Volume 24 Issue 6
Dec.  2018
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SHEN Chonghui, ZHOU Xiaofeng, GUO Wei, 2018. ANALYSIS ON DENSIFICATION PROCESS OF CHANG 6 SANDSTONES IN WESTERN ORDOS BASIN. Journal of Geomechanics, 24 (6): 776-784. DOI: 10.12090/j.issn.1006-6616.2018.24.06.080
Citation: SHEN Chonghui, ZHOU Xiaofeng, GUO Wei, 2018. ANALYSIS ON DENSIFICATION PROCESS OF CHANG 6 SANDSTONES IN WESTERN ORDOS BASIN. Journal of Geomechanics, 24 (6): 776-784. DOI: 10.12090/j.issn.1006-6616.2018.24.06.080

ANALYSIS ON DENSIFICATION PROCESS OF CHANG 6 SANDSTONES IN WESTERN ORDOS BASIN

doi: 10.12090/j.issn.1006-6616.2018.24.06.080
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  • Received: 2017-12-28
  • Revised: 2018-03-21
  • Published: 2018-12-01
  • By core physical property, casting slice, scanning electron microscope analysis with energy disperse spectroscopy, the densification process of Chang 6 sandstones in western Ordos Basin was studied quantitatively. The study showed that the initial porosity and permeability of sandstones in the area were 39.3% and 22400×10-3 μm2 respectively, and its densification process was divided into two stages. In the course of early diagenesis stage, both calcite and chlorite coat cements and mechanical compaction caused the sandstones into ultra-low permeability reservoir whose porosity and permeability were 8.0% and 0.17×10-3 μm2 apart. During hydrocarbon accumulation in middle diagenesis stage A, hydrocarbon with organic acid came into this ultra-low permeability sandstones, and under organic acid circumstance feldspar dissolution formed secondary pore, which made porosity and permeability up to 11.6% and 0.61×10-3 μm2 individually. So the relationship between the densification process of Chang 6 sandstone and hydrocarbon accumulation is first densification then accumulation and accumulation with increased porosity and permeability.

     

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