Characteristics of Jurassic Source Rocks and Evaluation of Hydrocarbon Resources in Tarim Basin, western China

Authors

  • Shiqin Liang
  • Yuhang Wang
  • Yanbo Guo

DOI:

https://doi.org/10.62051/ijnres.v2n2.09

Keywords:

Tarim Basin; Jurassic; Hydrocarbon source rocks; Hydrocarbon accumulation.

Abstract

Jurassic strata in Tarim are significant for their hydrocarbon-rich content. However, the distribution of hydrocarbon source rocks in this region is uneven, and the conditions for hydrocarbon accumulation vary significantly among the different structural elements. Therefore, it is essential to investigate the distribution of Jurassic source rocks, the evolution history of hydrocarbon generation, and the mechanisms influencing hydrocarbon accumulation for effective hydrocarbon exploration and development. To achieve this, seismic, geologic, drilling, logging, and testing data were integrated to analyze the distribution and quality of hydrocarbon source rocks, the evolution of hydrocarbon generation, and the factors influencing hydrocarbon accumulation in Jurassic hydrocarbon source rocks in Tarim Basin. The study revealed that the Jurassic effective hydrocarbon source rock centers are mainly located in the piedmont areas of Kuqa depression, southwest depression, and southeast depression, as well as Yingjisu sag and Manjiaer sag in the eastern Tarim area. Based on a comprehensive evaluation and comparison of the potential of Jurassic hydrocarbon potential in each secondary structural unit, it is concluded that Kuqa Depression has the most favorable exploration zone due to its excellent hydrocarbon accumulation conditions and abundant hydrocarbon resources. Although the overall exploration potential of the southwest depression is lower than that of the Kuqa depression, the hydrocarbon resources potential of the piedmont thrust belt and the associated depression is very high. Similarly, the eastern part of the Manjiaer sag and the Altun piedmont zone of the southeastern depression still have promising exploration prospects, although the overall exploration potential of the eastern Tarim area and the southeastern depression is not as good as the former two.

References

DAI J D J, ZOU C Z C, LI J L J, et al. Carbon isotopes of Middle-Lower Jurassic coal-derived alkane gases from the major basins of northwestern China(Article)[J]. International Journal of Coal Geology, 2009, No.2): 124-134.

GONG D G D, WANG Z W Z, LIU G L G, et al. Re‐Examination of the Oil and Gas Origins in the Kekeya Gas Condensate Field, Northwest China–A Case Study of Hydrocarbon‐Source Correlation Using Sophisticated Geochemical Methods[J]. Acta Geologica Sinica ‐ English Edition, 2017, No.1): 186-203.

JIA C J C, LI Q L Q. Petroleum geology of Kela-2, the most productive gas field in China.[J]. Marine and Petroleum Geology, 2008, No.4-5): 335-343.

XIAO X X X, HU Z H Z, JIN Y J Y, et al. Hydrocarbon source rocks and generation history in the Lunnan oilfield area, northern Tarim Basin (NW China).[J]. Journal of Petroleum Geology, 2006, No.3): 319-333.

ZHAO W, ZHANG S, WANG F, et al. Gas accumulation from oil cracking in the eastern Tarim Basin: A case study of the YN2 gas field[J]. Organic Geochemistry, 2005, No.12): 1602-1616.

ZHU G Z G, WANG H W H, WENG N W N, et al. Geochemistry, origin and accumulation of continental condensate inthe ultra-deep-buried Cretaceous sandstone reservoir, Kuqa Depression, Tarim Basin, China(Article)[J]. Marine and Petroleum Geology, 2015, 103-113.

MA W A, HAN W A V Q, HOU L A, et al. Geochemical characteristics, genetic types and sources of natural gas in the Yingjisu Depression, Tarim Basin, China.[J]. International Journal of Coal Geology, 2019, 103300.

YANG P, WU G, REN Z, et al. Tectono-thermal evolution of Cambrian–Ordovician source rocks and implications for hydrocarbon generation in the eastern Tarim Basin, NW China[J]. Journal of Asian Earth Sciences, 2020, 2020,

ZHANG Z Z Z, ZHANG Y Z Y, ZHU G Z G, et al. Geochemical and Isotopic Evidence of the Genesis of a Condensate in the Eastern Tarim Basin, China: Implications for Petroleum Exploration[J]. ENERGY & FUELS, 2019, No.6): 4849-4856.

WANG T, JIN Z, LI H, et al. Processes and causes of Phanerozoic tectonic evolution of the western Tarim Basin, northwest China.[J]. Petroleum Science, 2020, No.2): 279-291.

FANG A F A, MA J M J, WANG S W S, et al. Sedimentary tectonic evolution of the southwestern Tarim Basin and west Kunlun orogen since Late Paleozoic[J]. ACTA PETROLOGICA SINICA, 2009, No.12): 3396-3406.

YI S, LI M, FAN T, et al. [Exploration directions on the Kelasu and East-Qiulitag fault hanging walls, Kuqa Depression, Tarim Basin][J]. Oil and Gas Geology, 2021, No.2): 309-324.

JIANG Z J Z, HUANG S H S, DU H D H, et al. The characteristics of the neotectonic movement and their effects on the formation of gas reservoirs in the marginal depressions of Tarim basin, NW China(Article)[J]. Journal of Natural Gas Science and Engineering, 2015, 503-514.

LIN C L C, LI H L H, LIU J L J. Major unconformities, tectonostratigraphic frameword, and evolution of the superimposed Tarim basin, Northwest China(Article)[J]. Journal of Earth Science, 2012, No.4): 395-407.

ZHAO Z. Stratum of Tarim Basin. 1997,

LI Z L Z, SONG W S W, PENG S P S, et al. Mesozoic–Cenozoic tectonic relationships between the Kuqa subbasin and Tian Shan, northwest China: constraints from depositional records.[J]. Sedimentary Geology, 2004, No.3-4): 223-249.

JIA C, ZHANG H, WU S. Tarim Basin and its surrounding strata. Volume I, summary of strata in each period. 2004,

Downloads

Published

29-04-2024

Issue

Section

Articles

How to Cite

Liang, S., Wang, Y., & Guo, Y. (2024). Characteristics of Jurassic Source Rocks and Evaluation of Hydrocarbon Resources in Tarim Basin, western China. International Journal of Natural Resources and Environmental Studies, 2(2), 79-85. https://doi.org/10.62051/ijnres.v2n2.09