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Richard A. D. Pattrick

Researcher at University of Manchester

Publications -  146
Citations -  6993

Richard A. D. Pattrick is an academic researcher from University of Manchester. The author has contributed to research in topics: Extended X-ray absorption fine structure & Magnetite. The author has an hindex of 44, co-authored 144 publications receiving 6311 citations. Previous affiliations of Richard A. D. Pattrick include Daresbury Laboratory & Lawrence Berkeley National Laboratory.

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Mechanism of molybdenum removal from the sea and its concentration in black shales: EXAFS evidence

TL;DR: In this article, the authors introduce the concept of a geochemical switch, in which HS- transforms the marine behavior of a conservative element to that of a particle reactive element, and the action point of the HS- switch is calculated to be, a(HS)- = 10(-3.6) - 10(-4.3).
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Variations in the compositional, textural and electrical properties of natural pyrite: a review

TL;DR: In this article, the results of a review that has been conducted to establish the range in variability of natural pyrite with regard to chemical composition, texture and electrical properties are presented.
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Electrical and magnetic properties of sulfides

TL;DR: In this article, the theory and measurement of electrical and magnetic properties of sulfide minerals are outlined along with spectroscopic and diffraction studies that can provide insights into magnetic behavior.
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Fluid inclusion noble gas and halogen evidence on the origin of Cu-Porphyry mineralising fluids

TL;DR: The naturally occurring noble gas isotopes (40Ar, 36Ar, 84Kr and 129Xe) and halogens (Cl, Br, I) have been determined simultaneously in irradiated quartz vein samples by noble gas mass spectrometry as discussed by the authors.
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The structure of amorphous copper sulfide precipitates: An X-ray absorption study

TL;DR: X-ray absorption and X-ray photoelectron spectroscopy (XPS) analysis of copper sulfide precipitated from aqueous solution at ambient temperatures reveals the existence of a metastable primitive structure that ages to a structure with the characteristics of amorphous covellite as discussed by the authors.