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ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.
Citation: ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.

Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area

  • Received Date: 2013-07-05
  • Rev Recd Date: 2013-10-14
  • Publish Date: 2014-10-10
  • Considering the modifications of reservoir property in tectonic compression and volcanic hydrothermal transformation area, according to the outcrop and core data, the experimental analysis, and the well logging information, based on the theory of sandstone dynamic diagenesis, we bring forward this research on the effects of tectonic compression and volcanic hydrothermal transformation in marine sandstone reservoirs. It indicates that clastic particles in Yingmai 35 are obviously more compacted than those in Yingmai 34, the rock porosity is 7%~8% less than the latter. The tectonic compaction in early Hercynian and the volcanic hydrothermal transformation in the late Hercynian had improved the reservoir quality in Yingmai 35. The quartz sandstone reservoirs are obviously affected by the tectonic compression and volcanic hydrothermal transformation. The tectonic compression is controlled by the duration,structural pattern,and the original sedimentary fabric. The volcanic hydrotherm has a zonal influence on the sanstone reservoir quality, influencing area is within the half thickness of the volcanic intrusive, the widely distributed metamorphic mineral is the evidence of the destruction of the reservoir.
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  • Received:  2013-07-05
  • Revised:  2013-10-14
  • Published:  2014-10-10

Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area

Abstract: Considering the modifications of reservoir property in tectonic compression and volcanic hydrothermal transformation area, according to the outcrop and core data, the experimental analysis, and the well logging information, based on the theory of sandstone dynamic diagenesis, we bring forward this research on the effects of tectonic compression and volcanic hydrothermal transformation in marine sandstone reservoirs. It indicates that clastic particles in Yingmai 35 are obviously more compacted than those in Yingmai 34, the rock porosity is 7%~8% less than the latter. The tectonic compaction in early Hercynian and the volcanic hydrothermal transformation in the late Hercynian had improved the reservoir quality in Yingmai 35. The quartz sandstone reservoirs are obviously affected by the tectonic compression and volcanic hydrothermal transformation. The tectonic compression is controlled by the duration,structural pattern,and the original sedimentary fabric. The volcanic hydrotherm has a zonal influence on the sanstone reservoir quality, influencing area is within the half thickness of the volcanic intrusive, the widely distributed metamorphic mineral is the evidence of the destruction of the reservoir.

ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.
Citation: ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.
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