Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 Database

We examined the hypothesis that the crater formation rate exhibits periodicity, employing data sets of Grieve (1991), Moon et al. (2001), and the Earth Impact Database (2002; DB02). DB02 is known to supercede previous compilations in terms of its accuracy and precision of the ages; it is the first t...

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Main Authors: Hong-Kyu Moon, Byung-Hee Min, Seung-Lee Kim
Format: Article
Language:English
Published: Korean Space Science Society (KSSS) 2003-12-01
Series:Journal of Astronomy and Space Sciences
Subjects:
Online Access:http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2003/v20n4/OJOOBS_2003_v20n4_269.pdf
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spelling doaj-8feacee8fd6349ee8654156505689ab82020-11-25T00:54:38ZengKorean Space Science Society (KSSS)Journal of Astronomy and Space Sciences2093-55872093-14092003-12-0120426928210.5140/JASS.2003.20.4.269Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 DatabaseHong-Kyu Moon0Byung-Hee Min1Seung-Lee Kim2Korea Astronomy Observatory, Yusong, Daejon 305-348, KoreaKorea Astronomy Observatory, Yusong, Daejon 305-348, KoreaKorea Astronomy Observatory, Yusong, Daejon 305-348, KoreaWe examined the hypothesis that the crater formation rate exhibits periodicity, employing data sets of Grieve (1991), Moon et al. (2001), and the Earth Impact Database (2002; DB02). DB02 is known to supercede previous compilations in terms of its accuracy and precision of the ages; it is the first time that this database has been used for periodicity analysis. For data sets comprising impact structures with D≥5km (and also those with D≥20km), there is no convincing evidence for periodicities in the crater ages, according to our Fourier analysis. However, we detected two peaks at 16.1Myr and 34.7Myr for craters with D≥30km; we confirm that the age distribution of impact craters with D≥45km has dominant power at 16.1Myr. Thus, we may conjecture a probable periodic shower of Earth impactors with sizes d≥1.5km. In addition, we found that the selection of data sets, the lower limits on the ages and diameters of impact craters, as well as the accuracy and precision of the ages, all constitute crucial factors in reconstructing the impact cratering history of the Earth.http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2003/v20n4/OJOOBS_2003_v20n4_269.pdfterrestrial impact cratersperiodicity of impacts
collection DOAJ
language English
format Article
sources DOAJ
author Hong-Kyu Moon
Byung-Hee Min
Seung-Lee Kim
spellingShingle Hong-Kyu Moon
Byung-Hee Min
Seung-Lee Kim
Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 Database
Journal of Astronomy and Space Sciences
terrestrial impact craters
periodicity of impacts
author_facet Hong-Kyu Moon
Byung-Hee Min
Seung-Lee Kim
author_sort Hong-Kyu Moon
title Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 Database
title_short Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 Database
title_full Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 Database
title_fullStr Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 Database
title_full_unstemmed Terrestrial Impact Cratering Chronology II: Periodicity Analysis with the 2002 Database
title_sort terrestrial impact cratering chronology ii: periodicity analysis with the 2002 database
publisher Korean Space Science Society (KSSS)
series Journal of Astronomy and Space Sciences
issn 2093-5587
2093-1409
publishDate 2003-12-01
description We examined the hypothesis that the crater formation rate exhibits periodicity, employing data sets of Grieve (1991), Moon et al. (2001), and the Earth Impact Database (2002; DB02). DB02 is known to supercede previous compilations in terms of its accuracy and precision of the ages; it is the first time that this database has been used for periodicity analysis. For data sets comprising impact structures with D≥5km (and also those with D≥20km), there is no convincing evidence for periodicities in the crater ages, according to our Fourier analysis. However, we detected two peaks at 16.1Myr and 34.7Myr for craters with D≥30km; we confirm that the age distribution of impact craters with D≥45km has dominant power at 16.1Myr. Thus, we may conjecture a probable periodic shower of Earth impactors with sizes d≥1.5km. In addition, we found that the selection of data sets, the lower limits on the ages and diameters of impact craters, as well as the accuracy and precision of the ages, all constitute crucial factors in reconstructing the impact cratering history of the Earth.
topic terrestrial impact craters
periodicity of impacts
url http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2003/v20n4/OJOOBS_2003_v20n4_269.pdf
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