May 1, 1993

The Scaling of Impact Processes in Planetary Sciences

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Abstract

Carbonatites are igneous rocks formed in the crust by fractional crystallization of carbonate-rich parental melts that are mostly mantle derived. They dominantly consist of carbonate minerals such as calcite, dolomite, and ankerite, as well as minor ...Read More

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K. A. Holsapple (Sat,) studied this question.

synapsesocial.com/papers/69d6a9f5fca0359822aa7f35 https://doi.org/https://doi.org/10.1146/annurev.ea.21.050193.002001

Also Consider

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

1GEOMORPHOLOGY OF IMPACT CRATERS ON MERCURY1989 · 120 citations
2On the Existence and Implications of Coupling Parameters in Cratering Mechanics1983 · 9 citations
3A material-strength model for apparent crater volume.1979 · 32 citations
4Complete fragmentation of the parent bodies of Themis, Eos, and Koronis families1982 · 41 citations
5THEORY OF IMPACT: SOME GENERAL PRINCIPLES AND THE METHOD OF EULERIAN CODES1970 · 93 citations

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