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An enhanced understanding of the Basinal Bowland shale in Lancashire (UK), through microtextural and mineralogical observations

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Title: An enhanced understanding of the Basinal Bowland shale in Lancashire (UK), through microtextural and mineralogical observations
Authors: Fauchille, AL
Ma, L
Rutter, E
Chandler, M
Lee, PD
Taylor, KG
Item Type: Journal Article
Abstract: Variability in the Lower Bowland shale microstructure is investigated here, for the first time, from the centimetre to the micrometre scale using optical and scanning electron microscopy (OM, SEM), X-Ray Diffraction (XRD) and Total Organic Carbon content (TOC) measurements. A significant range of microtextures, organic-matter particles and fracture styles was observed in rocks of the Lower Bowland shale, together with the underlying Pendleside Limestone and Worston Shale formations encountered the Preese Hall-1 Borehole, Lancashire, UK. Four micro-texture types were identified: unlaminated quartz-rich mudstone; interlaminated quartz- and pyrite-rich mudstone; laminated quartz and pyrite-rich mudstone; and weakly-interlaminated calcite-rich mudstone. Organic matter particles are classified into four types depending on their size, shape and location: multi-micrometre particles with and without macropores: micrometre-size particles in cement and between clay minerals; multi-micrometre layers; and organic matter in large pores. Fractures are categorized into carbonate-sealed fractures; bitumen-bearing fractures; resin-filled fractures; and empty fractures. We propose that during thermal maturation, horizontal bitumen-fractures were formed by overpressuring, stress relaxation, compaction and erosional offloading, whereas vertical bitumen-bearing, resin-filled and empty fractures may have been influenced by weak vertical joints generated during the previous period of veining. For the majority of samples, the high TOC (>2 wt%), low clay content (<20 wt%), high proportion of quartz (>50 wt%) and the presence of a multi-scale fracture network support the increasing interest in the Bowland Shale as a potentially exploitable oil and gas source. The microtextural observations made in this study highlight preliminary evidence of fluid passage or circulation in the Bowland Shale sequence during burial.
Issue Date: 27-Jul-2017
Date of Acceptance: 25-Jul-2017
URI: http://hdl.handle.net/10044/1/53187
DOI: https://dx.doi.org/10.1016/j.marpetgeo.2017.07.030
ISSN: 0264-8172
Publisher: ELSEVIER SCI LTD
Start Page: 1374
End Page: 1390
Journal / Book Title: MARINE AND PETROLEUM GEOLOGY
Volume: 86
Copyright Statement: © 2017 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
Keywords: Science & Technology
Physical Sciences
Geosciences, Multidisciplinary
Geology
Bowland shale
Variability
Micro-texture
Organic matter
Fractures
Microscopy
Characterization
MISSISSIPPIAN BARNETT SHALE
NORTHEASTERN BRITISH-COLUMBIA
NORTH-CENTRAL TEXAS
FORT-WORTH BASIN
SEDIMENTARY BASINS
NATURAL FRACTURES
PENNINE BASIN
BLACK SHALES
GAS SYSTEMS
FLUID-FLOW
0403 Geology
0404 Geophysics
Publication Status: Published
Open Access location: http://dx.doi.org/10.1016/j.marpetgeo.2017.07.030
Appears in Collections:Materials