Can One-Run-Fixed-Arrhenius Kerogen Analysis Provide Comparable Organofacies Results to Detailed Palynological Analysis? A Case Study from a Prospective Mississippian Source Rock Reservoir (Bowland Shale, UK)

Newport, Sarah M.; Hennissen, Jan A.I.; Armstrong, James P.; Taylor, Kevin G.; Newport, Leo P.; Hough, Edward. 2020 Can One-Run-Fixed-Arrhenius Kerogen Analysis Provide Comparable Organofacies Results to Detailed Palynological Analysis? A Case Study from a Prospective Mississippian Source Rock Reservoir (Bowland Shale, UK). Natural Resources Research, 29 (3). 2011-2031. https://doi.org/10.1007/s11053-019-09543-z

Before downloading, please read NORA policies.

Preview

Text (Open Access Paper)
Newport2020_Article_CanOne-Run-Fixed-ArrheniusKero.pdf - Published Version
Available under License Creative Commons Attribution 4.0.
Download (1MB) | Preview

Official URL: http://dx.doi.org/10.1007/s11053-019-09543-z

Abstract/Summary

Organofacies analysis, a fundamental component within source rock appraisal based on the study of kerogen within a source rock, is typically produced from microscopy (palynological) and geochemical (kerogen kinetic) data, both of which are costly to acquire. One-Run-Fixed-Arrhenius (ORFA) kerogen kinetic analysis based on Rock–Eval pyrolysis offers a substantially cheaper kinetic dataset. Here, ORFA and palynological analyses are compared in organofacies characterization of a prospective Mississippian source rock reservoir (Bowland Shale, UK). Two-end-member organofacies were determined based on the abundance of the 56 kcal/mol activation energy peak derived from ORFA data: absence (< 5%) indicating ‘organofacies A’ containing the highest proportion of algal material (Type I kerogen); and presence (> 15%) indicating ‘organofacies B’ containing the highest proportion of sporomorphs (Type II kerogen). A mud-dominated slope setting for the rock reservoir was also used to test the accuracy of organofacies analysis in determining depositional environment. Organofacies A found within lithofacies deposited from dilute waning density flows and hemipelagic suspension settling occurred between shelf edge, slope and basin. Organofacies B found within lithofacies deposited from dilute waning density flows, and low-strength cohesive debrites occurred only within the lower slope. This study demonstrates that ORFA kerogen kinetic analysis provides comparable net results to palynological analysis, enabling cheaper and faster organic characterization during initial source rock appraisal. However, caution must be exercised in drawing interpretations as to biological source(s), organic matter mixing and preservation state(s) without additional investigation using data from detailed palynological analysis.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1007/s11053-019-09543-z
ISSN:	1520-7439
Date made live:	09 Jul 2020 13:54 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/528133

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1007/s11053-019-09543-z

ISSN:

1520-7439

Date made live:

09 Jul 2020 13:54 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/528133