Regolith Formation
Regolith Formation is a geological process denoting the in situ development of unconsolidated, fragmented mineral and rock material at the surface of a planetary body through the mechanical and chemical breakdown of bedrock by weathering, impact, and other surficial processes.
160
Publications
9.3K
Citations
686
Authors
287
Institutions
Publications per year
2017–2026
52
160
The lunar regolith: Chemistry, mineralogy, and petrology
J. J. Papike, S. B. Simon, J. C. Laul · Reviews of Geophysics · 1982 · 331 citations
Evidence of atmospheric sulphur in the martian regolith from sulphur isotopes in meteorites
James Farquhar, Joël Savarino, T. L. Jackson et al. · Nature · 2000 · 290 citations
1–5 of 160
686
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Commonwealth Scientific and Industrial Research Organisation, Australia
4 publications · 625 citations
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4
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287

Pennsylvania State University
State College, United States
14 h-index
44 publications
4.1K citations

Centre National de la Recherche Scientifique
Paris, France
14 h-index
74 publications
6K citations
Johnson Space Center
Houston, United States
11 h-index
20 publications
1.1K citations
Planetary Science Institute
Tucson, United States
11 h-index
43 publications
6.6K citations
University of Arizona
Tucson, United States
8 h-index
41 publications
6.1K citations

Commonwealth Scientific and Industrial Research Organisation
Canberra, Australia
7 h-index
13 publications
1.6K citations
United States Geological Survey
Reston, United States
6 h-index
8 publications
829 citations
Arizona State University
Tempe, United States
5 h-index
10 publications
710 citations
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JGR · 12 publications · 939 citations
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9 publications · 531 citations
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8 publications · 348 citations
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8 publications · 583 citations
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8 publications · 199 citations
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