Kilometer-scale fault-related thermal anomalies in tight gas sandstones. (September 2017)

• Record Type: Journal Article
• Authors: Wüstefeld, Patrick; Hilse, Ulrike; Lüders, Volker; Wemmer, Klaus; Koehrer, Bastian; Hilgers, Christoph
• Is Part Of: Marine and petroleum geology. Volume 86(2017)
• Page Start: 288
• Page End: 303
• Publication Date: 2017-09
• Subjects: Thermal anomaly -- Diagenesis -- Geothermometers -- Stable isotopes -- Reservoir outcrop analog -- Upper Carboniferous -- Lower Saxony Basin -- Tight gas sands; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2017.05.015
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: Upper Carboniferous sandstones make one of the most important tight gas reservoirs in Central Europe. This study integrates a variety of geothermometers (chlorite thermometry, fluid inclusion microthermometry and vitrinite reflection measurements) to characterize a thermal anomaly in a reservoir outcrop analog (Piesberg quarry, Lower Saxony Basin), which is assumed responsible for high temperatures of circa 300 °C, deteriorating reservoir quality entirely. The tight gas siliciclastics were overprinted with temperatures approximately 90–120 °C higher compared to outcropping rocks of a similar stratigraphic position some 15 km to the west. The local temperature increase can be explained by circulating hydrothermal fluids along the fault damage zone of a large NNW-SSE striking fault with a displacement of up to 600 m in the east of the quarry, laterally heating up the entire exposed tight gas sandstones. The km-scale lateral extent of this fault-bound thermal anomaly is evidenced by vitrinite reflectance measurements of meta-anthracite coals (VRrot ∼ 4.66) and the temperature-related diagenetic overprint. Data suggest that this thermal event and the associated highest coalification was reached prior to peak subsidence during Late Jurassic rifting (162 Ma) based on K-Ar dating of the <2 μm fraction of the tight gas sandstones. Associated stable isotope data from fluid inclusions, hosted in a first fracture filling quartz generation (T ∼ 250 °C) close to lithostatic fluid pressure (P ∼ 1000 bars), together with authigenic chlorite growth in mineralized extension fractures, demonstrate that coalification was not subject to significant changes during ongoing burial. This is further evidenced by the biaxial reflectance anisotropy of meta-anthracite coals. A second event of quartz vein formation occurred at lower temperatures (T ∼ 180 °C) and lower (hydrostatic) pressure conditions (P ∼ 400 bars) and can be related to basin inversion. This second quartz generation might be associated with a second event of illite growth and K-Ar ages of 96.5–106.7 Ma derived from the <0.2 μm fraction of the tight gas sandstones. This study demonstrates the exploration risk of fault-bound thermal anomalies by deteriorating entirely the reservoir quality of tight gas sandstones with respect to porosity and permeability due to the cementation with temperature-related authigenic cements. It documents that peak temperatures are not necessarily associated with peak subsidence. Consequently, these phenomena need to be considered in petroleum system models to avoid, for example, overestimates of burial depth and reservoir quality. Highlights: Kilometer-scale high-temperature overprint (about 300 °C) of reservoir sandstones. The thermal anomaly is the result of hydrothermal fluids circulating along a large fault system. Exploration risk of fault-related thermal anomalies laterally heating up tight gas sandstones. Peak temperatures do not necessarily imply peak subsidence. Local thermal anomalies need to be incorporated in the modeling of petroleum systems and reservoir quality prediction.