Abstract

The Lucaogou Formation in the Jimusar Sag of the eastern Junggar Basin is an important sedimentary stratum accumulating huge amounts of lacustrine tight oil in China, where organic-rich rocks are commonly observed. Focusing on the Lucaogou Formation, a precise analysis of the inorganic and organic petrology and the inorganic geochemistry characteristics was conducted. The paleoclimate and paleoenvironment during sedimentation of the Lucaogou Formation were established, and the key factors that were controlling the accumulation of organic matter during this time were identified. The results of this study suggest that during the sedimentation of the Lucaogou Formation, the paleoclimate periodically changed from a humid environment to an arid environment. As a result, the salinity of the water and the redox environment fluctuated. During the sedimentation period, the lake showed sufficient nutrient supplies and a high primary productivity. The interval studies in the Lucaogou Formation were divided into five sedimentary cycles, where the first, second, and fifth sedimentary cycles consisted of cyclical paleoclimate fluctuations varied from a humid environment to an arid environment and shifted back to a humid environment with levels of salinity from low to high and decreased again. The third and fourth cycles have cyclical fluctuations from a humid to an arid environment and corresponding salinity variation between low and high levels. During the period when organic-rich rocks in the Lucaogou Formation deposited in the Jimusar Sag, the paleoclimate and the water body were suitable for lower aquatic organisms to flourish. As a result, its paleoproductivity was high, especially during the early period of each cycle. A quiet deep water body is likely to form an anoxic environment at the bottom and is also good for accumulation and preservation of organisms. Fine-grained sediments were accumulated at a low deposition rate, with a low dilution of organic matter. Therefore, high paleoproductivity provided a sufficient volume of organisms in the studied area in a quiet deep water body with an anoxic environment and these were the key factors controlling formation of organic-rich rocks.

Highlights

  • The Junggar Basin is located in the north of the Xinjiang Uygur Autonomous Region of China and is one of the most important petroliferous basins with abundant oil, gas, and tight oil resources (Jia et al 2012a, b; Zou et al 2015a, b, 2016a, b)

  • While significant studies have been conducted to identify the key lithological features, reservoir properties, source rock, and the hydrocarbon generation potential (Kuang et al 2013; Wang et al 2014; Jiang et al 2015; Shao et al 2015; Xi et al 2015; Gao et al 2016; Zha et al 2017; Yang et al 2017), few studies have focused on the paleoenvironment, the paleoproductivity, or the other factors controlling the accumulation of organic matter

  • The paleoclimate during the sedimentation period of the Lucaogou Formation in the Jimusar Sag was dominated by frequent variations between a humid and an arid climate

Read more

Summary

Introduction

The Junggar Basin is located in the north of the Xinjiang Uygur Autonomous Region of China and is one of the most important petroliferous basins with abundant oil, gas, and tight oil resources (Jia et al 2012a, b; Zou et al 2015a, b, 2016a, b). While significant studies have been conducted to identify the key lithological features, reservoir properties, source rock, and the hydrocarbon generation potential (Kuang et al 2013; Wang et al 2014; Jiang et al 2015; Shao et al 2015; Xi et al 2015; Gao et al 2016; Zha et al 2017; Yang et al 2017), few studies have focused on the paleoenvironment, the paleoproductivity, or the other factors controlling the accumulation of organic matter. By identifying and reconstructing the paleoclimate and the paleoenvironment characteristics and their evolution over time, this study sought to identify the key factors controlling the accumulation of organic matter, reveal the distribution of high-quality source rock, and demonstrate the feasibility for tight oil exploration in the region

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call