Diffusive anisotropy in low-permeability Ordovician sedimentary rocks from the Michigan Basin in southwest Ontario

2013 ◽  
Vol 155 ◽  
pp. 31-45 ◽  
Author(s):  
Y. Xiang ◽  
T. Al ◽  
L. Scott ◽  
D. Loomer
2018 ◽  
Vol 92 ◽  
pp. 157-165 ◽  
Author(s):  
Cornelia Wigger ◽  
Laura Kennell-Morrison ◽  
Mark Jensen ◽  
Martin Glaus ◽  
Luc Van Loon

2017 ◽  
Vol 86 ◽  
pp. 121-137 ◽  
Author(s):  
D.C. Petts ◽  
J.K. Saso ◽  
L.W. Diamond ◽  
L. Aschwanden ◽  
T.A. Al ◽  
...  

2020 ◽  
Author(s):  
Robert H. Goldstein ◽  
◽  
Sahar Mohammadi ◽  
Andrew Michael Hollenbach

2021 ◽  
Author(s):  
Besmir Buranaj Hoxha ◽  
Claudio Rabe

Abstract Shale ‘stability’ has been extensively studied the past few decades in an attempt to understand wellbore instability problems encountered while drilling. Drilling through shale is almost inevitable, it makes up 75 percent of sedimentary rocks. Shale tends to be characterized as having high in-situ stresses, fissile, laminated, with low permeability. However, not all shale are the same, and the problem herein lies where they are all treated as such, in which most cases, has shown to be ineffective. Ironically, shale is predominantly generalized as being "reactive/swelling". Even though this can be true, it is not always the case because not all shale is reactive! In reality, there are many different types of shale: ductile, brittle, carbonaceous, argillaceous, flysch, dispersive, kaolinitic, micro-fractured etc. This study aims to clear many misconceptions and define different types of shale (global case scenarios) and their failing mechanisms that lead to wellbore instability, formation damage and high drilling cost. Afterwards, solutions will be offered, from a filed operation perspective, which will provide guidelines for stabilizing various shale based on their failure mechanism. Furthermore, we will define the symptoms for shale instability and propose industry accepted remedies.


2014 ◽  
Vol 509 ◽  
pp. 163-178 ◽  
Author(s):  
Richard L. Beauheim ◽  
Randall M. Roberts ◽  
John D. Avis

2019 ◽  
Vol 56 (3) ◽  
pp. 201-208 ◽  
Author(s):  
Laurianne Bouchard ◽  
Ján Veizer ◽  
Laura Kennell-Morrison ◽  
Mark Jensen ◽  
Ken G. Raven ◽  
...  

Porewater extractions and acid leachates of rock core from a 250 m thick sequence of low-permeability Ordovician-age shales and limestones, on the eastern flank of the Michigan Basin, were analysed for strontium isotope ratios in an attempt to infer porewater ages from observed 87Sr/86Sr enrichments. The porewaters originated as Ordovician seawater, which subsequently mixed with evaporated Silurian seawater infiltrating from above, and, to some extent, with a deep brine—with an enriched 87Sr/86Sr signature—from the underlying crystalline shield or deep basin. The porewater 87Sr/86Sr ratios are more radiogenic than contemporaneous seawater but show no obvious correlation to those leached from the solid rock phases. Accepting that the initial 87Sr/86Sr signatures in porewaters were dominated by Late Silurian brine, potentially with an additional deep brine component, the excess of radiogenic 87Sr appears to represent ingrowth from 87Rb decay over a time span of some 420 million years, approaching the depositional age of the rocks. Similarly, Rb/Sr errochron ages of acid leachates of solid phases, and the calculated initial 87Sr/86Sr isotopic ratios, are consistent with a proposition that the calcites inherited their Sr from Ordovician seawater and were dolomitized shortly afterwards by infiltrating Mg-enriched evaporative brine, indicating long-term conservative behaviour for the enclosing carbonate rocks. The errochron for leachates from (alumino)silicates yields a high initial 87Sr/86Sr, but with an errochron age of about 340 ± 48 Ma, likely owing to variable admixtures of diagenetic illite in the shales. Overall, the data provide evidence for a stable hydrologic regime since Paleozoic time.


2015 ◽  
Vol 404 ◽  
pp. 1-17 ◽  
Author(s):  
Tom A. Al ◽  
Ian D. Clark ◽  
Laura Kennell ◽  
Mark Jensen ◽  
Ken G. Raven

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