Diagenesis and reservoir quality of Rotliegend sandstones in the northern Netherlands—A Review

2011 ◽  
pp. 193-226 ◽  
Author(s):  
REINHARD GAUPP ◽  
JOS A. OKKERMAN
Keyword(s):  
Reservoir Quality

Effects of igneous intrusions on diagenesis and reservoir quality of sandstone in the Songliao Basin, China

2021 ◽  
Vol 127 ◽  
pp. 104980
Author(s):  
Hui Rong ◽  
Yangquan Jiao ◽  
Liqun Wu ◽  
Xinfu Zhao ◽  
Minqiang Cao ◽  
...  
Keyword(s):  
Songliao Basin ◽  
Reservoir Quality ◽  
Igneous Intrusions

Factors Controlling Reservoir Quality of a Paleozoic Tight Sandstone, Rub’ al Khali Basin, Saudi Arabia

2019 ◽  
Vol 44 (7) ◽  
pp. 6489-6507 ◽  
Author(s):  
Abdullah Alqubalee ◽  
Lameed Babalola ◽  
Osman Abdullatif ◽  
Mohammed Makkawi
Keyword(s):  
Saudi Arabia ◽  
Reservoir Quality ◽  
Tight Sandstone

scholarly journals The role played by carbonate cementation in controlling reservoir quality of the Triassic Skagerrak Formation, Norway

2017 ◽  
Vol 85 ◽  
pp. 316-331 ◽  
Author(s):  
Yufeng Cui ◽  
Stuart J. Jones ◽  
Christopher Saville ◽  
Stephan Stricker ◽  
Guiwen Wang ◽  
...  
Keyword(s):  
Reservoir Quality ◽  
Carbonate Cementation

Depositional facies, diagenetic clay minerals and reservoir quality of Rotliegend sediments in the Southern Permian Basin (North Sea): a review

Clay Minerals ◽  
1982 ◽  
Vol 17 (1) ◽  
pp. 55-67 ◽  
Author(s):  
U. Seemann
Keyword(s):  
Clay Minerals ◽  
North Sea ◽  
Effective Porosity ◽  
Hydrocarbon Exploration ◽  
Reservoir Quality ◽  
Burial Diagenesis ◽  
Permian Basin ◽  
Northern Margin ◽  
The North

AbstractThe Southern Permian Basin of the North Sea represents an elongate E-W oriented depo-centre along the northern margin of the Variscan Mountains. During Rotliegend times, three roughly parallel facies belts of a Permian desert developed, these following the outline of the Variscan Mountains. These belts were, from south to north, the wadi facies, the dune and interdune facies, and the sabkha and desert lake facies. The bulk of the gas reservoirs of the Rotliegend occur in the aeolian dune sands. Their recognition, and the study of their geometry, is therefore important in hydrocarbon exploration. Equally important is the understanding of diagenesis, particularly of the diageneticaily-formed clay minerals, because they have an important influence on the reservoir quality of these sands. Clay minerals were introduced to the aeolian sands during or shortly after their deposition in the form of air-borne dust, which later formed thin clay films around the grains. During burial diagenesis, these clay films may have acted as crystallization nuclei for new clay minerals or for the transformation of existing ones. Depending on their crystallographic habit, the clay minerals can seriously affect the effective porosity and permeability of the sands.

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