Origin of palaeo-waters in the Ordovician carbonates in Tahe oilfield, Tarim Basin: constraints from fluid inclusions and Sr, C and O isotopes

Petrographic features, isotopes, and trace elements were determined, and fluid inclusions were analyzed on fracture-filling, karst-filling and interparticle calcite cement from the Ordovician carbonates in Tahe oilfield, Tarim basin, NW China. The aim was to assess the origin and evolution of palaeo-waters in the carbonates. The initial water was seawater diluted by meteoric water, as indicated by bright cathodoluminescence (CL) in low-temperature calcite. The palaeoseawater was further buried to temperatures from 57 to 110 degrees C, nonluminescent calcite precipitated during the Silurian to middle Devonian. Infiltration of meteoric water of late Devonian age into the carbonate rocks was recorded in the first generation of fracture- and karst-filling dull red CL calcite with temperatures from < 50 degrees C to 83 degrees C, low salinities (< 9.0 wt%), high Mn contents and high 86Sr/87Sr ratios from 0.7090 to 0.7099. During the early Permian, 87Sr-rich hydrothermal water may have entered the carbonate rocks, from which precipitated a second generation of fracture-filling and interparticle calcite and barite cements with salinities greater than 22.4 wt%, and temperatures from 120 degrees C to 180 degrees C. The hydrothermal water may have collected isotopically light CO2 (possibly of TSR-origin) during upward migration, resulting in hydrothermal calcite and the present-day oilfield water having delta 13C values from -4.3 to -13.8 parts per thousand and showing negative relationships of 87Sr/86Sr ratios to delta 13C and delta 18O values. However, higher temperatures (up to 187 degrees C) and much lower salinities (down to 0.5 wt%) measured from some karst-filling, giant, nonluminescent calcite crystals may suggest that hydrothermal water was deeply recycled, reduced (Fe-bearing) meteoric water heated in deeper strata, or water generated from TSR during hydrothermal water activity. Mixing of hydrothermal and local basinal water (or diagenetically altered connate water) with meteoric waters of late Permian age and/or later may have resulted in large variations in salinity of the present oilfield waters with the lowest salinity formation waters in the palaeohighs.