Description
Location: Western Folklife Center, 501 Railroad St., Elko, NV
Contact: Sergey606@gmail.com
The GSN Elko Chapter invites you to their January meeting!
Thursday, January 15, 2026
Western Folklife Center, 501 Railroad St., Elko, NV
Food and Drinks @ 6 p.m., Talk @ 7 p.m.
FOOD & BEER SPONSOR: TONATEC
Speaker: Lauren Terry
Title: “Microtextural characteristics of adularia in banded quartz veins from the Midas low-sulfidation epithermal deposit, Nevada”
Abstract: High-grade ores at the Miocene Midas low-sulfidation epithermal deposit in northern Nevada are confined to crustiform quartz veins containing abundant adularia. Micro-X-ray fluorescence elemental mapping reveals that adularia is a common gangue mineral occurring in colloform bands, bands showing bladed textures, and bands with dendritic terminations. The adularia aggregates have delicate shapes and are comprised of stacked, submillimeter crystals hosted by fine-grained quartz. The textural evidence suggests that the adularia aggregates originally formed within a gel-like noncrystalline silica matrix that subsequently transformed into quartz. This indicates that the adularia did not precipitate in open space along the vein walls. Correlative microscopy, involving scanning electron microscopy-based automated mineralogy and optical petrography, demonstrates that bands containing abundant adularia are not the primary host to ore minerals. The ore minerals occur within different bands in the crustiform veins, implying that adularia and ore mineral precipitation did not always occur at the same time. It is hypothesized here that fluid flow at Midas involved intermittent short-lived events of fluid flashing, causing rapid solute supersaturation in the liquid. During each flashing event, different amounts of vapor were produced along a given vein. Compositional differences between adjacent bands in the crustiform quartz veins may, therefore, be linked to variations in the amount of vapor formed during each flash event.
Please contact Elko Chapter President, Sergey Konyshev if you have any questions. Sergey606@gmail.com
Details
01/15/2026 18:00:0001/15/2026 21:00:00America/Los_AngelesGSN Elko Chapter Meeting – Thursday, January 15thThe GSN Elko Chapter invites you to their January meeting!
Thursday, January 15, 2026
Western Folklife Center, 501 Railroad St., Elko, NV
Food and Drinks @ 6 p.m., Talk @ 7 p.m.
FOOD & BEER SPONSOR: TONATEC
Speaker: Lauren Terry
Title: “Microtextural characteristics of adularia in banded quartz veins from the Midas low-sulfidation epithermal deposit, Nevada”
Abstract: High-grade ores at the Miocene Midas low-sulfidation epithermal deposit in northern Nevada are confined to crustiform quartz veins containing abundant adularia. Micro-X-ray fluorescence elemental mapping reveals that adularia is a common gangue mineral occurring in colloform bands, bands showing bladed textures, and bands with dendritic terminations. The adularia aggregates have delicate shapes and are comprised of stacked, submillimeter crystals hosted by fine-grained quartz. The textural evidence suggests that the adularia aggregates originally formed within a gel-like noncrystalline silica matrix that subsequently transformed into quartz. This indicates that the adularia did not precipitate in open space along the vein walls. Correlative microscopy, involving scanning electron microscopy-based automated mineralogy and optical petrography, demonstrates that bands containing abundant adularia are not the primary host to ore minerals. The ore minerals occur within different bands in the crustiform veins, implying that adularia and ore mineral precipitation did not always occur at the same time. It is hypothesized here that fluid flow at Midas involved intermittent short-lived events of fluid flashing, causing rapid solute supersaturation in the liquid. During each flashing event, different amounts of vapor were produced along a given vein. Compositional differences between adjacent bands in the crustiform quartz veins may, therefore, be linked to variations in the amount of vapor formed during each flash event.| Event Starts | Event Ends |
| 01/15/2026 | 01/15/2026 |
| All Day Event | |
| 6:00pm | 9:00pm |
