| 000 | 00000cam 2200000zi 4500 |
| 001 | 9.964953 |
|---|
| 003 | CaOODSP |
|---|
| 005 | 20260807134507 |
|---|
| 006 | m o d f |
|---|
| 007 | cr |n||||||||| |
|---|
| 008 | 260807t20152015oncdab ob f|0| 0 eng d |
|---|
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
|---|
| 043 | |an-cn--- |
|---|
| 086 | 1 |aM183-2/7852E-PDF |
|---|
| 245 | 00|aTargeted Geoscience Initiative 4 : |bcontributions to the understanding of Precambrian lode gold deposits and implications for exploration / |cB. Dubé and P. Mercier-Langevin (editors). |
|---|
| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2015. |
|---|
| 264 | 4|c©2015 |
|---|
| 300 | |a1 online resource (ii, 293 pages) : |bcharts, illustrations, maps. |
|---|
| 336 | |atext|btxt|2rdacontent |
|---|
| 337 | |acomputer|bc|2rdamedia |
|---|
| 338 | |aonline resource|bcr|2rdacarrier |
|---|
| 490 | 1 |aOpen file, |x2816-7155 ; |v7852 |
|---|
| 520 | |a"The TGI-4 Lode Gold project, which comprises numerous site-specific and thematic research activities, covers the entire spectrum of crustal settings for lode gold deposits, from orogenic banded iron formation hosted and greenstone-hosted quartz carbonate vein-type gold deposits formed deep in the crust (>5 km), to intrusion-related deposits that are formed at shallower crustal levels (~2–5 km), and to deposits formed at or near the seafloor. Herein we synthesize a number of important project contributions that have significant implications for on-going mineral exploration for hidden deposits"--Abstract, page 3. |
|---|
| 650 | 0|aGold mines and mining|zCanada. |
|---|
| 650 | 0|aGeology, Stratigraphic|xPrecambrian. |
|---|
| 650 | 6|aOr|xMines et extraction|zCanada. |
|---|
| 650 | 6|aStratigraphie|xPrécambrien. |
|---|
| 700 | 1 |aDubeĢ, Benoit, |eeditor. |
|---|
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
|---|
| 830 | #0|aOpen file (Geological Survey of Canada)|v7852.|w(CaOODSP)9.506878 |
|---|
| 856 | 40|qPDF|s108 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-7852-eng.pdf |
|---|
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/296624 |
|---|