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Bodnar, R.J. (1994) Synthetic Fluid Inclusions: XII. The System H2O-NaCl. Experimental Determination of the Halite Liquidus and Isochores for a 40 wt% NaCl Solution. Geochimica et Cosmochimica Acta, 58, 1053-1063.
http://www.sciencedirect.com/science/article/pii/0016703794905711
http://dx.doi.org/10.1016/0016-7037(94)90571-1

has been cited by the following article:

• TITLE: Fluid Inclusion Studies on Quartz Veinlets at the Ali Javad Porphyry Copper (Gold) Deposit, Arasbaran, Northwestern Iran

  AUTHORS: Behzad Hajalilou, Mehraj Aghazadeh

  KEYWORDS: Fluid Inclusion, Silica Veinlet, Porphyry Copper Deposit, Ali Javad, Arasbaran, Iran

  JOURNAL NAME: Journal of Geoscience and Environment Protection, Vol.4 No.6, June 14, 2016

  ABSTRACT: Ali Javad porphyry copper-gold deposit is located in Arasbaran porphyry copper belt at northwestern Iran, some 20 km east of Sungun Mine. Porphyry mineralization at the Ali Javad deposit occurred in post-Oligocene quartz monzonite bodies which intruded in the Eocene volcanic rocks. Mineralization occurred as veins, veinlets and dissemination both as hypogene and supergene type. Several types of veinlets were distinguished during the study of the deposit. Fluid inclusion studies on fluids trapped in quartz which were taken from drill core samples indicated a wide range of homogenization temperature in the veinlets from 138°C to 565°C which their salinity demonstrated 33 - 61 wt% NaCl equivalent. Mineralizing fluids density at the deposit was 0.8 - 1.2 g/cm3. Fluid inclusion studies suggested that Ali Javad deposit is an Au-rich porphyry copper deposit; its fluid inclusion features were comparable with other porphyry deposits.