| 摘要 |
<p>Methods for quantifying a hydrothermal impact on a stratigraphic unit are disclosed herein. In particular, the described methods may be used to quantify hydrothermal anomalies of a stratigraphic unit of a geological reservoir, where porosity reduction in the stratigraphic unit would have been accelerated some point or points in the past. Embodiments of the method generally comprise (a) receiving first data indicative of a reservoir temperature associated with the stratigraphic unit, (b) receiving second data indicative of estimates of the trapping temperatures associated with a plurality of fluid inclusions in a sample of the stratigraphic unit, (c) generating comparison data indicative of a comparison between the first data and the second data, and (d) generating based on the comparison data an impact parameter indicative of a hydrothermal impact on the stratigraphic unit.</p> |
