Display title | Physics:Paleostress inversion |
Default sort key | Paleostress inversion |
Page length (in bytes) | 26,880 |
Namespace ID | 3020 |
Namespace | Physics |
Page ID | 445230 |
Page content language | en - English |
Page content model | wikitext |
Indexing by robots | Allowed |
Number of redirects to this page | 0 |
Counted as a content page | Yes |
HandWiki item ID | None |
Edit | Allow all users (infinite) |
Move | Allow all users (infinite) |
Page creator | imported>LinuxGuru |
Date of page creation | 06:41, 5 February 2024 |
Latest editor | imported>LinuxGuru |
Date of latest edit | 06:41, 5 February 2024 |
Total number of edits | 1 |
Recent number of edits (within past 90 days) | 0 |
Recent number of distinct authors | 0 |
Description | Content |
Article description: (description ) This attribute controls the content of the description and og:description elements. | Paleostress inversion refers to the determination of paleostress history from evidence found in rocks, based on the principle that past tectonic stress should have left traces in the rocks. Such relationships have been discovered from field studies for years: qualitative and quantitative analyses of... |