Edithistory:Geology of Ray
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| 1314937888 | 2025-10-04T00:57:45Z | Citation bot | Altered template type. Add: chapter-url, isbn, pages, series, chapter, bibcode, doi, article-number, issue, volume, date, journal, title, authors 1-1. Removed or converted URL. Changed bare reference to CS1/2. Upgrade ISBN10 to 13. | [[:en:WP:UCB|Use this bot]]. [[:en:WP:DBUG|Report bugs]]. | Suggested by Eastmain | #UCB_webform 29/799 |
| 1314387588 | 2025-10-01T03:51:26Z | R Prazeres | [[WP:AFC|AFC]] draft |
| 1314387575 | 2025-10-01T03:51:24Z | R Prazeres | R Prazeres moved page [[Geology of Ray]] to [[Draft:Geology of Ray]]: [[WP:DRAFTIFY|Not ready]] for mainspace, incubate in draftspace. Reason/s: custom reason |
| 1314201541 | 2025-09-30T06:30:30Z | Nastaliqq | |
| 1314066925 | 2025-09-29T15:01:50Z | Dclemens1971 | Added tags to the page using [[Wikipedia:Page Curation|Page Curation]] (essay-like, linkrot) |
| 1314053708 | 2025-09-29T13:31:14Z | Nastaliqq | /* Ray’s Shaken Continuity */ |
| 1314053674 | 2025-09-29T13:30:55Z | Nastaliqq | /* Ray’s Shaken Continuity */ |
| 1314053574 | 2025-09-29T13:30:12Z | Nastaliqq | /* Ray’s Shaken Continuity */ |
| 1314053356 | 2025-09-29T13:28:44Z | Nastaliqq | /* Tectonic Archive */ |
| 1314052876 | 2025-09-29T13:25:14Z | Nastaliqq | /* Resources */ |
| 1314052643 | 2025-09-29T13:23:16Z | Nastaliqq | /* Tectonic Archive */ |
| 1314052139 | 2025-09-29T13:19:28Z | Nastaliqq | |
| 1314051849 | 2025-09-29T13:17:05Z | Nastaliqq | |
| 1314051770 | 2025-09-29T13:16:25Z | Nastaliqq | |
| 1314051665 | 2025-09-29T13:15:33Z | Nastaliqq | /* Chronology */ |
| 1314051215 | 2025-09-29T13:11:47Z | Nastaliqq | /* Chronology */ |
| 1314051119 | 2025-09-29T13:11:03Z | Nastaliqq | /* Magmatic Undercurrents */ |
| 1314050449 | 2025-09-29T13:05:35Z | Nastaliqq | |
| 1314050241 | 2025-09-29T13:03:48Z | Nastaliqq | |
| 1314050144 | 2025-09-29T13:03:05Z | Nastaliqq | |
| 1314050106 | 2025-09-29T13:02:46Z | Nastaliqq | [[WP:AES|←]]Created page with 'Ray is located within the tectonically-active Central Iranian zone, bordered by the Alborz Mountains to the north and the Lut Block to the east. This region has built up a complex, multi-layered geological profile shaped by repeated orogenic phases and magmatic intrusions. The bedrock consists of sedimentary, metamorphic, and igneous formations that date back to the Precambrian and Mesozoic eras. Geologists have pointed out that Ray sits atop fault-fracture...' |
