Geochemical Characteristics of Carbonates and Indicative Significance of the Sedimentary Environment Based on Carbon–Oxygen Isotopes and Trace Elements: Case Study of the Lower Ordovician Qiulitage Formation in Keping Area, Tarim Basin (NW China)

Abstract

The carbonate rock of the Qiulitage Formation is a significant stratum for oil and gas exploration in the Tarim Basin. To elucidate its environmental characteristics, we conducted tests and analyses of trace elements, carbon, and oxygen isotopes of the carbonate rocks of the Qiulitage Formation in the Kekeqigankake section of the Keping area. The results reveal that δ13C values range between −1.7‰ and 4.3‰, with an average value of 1.645‰. δ18O values fluctuate from −11.4‰ to −6‰, with an average value of −8.2475‰. Z values (paleosalinity) vary from 120.33 to 131.67, significantly exceeding 120 with an average value of 126.52, indicating a marine sedimentary environment. Paleotemperature values (T) range from 12.75 to 29.09 °C, with an average value of 21.36 °C, suggesting warm climate conditions. The Sr/Ba (3.42~24.39) and Sr/Cu (57.5~560) ratios are elevated, while Th/U (<1.32) and V/Cr (0.989~1.70) ratios are reduced, suggesting that the Qiulitage Formation was deposited in an oxygen-rich, warm marine sedimentary environment with relatively high salinity.

Keywords

• Tarim Basin
• Qiulitage Formation
• carbon and oxygen isotopes
• trace element
• sedimentary environment