1985
DOI: 10.1007/978-94-009-5464-9_19
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The Interplanetary Micrometeoroid Flux and Lunar Primary and Secondary Microcraters

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“…Additional sources of damage are the fast secondary ejecta particles that have speeds above the lunar escape speed, generated at shallow angles [26]. They dominate the generation of micro craters with diameters below 7 μm observed on lunar rocks [27,28]. The cratering rate of these small pits, compared with the predictions based on in situ measurements of micrometeoroids in space, indicate a flux of fast ejecta 10 normalm2 normals1 of particles with radii 1 μm [9], that generates a negligibly slow surface degradation rate due to cratering.…”
Section: High-altitude Dust Ejecta Cloudmentioning
confidence: 99%
“…Additional sources of damage are the fast secondary ejecta particles that have speeds above the lunar escape speed, generated at shallow angles [26]. They dominate the generation of micro craters with diameters below 7 μm observed on lunar rocks [27,28]. The cratering rate of these small pits, compared with the predictions based on in situ measurements of micrometeoroids in space, indicate a flux of fast ejecta 10 normalm2 normals1 of particles with radii 1 μm [9], that generates a negligibly slow surface degradation rate due to cratering.…”
Section: High-altitude Dust Ejecta Cloudmentioning
confidence: 99%