Diagenesis and controls on reservoir quality of Lower Triassic red bed sandstones (Buntsandstein) from a marginal basin facies, southwest Germany

被引:9
|
作者
Quandt, Dennis [1 ]
Schmidt, Benjamin Busch Christina [1 ]
Schmidt, Christina [1 ,2 ]
机构
[1] KIT Karlsruhe Inst Technol, Inst Appl Geosci Struct Geol & Tecton, Campus South,Adenauerring 20A, D-76131 Karlsruhe, Germany
[2] GeoThermal Engn GmbH GeoT, An Der RaumFabr 33C, D-76227 Karlsruhe, Germany
关键词
Buntsandstein; Red bed; Porosity; Permeability; Reservoir quality; Diagenesis; UPPER RHINE GRABEN; JURASSIC NAVAJO SANDSTONE; GRAIN SIZE RELATIONS; LOWER SAXONY BASIN; ROTLIEGEND SANDSTONES; FLUVIAL SEDIMENTATION; DEPOSITIONAL FACIES; CLASTIC SEDIMENTS; CENTRAL-EUROPE; GARN FORMATION;
D O I
10.1016/j.marpetgeo.2022.105744
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
After decades of hydrocarbon exploration and production in the Lower Triassic Buntsandstein from the Central European Basin center, the marginal southern German Buntsandstein has gained interest as a potential lithology for geothermal applications and lithium brine extractions. For this purpose and in order to better understand reservoir quality, porosity and permeability in combination with point-counted petrographic data of sandstones from SW Germany covering the Lower, Middle, and Upper Buntsandstein are studied. Textural, mineralogical, and petrophysical data show that the eolian and fluvial sandstones represent a heterogeneous reservoir system. Permeabilities vary over six orders of magnitude from 0.001 to 515 mD, while porosities are in the range of 7.9-21.5%. Different controls on reservoir quality exist. Large grain sizes >= 0.31 mm together with total quartz contents are the major controls on reservoir quality. Additional controls on reservoir quality are exerted by authigenic phases. Since porosity loss is dominated by compaction, the influence of authigenic clay phases on reservoir quality is minor. However, illite coatings on detrital quartz efficiently inhibited syntaxial quartz overgrowth. Where illite coatings lack, syntaxial quartz overgrowths locally stabilized the granular framework and, thus, preserved primary porosity. These authigenic phases, however, represent a local control, which cannot be applied on a regional scale. Similarly, enhanced secondary porosity due to feldspar dissolution is locally restricted and minor. The comparison with other studies on the Buntsandstein shows that its reservoir system is highly heterogeneous over small and large scales and within the same stratigraphic levels. In this study, quartz rich and authigenic clay-poor sandstones with relative large grain sizes interpreted as eolian deposits reveal the best reservoir qualities.
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页数:17
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