Skip to main content
Log in

Geochemistry on mantle-derived volatiles in natural gases from eastern China oil/gas provinces (I)

A novel helium resource—commercial accumulation of mantle-derived helium in the sedimentary crust

  • Published:
Science in China Series D: Earth Sciences Aims and scope Submit manuscript

Abstract

Commercial accumulation of mantle-derived helium in the sedimentary shell is discussed. Generally speaking, a commercial helium pool is formed by accumulated4He that comes from uranium and thorium via α-decay; therefore, it has a very low3He/4He value in the magnitude of 10-8. The helium concentration in some gas wells of eastern China oil/gas provinces is about or over 0.05% —0. 1%, consequently forming commercial helium wells (pools), such as the Wangjinta Gas Pool in Songliao Basin, Huangqiao Gas Pool in North Jiangsu Basin and some gas wells in Sanshui Basin. Studies have proved that when the3He/4He value of a helium gas pool is about 3.7 × 10-6 -7.2×10-6 namely mantle-derived helium in its total helium concentration accounts for 33.5%—65.4%, it is a crust-mantle dual-source or dominantly mantle-derived helium gas pool, which is a novel helium resource and its formation is mainly related to the distribution of megafractures.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Craig, H., Lupton, J. E., Primordial neon, helium and hydrogen in oceanic hasalts,Earth Planet Sci Tett, 1976, 31: 369.

    Article  Google Scholar 

  2. Craig, H., Lupton, J. E., Helium isotope variations,Trans Am Geophy Union, 1978, 58: 1194

    Google Scholar 

  3. Kaneoka, I., Takaoka, N., Noble gas state in the Earth’s interior—some constaints on the present state,Chemical Geology (Isotope Geoscience Section), 1985, 52: 75

    Article  Google Scholar 

  4. Lupton, J E., Terrestrial inert gases—isotopic trace studies and clues primordial components,Annual Review Earth Plant Science, 1983, 11:371

    Article  Google Scholar 

  5. Ozima, M., Podosek, F. A.,Noble Gas Geochemistry, Cambridge: Cambridge Univ Press, 1983

    Google Scholar 

  6. Xu Yongchang, Shen Ping, Tao Mingxinet al., A commercial accumulation of mantle-derived helium and the Tanlu megafracture zone,Chinese Science Bulletin, 1990, 35(12): 932

    Google Scholar 

  7. Qiu Songyu, Zhong Shiyou, Geological chararteristics of the Wanjinta CO2 gasfield in the southern Songliao Basin and its genesis,Oil & Gas Geology. 1985, 6(4) 434.

    Google Scholar 

  8. Tang Zhongyu, An approach to petrochemical characteristics of volcanism and volcanic rocks in the Sanshui basin,Marine Geology, 1987, (3): 50

  9. Poreda, R. J., Jenden, P. D., Kaplan, E. R.et al, Mantle helium in Sacramento Basin natural gas wells,Geochim Cosmochim Acta, 1986, 65(5): 2847.

    Article  Google Scholar 

  10. Sakata, S., Takahashi, M., Hoshino, K., Geochemical study on genesis of natural gases accumulated in deep valcaniclastic rocks,Journal of the Japanese Association for Petroleum Technology, 1986, 51(3): 32

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Xu, Y., Shen, P., Tao, M. et al. Geochemistry on mantle-derived volatiles in natural gases from eastern China oil/gas provinces (I). Sci. China Ser. D-Earth Sci. 40, 120–129 (1997). https://doi.org/10.1007/BF02878370

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02878370

Keywords

Navigation