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The geology and geochemistry of the North Fork stock, northeastern OregonMatty, David Joseph 01 January 1979 (has links)
The North Fork stock is a composite intrusive body of Late Jurassic-Early Cretaceous age which outcrops in the Blue Mountains of northeastern Oregon. The upper 600 m of the intrusion are exposed over an area of approximately 36 km squared along the canyon walls of the North Fork of the John Day River in Grant and Umatilla counties. The stock intrudes metasediments, metavolcanics, and metagabbros associated with the Permian-Triassic Elkhorn Ridge Argillite. Contact metamorphism of the Elkhorn Ridge Argillite is developed to the hornblende-hornfels facies throughout most of the exposed area of this unit in the study area. The contact aureole of the North Fork stock extends away from the intrusive margins and ultimately grades into regionally metamorphosed greenschist- and amphibolite facies rocks. The metamorphic rocks exhibit a pronounced regional trend of foliation which is disrupted where it intersects intrusive contacts at steep angles.
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Removal of Select Chlorinated Hydrocarbons by Nanoscale Zero-valent Iron Supported on Powdered Activated CharcoalChowdhury, Md Abu Raihan 06 June 2017 (has links)
No description available.
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573 |
The Fate of Nutrients in Streams Affected by Acid Mine DrainageMaj, Sarah K. 21 September 2016 (has links)
No description available.
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574 |
Geochronology, geochemistry, and petrogenesis of basaltic rocks from the Western Cascades, Oregon /Lux, Daniel R. January 1981 (has links)
No description available.
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Major and Trace Elements Associated with Kerogen in the Eagle Ford ShaleVanHazebroeck, Ethan J. 03 February 2016 (has links)
<p> Despite an increased interest in exploitation of hydrocarbon source rock resource plays, there remains an incomplete understanding of organic and inorganic component interaction within source rocks. Few studies have been conducted concerning the associations between organic and inorganic geochemistry for the purposes of understanding kerogen type, thermal maturity influence, and paleoredox setting. This investigation’s goal was evaluating these relationships with samples from the Eagle Ford Formation using organic data, obtained by Rock-Eval pyrolysis and oxidation, and inorganic data, obtained using high-temperature and pressure leaching experiments. The study additionally tested various parameters for whole rock batch leaching, including time, temperature of leaching, and use of acids. The most successful leaching technique was applied to samples that (1) had first been subjected to Rock-Eval pyrolysis, at three different maximum temperatures (450°C, 550°C, and 650°C), as well as (2) samples that had not been subjected to pyrolysis. As different kerogen fractions were destroyed at these different temperatures, variances in elemental concentrations leached from these samples could be attributed, at least partially, to these fractions. Using this approach, the lower molecular weight kerogen fraction contained most of the elements likely attributable to carbonates and sulfides associated with the kerogen (e.g., Ca, Mg, Mn, Mo, P, S, Sr, Zn). The higher molecular weight portion contained more elements probably attributable to clays, quartz, and other clastic minerals (e.g., Al, Fe, K, Si). An evaluation of the overall element chemistry of the rock paired with Rock-Eval parameters showed (1) major/trace elements varied according to amount and type of organic carbon in the Eagle Ford samples, (2) relative abundances of certain major/trace elements were useful proxies for bulk mineralogy and depositional environment, and (3) relationships between certain clay-related major and trace elements and T<sub>max</sub> values suggesting clays and trace elements acted to catalyze the cracking of the kerogen.</p>
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Experimental study of phase relationships in part of the system Mg-Fe-Ca-Ti-Si-O at 1300°C, 1atm, and various oxygen fugacities, with applications to redox partial meltingShi, Ping January 1989 (has links)
No description available.
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577 |
Petrological studies of igneous rocks, mainly from continental extensional zonesMacdonald, Raymond January 1987 (has links)
No description available.
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578 |
The geochemistry of sediments of the Panama Basin, eastern equatorial Pacific OceanPedersen, Thomas Frederick January 1979 (has links)
No description available.
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579 |
Geochemical studies of peridotite xenoliths from southern African kimberlitesWinterburn, Peter Alan January 1987 (has links)
No description available.
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580 |
Geochemical associations of metals and organic matter in west coast Scottish sedimentsO'Donnell, David January 1987 (has links)
No description available.
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