| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.949447 |
| 003 | CaOODSP |
| 005 | 20250822122643 |
| 006 | m o d f |
| 007 | cr cn |||||||| |
| 008 | 250324t20252025oncabo ob f000 0 eng d |
| 020 | |a9780660766164 |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 086 | 1 |aM41-11/175-2025E-PDF |
| 100 | 1 |aCawood, T. K., |eauthor. |
| 245 | 10|aIs there a link between orogenic collapse and lithium-bearing pegmatites? / |cTarryn Kim Cawwod, Jamie Cutts, Antoine Godet. |
| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2025. |
| 264 | 4|c©2025 |
| 300 | |a1 online resource (33 unnumbered pages) : |billustrations, maps, photographs. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aScientific presentation ; |v175 |
| 500 | |aPresented at the Sustainable Mineral Exploration and Development SEG Conference, September 27-30, 2024, Namibia. |
| 504 | |aIncludes bibliographical references. |
| 520 | |a"Lithium-bearing pegmatites are typically found in the eroded remnants of mountain belts, and are thought to form during the mountain building events. However, we suggest that many lithium-bearing pegmatites actually form later, when the thickened crust of the mountain belt collapses under its own weight. We cite several examples from around the world to support this idea"--Provided from the publisher. |
| 650 | 0|aOrogenic belts. |
| 650 | 0|aPegmatites. |
| 650 | 0|aLithium. |
| 650 | 6|aCeintures orogéniques. |
| 650 | 6|aPegmatites. |
| 650 | 6|aLithium. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aScientific presentation (Geological Survey of Canada)|v175.|w(CaOODSP)9.820265 |
| 856 | 40|qPDF|s10.9 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m41-11/M41-11-175-2025-eng.pdf |
| 856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/pkm7sta6f5 |