THE CHARACTERISTICS OF PRIMARY INCLUSIONS IN HALITE AND ITS IMPLICATION FOR PALEO-TEMPERATURE IN WELL BT5, BACHU UPLIFT, TARIM BASIN

摘要

Halite is one of the most important minerals inrnevaporate deposits. The primary fluid inclusions inrnhalite can provide valuable information aboutrnpaleoclimate (Lowenstein et al., 1998; Benison andrnGoldstein, 1999; Meng et al., 2011; Meng et al.,rn2013). Because halite is easily to be dissolved andrnhence be altered due to its high solubility, thernhomogenization temperature of fluid inclusions inrnancient halite should be carefully evaluated then.