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An enhanced understanding of the Basinal Bowland shale in Lancashire (UK), through microtextural and mineralogical observations
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1-s2.0-S0264817217302854-main.pdf | Published version | 6.76 MB | Adobe PDF | View/Open |
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 |