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Nicholas B. Harris

Researcher at University of Alberta

Publications -  72
Citations -  2484

Nicholas B. Harris is an academic researcher from University of Alberta. The author has contributed to research in topics: Oil shale & Carbonate. The author has an hindex of 25, co-authored 65 publications receiving 1958 citations. Previous affiliations of Nicholas B. Harris include Colorado School of Mines & ConocoPhillips.

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Geochemical facies analysis of fine-grained siliciclastics using Th/U, Zr/Rb and (Zr+Rb)/Sr ratios

TL;DR: In this article, the trace elements Zr, Rb, Sr, Th and U were used as indicators of the redox conditions of fine-grained siliciclastic sediments.
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The character and origin of lacustrine source rocks in the Lower Cretaceous synrift section, Congo Basin, west Africa

TL;DR: In this article, a lower Cretaceous synrift synrift lacustrine shales from the Congo Basin, west Africa, have been analyzed with sedimentological and geochemical techniques to characterize source rock quality and identify triggers for deposition of intervals richest in organic carbon.
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Porosity characteristics of the Devonian Horn River shale, Canada: Insights from lithofacies classification and shale composition

TL;DR: In this article, the pore systems of the Horn River shale in Western Canada Sedimentary Basin from core samples to micro-scale pore structure investigation were evaluated by core description, porosity measurement, SEM, and TEM imaging of ion milled samples, and nitrogen adsorption analysis.
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Secular variation in the major-ion chemistry of seawater: Evidence from fluid inclusions in Cretaceous halites

TL;DR: The major-ion chemistry of Cretaceous seawater was determined from analyses of seawater-derived brines preserved as fluid inclusions in marine halites using the environmental scanning electron microscopy (ESEM) X-ray energy dispersive spectrometry (EDS) technique as discussed by the authors.
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Diagenesis of a tight gas sand reservoir: Upper Cretaceous Mesaverde Group, Piceance Basin, Colorado

TL;DR: The Upper Cretaceous Mesaverde Group in the Piceance Basin, western Colorado, contains thick sections of low porosity, low permeability sandstones that are reservoirs for large accumulations of hydrocarbon gas as discussed by the authors.