scholarly journals Fluid inclusion and stable isotope evidence for mixing of magmatic - hydrothermal fluids with meteoric water in vein-type Cu-Au-Bi deposits, southern New Brunswick, Canada

2015 ◽  
Author(s):  
J J Hanley ◽  
F Tweedale ◽  
K Neyedley ◽  
R Sharpe ◽  
M Fayek
Keyword(s):  
Stable Isotope ◽  
Fluid Inclusion ◽  
New Brunswick ◽  
Meteoric Water ◽  
Hydrothermal Fluids ◽  
Vein Type ◽  
Isotope Evidence

Giant quartz vein formation and high-elevation meteoric fluid infiltration into the South Armorican Shear Zone: geological, fluid inclusion and stable isotope evidence

2012 ◽  
Vol 169 (1) ◽  
pp. 17-27 ◽  
Author(s):  
Jérémie Lemarchand ◽  
Philippe Boulvais ◽  
Martin Gaboriau ◽  
Marie-Christine Boiron ◽  
Romain Tartèse ◽  
...  
Keyword(s):  
Stable Isotope ◽  
Fluid Inclusion ◽  
Shear Zone ◽  
Quartz Vein ◽  
High Elevation ◽  
The South ◽  
Vein Formation ◽  
Fluid Infiltration ◽  
Isotope Evidence

Pressure, temperature and fluid conditions during emerald precipitation, southeastern Yukon, Canada: fluid inclusion and stable isotope evidence

2003 ◽  
Vol 194 (1-3) ◽  
pp. 187-199 ◽  
Author(s):  
Dan Marshall ◽  
Lee Groat ◽  
Gaston Giuliani ◽  
Don Murphy ◽  
Dave Mattey ◽  
...  
Keyword(s):  
Stable Isotope ◽  
Fluid Inclusion ◽  
Isotope Evidence

scholarly journals Isotope Evidence of Rainfall and Groundwater for Tracing Recharge Areas in Kaeng Khoi District, Saraburi Province, Thailand

2016 ◽  
pp. 49-58 ◽  
Author(s):  
Wanlapa Wisittammasri ◽  
Srilert Chotpantarat
Keyword(s):  
Stable Isotopes ◽  
Surface Water ◽  
Stable Isotope ◽  
Meteoric Water ◽  
Water Line ◽  
Meteoric Water Line ◽  
Isotope Technique ◽  
Isotope Evidence ◽  
Stable Isotope Technique ◽  
Central Thailand

This study was conducted in the districts of Kaeng Khoi and Muang, located in the center of Saraburiprovince, Central Thailand. The purpose was to use a stable isotope technique to iden-tify recharge areas where rainfall infiltrates. Analysis of stable isotopes in groundwater, surface water and rainwater were conducted in September 2014. Isotope compositions of groundwater were found to have δD values that ranged from -37.55‰ to -48.04‰ while δ18O values ranged from -5.30‰ to -7.34‰. The Local Meteoric Water Line (LMWL) in the study area was indis-tinguishablefrom the Bangkok Local Meteoric Water Line (BKK LMWL), and the stable iso-tope values of rainwater in area were more depleted than BKK LMWL. The isotope compo-sitions of surface water revealed that the effect of evaporation could divide the groundwater into two groups, with the first group locally receiving rainfall and the second group interacting directly with surface water. Therefore, care must be taken to prevent groundwater contamination in the latter group due to polluted surface water caused by human activities.

Sign in / Sign up

Export Citation Format

Share Document