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Volume 29 Issue 3
Aug 2018
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Journal of Earth Science  > 2018  >  29(3): 629-638.
Longzhang Wang, Liyun Wang, Ping'an Peng, Tongmo Dai, Dayong Liu. A Thermal Event in the Ordos Basin: Insights from Illite 40Ar-39Ar Dating with Regression Analysis. Journal of Earth Science, 2018, 29(3): 629-638. doi: 10.1007/s12583-017-0903-7
Citation: Longzhang Wang, Liyun Wang, Ping'an Peng, Tongmo Dai, Dayong Liu. A Thermal Event in the Ordos Basin: Insights from Illite 40Ar-39Ar Dating with Regression Analysis. Journal of Earth Science, 2018, 29(3): 629-638. doi: 10.1007/s12583-017-0903-7
shu

A Thermal Event in the Ordos Basin: Insights from Illite 40Ar-39Ar Dating with Regression Analysis

doi: 10.1007/s12583-017-0903-7
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China

  • 2.

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

  • 3.

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

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  • Corresponding author: Longzhang Wang, longz_wang@cug.edu.cn
  • Received Date: 17 May 2016
  • Accepted Date: 01 Jan 2017
  • Publish Date: 01 Jun 2018
    Abstract
  • Four samples from a Permian reservoir in the Ordos Basin of North China were separated into twelve fractions in grain sizes of < 0.5, 0.5–1 and 1–2 μm. Using the 40Ar-39Ar step-heating method, all of the fractions essentially yielded plateau ages ranging from 172.5 to 217.1 Ma. These scattered plateau ages might not have been obtained from pure diagenetic illites but from mixed clay minerals, although the samples were disaggregated using a gentle freeze-thaw cycle to free them of non-clay minerals. A regional thermal event, as suggested by several proxies, led to intensive illitization as a distinct diagenetic process when the Yanshanian Movement triggered magmatism around the entire North China Block during the Jurassic to Cretaceous. Thermal illites formed during a short time period, whereas detrital illites came from various sources. The scattered plateau ages could have resulted from mixed degassing of thermal and detrital illites. Within one sample, the plateau ages decrease with the diminution of grain sizes, but it is difficult to extrapolate to the detrital-illite-free ages. Because the plateau age is a mixture of ages for thermal and detrital illites, this regression analysis studies the dependence of the plateau ages on the synthetic values of contents and ages of detrital illites instead of on the grain sizes. Comparing the samples to one another, the plateau ages show the same trend among the different grain sizes. Weighted by the contents and ages of detrital illites, linear regression analysis revealed the relationship between the plateau ages and the relative weight proportions. Based on iterated calculations, a thermal event age and a set of weight proportions were derived. The regressed thermal event age is 163.3±1.6 Ma, which coincides with regional thermal activities and links to gas accumulation.

     

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