![Geology, mineralogy, S and Sr isotope geochemistry, and fluid inclusion analysis of barite associated with the Lemarchant Zn–Pb–Cu–Ag–Au-rich volcanogenic massive sulphide deposit, Newfoundland, Canada Geology, mineralogy, S and Sr isotope geochemistry, and fluid inclusion analysis of barite associated with the Lemarchant Zn–Pb–Cu–Ag–Au-rich volcanogenic massive sulphide deposit, Newfoundland, Canada](https://cdnsciencepub.com/cms/10.1139/cjes-2018-0161/asset/images/large/cjes-2018-0161f9.jpeg)
Geology, mineralogy, S and Sr isotope geochemistry, and fluid inclusion analysis of barite associated with the Lemarchant Zn–Pb–Cu–Ag–Au-rich volcanogenic massive sulphide deposit, Newfoundland, Canada
Arch. Metall. Mater. 62 (2017), 2, 697-702 1. Introduction Barite (barium sulfate BaSO4) and barite aggregates find widespread u
![The Kohlou barite deposit, Markazi Province, Iran: studies on rare earth element geochemistry, O and S isotopes, and fluid inclusions | SpringerLink The Kohlou barite deposit, Markazi Province, Iran: studies on rare earth element geochemistry, O and S isotopes, and fluid inclusions | SpringerLink](https://media.springernature.com/lw685/springer-static/image/art%3A10.1007%2Fs13146-022-00785-2/MediaObjects/13146_2022_785_Fig4_HTML.jpg)
The Kohlou barite deposit, Markazi Province, Iran: studies on rare earth element geochemistry, O and S isotopes, and fluid inclusions | SpringerLink
![Minerals | Free Full-Text | Controls on Barite Mineralization in a Major Intracontinental Shear Zone: Carboniferous of the Cobequid Highlands, Nova Scotia Minerals | Free Full-Text | Controls on Barite Mineralization in a Major Intracontinental Shear Zone: Carboniferous of the Cobequid Highlands, Nova Scotia](https://pub.mdpi-res.com/minerals/minerals-11-01413/article_deploy/html/images/minerals-11-01413-g005.png?1639474062)
Minerals | Free Full-Text | Controls on Barite Mineralization in a Major Intracontinental Shear Zone: Carboniferous of the Cobequid Highlands, Nova Scotia
![Figure F70. Barite (low birefringence) replacing and overgrowing anhydrite in a quartz-breccia matrix (interval 193-1189B-13R-1, 34-36 cm, Unit 20, in cross-polarized light; width of view = 1.4 mm [Photomicrograph ID# 1189B_54; thin Figure F70. Barite (low birefringence) replacing and overgrowing anhydrite in a quartz-breccia matrix (interval 193-1189B-13R-1, 34-36 cm, Unit 20, in cross-polarized light; width of view = 1.4 mm [Photomicrograph ID# 1189B_54; thin](http://www-odp.tamu.edu/publications/193_IR/chap_04/images/04_f70.jpg)
Figure F70. Barite (low birefringence) replacing and overgrowing anhydrite in a quartz-breccia matrix (interval 193-1189B-13R-1, 34-36 cm, Unit 20, in cross-polarized light; width of view = 1.4 mm [Photomicrograph ID# 1189B_54; thin
![Observations in petrographic thin sections of secondary features in... | Download Scientific Diagram Observations in petrographic thin sections of secondary features in... | Download Scientific Diagram](https://www.researchgate.net/publication/355486246/figure/fig4/AS:1082362796474368@1635066808050/Observations-in-petrographic-thin-sections-of-secondary-features-in-some-collected.png)
Observations in petrographic thin sections of secondary features in... | Download Scientific Diagram
![Bulletin of the Geological Society of America. Geology. F&.3. Flg.G Figure 1.—Thin-sections of oolitic and pisolitic Barite Figures 1 and 2. Pisolitic barite (3 diameters). Figure 3. Barite ring resembling travertine ( Bulletin of the Geological Society of America. Geology. F&.3. Flg.G Figure 1.—Thin-sections of oolitic and pisolitic Barite Figures 1 and 2. Pisolitic barite (3 diameters). Figure 3. Barite ring resembling travertine (](https://c8.alamy.com/comp/RGH123/bulletin-of-the-geological-society-of-america-geology-famp3-flgg-figure-1thin-sections-of-oolitic-and-pisolitic-barite-figures-1-and-2-pisolitic-barite-3-diameters-figure-3-barite-ring-resembling-travertine-3-diameters-figure-4-large-oolites-2-diameters-figure-5-thin-sec-tion-of-oolite-showing-central-structure-and-fine-lines-25-diameters-figure-6-thin-section-of-oolite-without-well-marked-concentric-spheres-arranged-and-the-spheres-marked-by-very-fine-lines-it-appears-that-the-con-cretions-began-to-form-by-deposition-of-barite-in-both-a-crystalline-and-earthy-RGH123.jpg)