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New Insights into the Steinheim Central Uplift - Part III: Shatter Cones and the `Cone-in-Cone' Problem Reloaded
| Content Provider | Semantic Scholar |
|---|---|
| Author | Schmieder, Martin Buchner, Elmar |
| Copyright Year | 2010 |
| Abstract | Background: Specific conical features in terrestrial rocks may originate from various geologic processes, such as (1) shatter cones generated during (and diagnostic for) meteorite impact events [1], or (2) ‘cone-in-cone’ structures (‘Tutenmergel’ or ‘Nagelkalke’ in German) that may sometimes appear similar to shatter cones but which are thought to represent sedimentarydiagenetic phenomena [2;3]. A thorough systematic comparison and distinction between shatter cones and cone-in-cone structures is given by [4]. |
| File Format | PDF HTM / HTML |
| Alternate Webpage(s) | https://www.lpi.usra.edu/meetings/metsoc2010/pdf/5012.pdf |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |
