Amorphous silica and its effects on shale reservoir: A case study about Yanchang formation lacustrine shale, Ordos Basin

ABSTRACT

The content of amorphous silica in Yanchang formation shale ranges from 1.48% to 19.89%, with an average of 11.77%. The Chang 7–3 submember (the submember 3 of the seventh member of Upper Triassic Yanchang formation) shale contains much larger content of amorphous silica. Amorphous silica appears as opal rim closely adjacent to detrital quartz, cement among clay minerals, and cement aside detrital minerals. Silica originates from clay mineral transformation and pressure solution of detrital quartz. Mineral composition, growth space, and overpressure affect the content of amorphous silica. Amorphous silica reduces the brittleness of shale reservoir, decreases the density of Chang 7–3 submember shale, and causes an increase in AC values for Chang 7–3 submember shale.

KEYWORDS:

• Amorphous SiO₂
• lacustrine shale
• ordos basin
• QEMSCAN
• quantitative calculation

Additional information

Funding

Our research was supported by the National Natural Science Foundation of China (No. 41272156 and No. 41472125), the Natural Science Foundation of Shanxi Province, China (2017JQ4004) and the National Science and Technology Major Project of the Ministry of Science and Technology of China (2016ZX05034);the National Natural Science Foundation of China [41272156,41472125];the National Science and Technology Major Project of the Ministry of Science and Technology of China [2016ZX05034];the Natural Science Foundation of Shanxi Province, China [2017JQ4004];