This is a PDF-only article. The first page of the PDF of this article appears above.
This article requires a subscription to view the full text. If you have a subscription you may use the login form below to view the article. Access to this article can also be purchased.
Log in using your username and password
Purchase access
You may purchase access to this article. This will require you to create an account if you don't already have one.
In this issue
Liquid-vapor relations for the system NaCl-H 2 O; summary of the P-T-x surface from 300 degrees to 500 degrees C
Jump to section
Related Articles
Cited By...
- Hydrogeological challenges in a low-carbon economy
- Physical-chemical properties and metal budget of Au-transporting hydrothermal fluids in orogenic deposits
- Distribution of Sulfur Between Melt and Fluid in S-O-H-C-Cl-Bearing Magmatic Systems at Shallow Crustal Pressures and Temperatures
- Synthetic Fluid Inclusions. XVII. PVTX Properties of High Salinity H2O-NaCl Solutions (>30 wt % NaCl): Application to Fluid Inclusions that Homogenize by Halite Disappearance from Porphyry Copper and Other Hydrothermal Ore Deposits
- The Cu Stockwork and Massive Sulfide Ore of the Feitais Volcanic-Hosted Massive Sulfide Deposit, Aljustrel, Iberian Pyrite Belt, Portugal: A Mineralogical, Fluid Inclusion, and Isotopic Investigation
- Fluid-Fluid Interactions in Geothermal Systems
- Experimental Studies in Model Fluid Systems
- Fluid Immiscibility in Volcanic Environments
- Magmatic Fluids in the Breccia-Hosted Epithermal Au-Ag Deposit of Rosia Montana, Romania
- Quantitative analysis of fluid inclusions by synchrotron X-ray fluorescence: calibration of Cu and Zn in synthetic quartz inclusions
- NEW FIELD EVIDENCE BEARING ON THE ORIGIN OF THE EL LACO MAGNETITE DEPOSIT, NORTHERN CHILE--A DISCUSSION
- Formation of a Magmatic-Hydrothermal Ore Deposit: Insights with LA-ICP-MS Analysis of Fluid Inclusions
- Organic matter alteration and fluid migration in hydrothermal systems