Unconventional Resources Technology Conference, Denver, Colorado, 12-14 August 2013 2013
DOI: 10.1190/urtec2013-123
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Expanding the Application of Chemostratigraphy within Cretaceous Mudrocks: Estimating Total Organic Carbon and Paleoredox Facies using Major, Minor and Trace Element Geochemistry

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Cited by 7 publications
(3 citation statements)
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“…In recent years XRF, specifically its ability to differentiate numerous major and minor elements, has been used as a chemostratigraphic tool to predict TOC, paleoredox conditions, and overall stratigraphic "sweet spots" attributed to well deliverability (Rowe et al, 2009, Tinnin et al, 2013, Hashmy et al, 2012, Harbor, 2011. Under a similar methodology employed by Tinnin et al (2013), key redox sensitive trace elements were correlated against core and log derived reservoir parameters including: TOC, porosity, mineralogy, gas chemistry (gas wetness), and SRA outputs (HI,OI,S1, S1/TOC, and S2).…”
Section: Reservoir Characterizationmentioning
confidence: 99%
See 1 more Smart Citation
“…In recent years XRF, specifically its ability to differentiate numerous major and minor elements, has been used as a chemostratigraphic tool to predict TOC, paleoredox conditions, and overall stratigraphic "sweet spots" attributed to well deliverability (Rowe et al, 2009, Tinnin et al, 2013, Hashmy et al, 2012, Harbor, 2011. Under a similar methodology employed by Tinnin et al (2013), key redox sensitive trace elements were correlated against core and log derived reservoir parameters including: TOC, porosity, mineralogy, gas chemistry (gas wetness), and SRA outputs (HI,OI,S1, S1/TOC, and S2).…”
Section: Reservoir Characterizationmentioning
confidence: 99%
“…Under a similar methodology employed by Tinnin et al (2013), key redox sensitive trace elements were correlated against core and log derived reservoir parameters including: TOC, porosity, mineralogy, gas chemistry (gas wetness), and SRA outputs (HI,OI,S1, S1/TOC, and S2). Overall enrichment of V, Ni, Mo, and Zn are observed in the upper section of the Lower Eagle Ford, with Cu and Cr enrichment in the lower section of the Lower Eagle Ford (Figure 6).…”
Section: Reservoir Characterizationmentioning
confidence: 99%
“…In fluvial settings, the elemental data are typically used to recognize changes in paleoclimate (Pearce et al 2005, changes in sedimentary facies, and changes in sediment provenance (Ehrenberg and Siring 1992, Armstrong-Altrin et al 2004, Pe-Piper et al 2008, Hildred et al 2010, Ramkumar et al 2011. In shale resource plays, the elemental data are commonly used to recognize terrigenous material influx and content (Algeo et al 2004, Soua 2010, ver Straeten et al 2011, Whalen et al 2015 and as a proxy for bottom water conditions during deposition (Tribovillard et al 2006, Rowe et al 2012, Tinnin et al 2013). These changes are then used to build a stratigraphic framework and provide stratigraphic correlations.…”
Section: Introductionmentioning
confidence: 99%