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DOI: 10.1002/2015GL066537
论文题名:
Regolith stratigraphy at the Chang'E-3 landing site as seen by lunar penetrating radar
作者: Fa W.; Zhu M.-H.; Liu T.; Plescia J.B.
刊名: Geophysical Research Letters
ISSN: 0094-8332
EISSN: 1944-8063
出版年: 2015
卷: 42, 期:23
起始页码: 10179
结束页码: 10187
语种: 英语
英文关键词: ejecta ; lunar penetrating radar ; paleoregolith ; regolith thickness ; stratigraphy
Scopus关键词: Moon ; Radar ; Stratigraphy ; Accumulation rates ; ejecta ; Initial depositions ; Landing site ; paleoregolith ; Penetrating radar ; regolith thickness ; Surface age ; Lunar landing
英文摘要: The Chang'E-3 lunar penetrating radar (LPR) observations at 500 MHz reveal four major stratigraphic zones from the surface to a depth of ∼20 m along the survey line: a layered reworked zone (<1 m), an ejecta layer (∼2-6 m), a paleoregolith layer (∼4-11 m), and the underlying mare basalts. The reworked zone has two to five distinct layers and consists of surface regolith. The paleoregolith buried by the ejecta from a 500 m crater is relatively homogenous and contains only a few rocks. Population of buried rocks increases with depth to ∼2 m at first, and then decreases with depth, representing a balance between initial deposition of the ejecta and later turnover of the regolith. Combining with the surface age, the LPR observations indicate a mean accumulation rate of about 5-10 m/Gyr for the surface regolith, which is at least 4-8 times larger than previous estimation. © 2015. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84953439501&doi=10.1002%2f2015GL066537&partnerID=40&md5=f2b4b305c8ce3d00bc9a566e51a43828
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/7948
Appears in Collections:科学计划与规划
气候变化与战略

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作者单位: Institute of Remote Sensing and Geographical Information System, Peking University, Beijing, China

Recommended Citation:
Fa W.,Zhu M.-H.,Liu T.,et al. Regolith stratigraphy at the Chang'E-3 landing site as seen by lunar penetrating radar[J]. Geophysical Research Letters,2015-01-01,42(23).
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