Thanks to SEM technician Peter Chung at the University of Glasgow, David Wilde and Peter Greatbatch at Keele University for careful thin section preparation, Chris Wibberley and Tom Blenkinsop for input and Kieran Keith from Harlaw Academy, Aberdeen for help collecting petrophysical data. Thanks to Fabrizio Storti, Michael Heap and Toru Takeshita for helping to improve this paper with their constructive reviews. This work forms part of a NERC Standard award for DH (NE/N003063/1), which is gratefully acknowledged.Peer reviewedPublisher PD
The authors would like to thank Anasuria Operating Company Ltd (AOC) for making available the rock s...
From Wiley via Jisc Publications RouterHistory: received 2021-06-21, rev-recd 2021-09-27, accepted 2...
In carbonates, the petrophysical interpretation is strongly controlled by the porosity exponent used...
AbstractStudies of fault rock permeabilities advance the understanding of fluid migration patterns a...
The goal of rock fabric characterization is to describe the spatial and geometric distribution of po...
This research was supported by STFC grant ST/I506102/1. DRN undertook measurements for a project con...
This research forms part of a PhD project supported by the Australian Research Council [Discovery Pr...
Systems of faults and joints are observed to span many scales of length and displacement. Spacing an...
Small-scale probe permeability measurements on differently oriented faces of highly compacted and qu...
We would like to express our gratitude to Dr Mehmet Kartal and Professor Dubravka Pokrajac for their...
Although the general influence of rock fabric on porosity and permeability (Φ-k) within carbonates i...
This paper presents a detailed description and evaluation of a multi-methodological petrophysical ap...
The fluvial-aeolian Upper Rotliegend sandstones from the Bebertal outcrop (Flechtingen High, Germany...
Deformation bands are the primary structural element of fault damage zones within porous granular ro...
We determined the structure and permeability variations of a 4 km-long normal fault by integrating s...
The authors would like to thank Anasuria Operating Company Ltd (AOC) for making available the rock s...
From Wiley via Jisc Publications RouterHistory: received 2021-06-21, rev-recd 2021-09-27, accepted 2...
In carbonates, the petrophysical interpretation is strongly controlled by the porosity exponent used...
AbstractStudies of fault rock permeabilities advance the understanding of fluid migration patterns a...
The goal of rock fabric characterization is to describe the spatial and geometric distribution of po...
This research was supported by STFC grant ST/I506102/1. DRN undertook measurements for a project con...
This research forms part of a PhD project supported by the Australian Research Council [Discovery Pr...
Systems of faults and joints are observed to span many scales of length and displacement. Spacing an...
Small-scale probe permeability measurements on differently oriented faces of highly compacted and qu...
We would like to express our gratitude to Dr Mehmet Kartal and Professor Dubravka Pokrajac for their...
Although the general influence of rock fabric on porosity and permeability (Φ-k) within carbonates i...
This paper presents a detailed description and evaluation of a multi-methodological petrophysical ap...
The fluvial-aeolian Upper Rotliegend sandstones from the Bebertal outcrop (Flechtingen High, Germany...
Deformation bands are the primary structural element of fault damage zones within porous granular ro...
We determined the structure and permeability variations of a 4 km-long normal fault by integrating s...
The authors would like to thank Anasuria Operating Company Ltd (AOC) for making available the rock s...
From Wiley via Jisc Publications RouterHistory: received 2021-06-21, rev-recd 2021-09-27, accepted 2...
In carbonates, the petrophysical interpretation is strongly controlled by the porosity exponent used...