SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIAL

I analysed and compared the size-frequency distributions of craters in the Apollo 17 landing region, comprising of six mare terrains with varying morphologies and cratering characteristics, along with three other regions allegedly affected by the same secondary event (Tycho secondary surge). I propo...

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Main Author: R. Bugiolacchi
Format: Article
Language:English
Published: Copernicus Publications 2017-07-01
Series:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Online Access:https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-3-W1/23/2017/isprs-archives-XLII-3-W1-23-2017.pdf
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spelling doaj-be5721aed22d468f805e7a57835aa09f2020-11-24T21:11:50ZengCopernicus PublicationsThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences1682-17502194-90342017-07-01XLII-3-W1232710.5194/isprs-archives-XLII-3-W1-23-2017SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIALR. Bugiolacchi0R. Bugiolacchi1Space Science Laboratory, MUST, Avenida Wai Long, Taipa, MacauDept. of Earth Sciences, University College London, Gower Street, WC1E 6BT, London, UKI analysed and compared the size-frequency distributions of craters in the Apollo 17 landing region, comprising of six mare terrains with varying morphologies and cratering characteristics, along with three other regions allegedly affected by the same secondary event (Tycho secondary surge). I propose that for the smaller crater sizes (in this work 9&ndash;30&thinsp;m), a] an exponential curve of power &minus;0.18D can approximate Nkm<sup>&minus;2</sup> crater densities in a regime of equilibrium, while b] a power function D<sup>&minus;3</sup> closely describes the factorised representation of craters by size (1&thinsp;m). The saturation level within the Central Area suggests that c] either the modelled rates of crater erosion on the Moon should be revised, or that the Tycho event occurred much earlier in time than the current estimate. We propose that d] the size-frequency distribution of small secondary craters may bear the signature (in terms of size-frequency distribution of debris/surge) of the source impact and that this observation should be tested further.https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-3-W1/23/2017/isprs-archives-XLII-3-W1-23-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Bugiolacchi
R. Bugiolacchi
spellingShingle R. Bugiolacchi
R. Bugiolacchi
SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIAL
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
author_facet R. Bugiolacchi
R. Bugiolacchi
author_sort R. Bugiolacchi
title SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIAL
title_short SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIAL
title_full SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIAL
title_fullStr SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIAL
title_full_unstemmed SMALL CRATERS AND THEIR DIAGNOSTIC POTENTIAL
title_sort small craters and their diagnostic potential
publisher Copernicus Publications
series The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
issn 1682-1750
2194-9034
publishDate 2017-07-01
description I analysed and compared the size-frequency distributions of craters in the Apollo 17 landing region, comprising of six mare terrains with varying morphologies and cratering characteristics, along with three other regions allegedly affected by the same secondary event (Tycho secondary surge). I propose that for the smaller crater sizes (in this work 9&ndash;30&thinsp;m), a] an exponential curve of power &minus;0.18D can approximate Nkm<sup>&minus;2</sup> crater densities in a regime of equilibrium, while b] a power function D<sup>&minus;3</sup> closely describes the factorised representation of craters by size (1&thinsp;m). The saturation level within the Central Area suggests that c] either the modelled rates of crater erosion on the Moon should be revised, or that the Tycho event occurred much earlier in time than the current estimate. We propose that d] the size-frequency distribution of small secondary craters may bear the signature (in terms of size-frequency distribution of debris/surge) of the source impact and that this observation should be tested further.
url https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-3-W1/23/2017/isprs-archives-XLII-3-W1-23-2017.pdf
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