Furthermore, volcanic deposits, such as tuff, ordinally exist in Miocene formations in Taiwan. Deformation bands behave like barriers of fluid flow in host rock because of their characteristics of low porosity and conductivity. Thus, documenting their existence and features in ignimbrites at Shihtiping is fairly important for the industrials of oil exploration and CO2 capture and storage in Taiwan.
|Effective start/end date||1/08/15 → 31/07/16|
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