbit, lunar landing, ascent, and return-to-Earth flight is shown. There are lunar surface shots, Moon views, Earth views from Earth orbit, Earth views from the Moon, and footage of actual moon walk by astronauts. Mission control and space to ground control communication is heard.
Live footage shows the Apollo 11 crew, Commander Neil A. Armstrong, Lunar Module Pilot Edwin E. Aldrin, Jr., and Command Module Pilot Michael Collins, preparing for their mission. The crewmembers are seen getting their medical examinations, suiting up, and walking out to the Astro-van. Scenes include a brief view of the Launch Control Center (LCC), ignition, liftoff, and shell and engine skirt separation. The most important images are those of the moon landing and astronauts walk on the moon. Also shown are the parachute landing of the shuttle and the celebration of the world.
Preflight information on Apollo 11 manned lunar landing mission
Quick time transcript of lunar geology from Apollo 11
Carbon compounds composition and origin in Apollo 11 lunar samples using pyrolytic chromatography and microscopy at elevated temperature
Fission track uranium distribution studies of Apollo 11 lunar volcanic rocks, using Lexan plastic print method
Glass spherule lunar particles and breccia from Apollo 11 site, showing passage through impact generated cloud of hot fragmental material
Apollo 11 lunar basalt petrogenesis, examining internal constitution and origin by high pressure
Lunar petrology of silicate melt inclusions from Apollo 11 rock samples, discussing heating experiments
Lunar rocks petrography, mineralogy and petrogenesis from Apollo 11 samples
Apollo 11 lunar rocks and fines oxygen, Si and Al content determination by neutron activation analysis
Petrogenesis of Apollo 11 basalts and implications for lunar origin
Apollo 11 lunar samples dielectric constants, losses and electrical conductivities as function of temperature and frequency, comparing with terrestrial and simulated lunar rocks
A study of basaltic fragments from the Apollo 11 bulk sample using instrumental neutron activation analysis, the petrographic microscope, and the electron microprobe is presented. The fragments include Group A, B2, and B3 basalts, of which two of the Group A samples are vitrophyres with bulk compositions similar to the crystalline high-K rocks which crystallized under different physical conditions and represent a second high-K cooling unit. The B2 samples relate to each other through ilmenite fractionation, and the B3 samples relate through olivine fractionation; it is concluded that the B2 samples have an anomalously high La/K ratio and may have generated in the same source region as the Group D basalts.
The Gemini program and the Apollo program which culminated in landing a man on the moon and safely returning him to earth are highlighted. The space program in the aftermath of Apollo 11 is briefly summarized, including: Skylab, Apollo Soyuz, Mars and Venus probes, improved world communications, remote sensing of world resources, and finally, space shuttle.
Analysis of returned lunar samples provides limited information about lunar geology. To obtain information about in-place lunar material, a closeup stereoscopic camera capable of photographing small-scale surface features was built and was used at the Apollo 11 landing site. Stereoscopic photographs were taken of surface areas relative to the lunar module, and the surfaces photographed were analyzed. The photographs are classified into five groups: soil disturbed by astronaut activities, generally undisturbed soil, loose aggregate surface material, crater bottoms with prominent glass deposits, and hard rock deposits. Glass deposits in the returned samples are described for comparison with the features observed in the photographs. The stereoscopic photographs were of outstanding quality and show the nature of lunar-surface material in detail. Lunar topography was reconstructed from the photographs with an analytical plotter. The photography results indicate that the closeup composition and genesis of lunar soil at the Apollo 11 landing site.