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Matthew J. Brzozowski
University of Windsor
GeologyRemanenceGeochemistryMagmaFelsicQuartz monzoniteStable isotope ratioHydrocarbonMagnetiteIsotope fractionationAmphiboleIsotopes of oxygenGabbroGeophysics
6Publications
1H-index
4Citations
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Publications 6
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#1Matthew J. Brzozowski (U of W: University of Windsor)H-Index: 1
#2Iain M. Samson (U of W: University of Windsor)H-Index: 28
Last. Robert L. Linnen (UWO: University of Western Ontario)H-Index: 24
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The Eastern Gabbro of the alkaline Coldwell Complex, Canada, represents a Ni-poor conduit-type system that comprises two rock series, the Layered Series and Marathon Series, which intruded into a metabasalt package. Based on distinct variations in magnetite compatible (e.g., Ni, Cr) and incompatible (e.g., Sn, Nb) elements in Fe–Ti oxide intergrowths, the metabasalts, Layered Series, and Marathon Series must have crystallized from magmas that originated from compositionally distinct sources. Of ...
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#1Matthew J. Brzozowski (U of W: University of Windsor)H-Index: 1
#2Iain M. Samson (U of W: University of Windsor)H-Index: 28
Last. D. J. Good (UWO: University of Western Ontario)H-Index: 6
view all 5 authors...
Magnetite (mag)–ilmenite (ilm) intergrowths are more common than mag–ulvospinel (usp) intergrowths in mafic–ultramafic Ni–Cu–PGE systems, yet the former has no known solid solution. The most accepted model for the formation of mag–ilm intergrowths in terrestrial environments is fluid-induced oxidation of mag–usp assemblages by oxygen in water. In this study, we re-examine this model in light of the fact that crustal fluids have very low pO2 and that mag–ilm intergrowths commonly occur in rocks t...
1 CitationsSource
#1Matthew J. Brzozowski (U of W: University of Windsor)H-Index: 1
#1M. J. Brzozowski (U of W: University of Windsor)
Last. Robert L. Linnen (UWO: University of Western Ontario)H-Index: 24
view all 5 authors...
2 CitationsSource
#1Hui Ye (NU: Nanjing University)H-Index: 1
#2Chang-Zhi Wu (NU: Nanjing University)H-Index: 12
Last. Weiqiang Li (NU: Nanjing University)H-Index: 15
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Abstract Equilibrium isotope fractionation factors are the basis for application of stable isotopes in geological studies. Experimental calibration and theoretical calculations have been employed to determine Fe isotope fractionation factors for a variety of minerals, however, these methods have their limitations. An alternative approach to calibrating inter-mineral Fe isotope fractionation factors is to use well-characterized geological samples; this approach has unique advantages over the othe...
1 CitationsSource
#1Wenjing Xu (SYSU: Sun Yat-sen University)
#2Xisheng Xu (NU: Nanjing University)H-Index: 30
Last. Matthew J. Brzozowski (NU: Nanjing University)H-Index: 1
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Understanding the mechanisms responsible for the interplay between mafic and felsic magmas is the key to retrieving information on their sources, and characterizing the exchange of mass between them. In order to characterize compositional and mineralogical changes in the mafic end-member during mafic-felsic magma interaction and to better understand the nature of early Paleozoic intracontinental magmatism in the South China Block (SCB), a detailed study was conducted on an early Paleozoic hornbl...
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#1Yong Zhang (NU: Nanjing University)H-Index: 4
#2Adrian R. Muxworthy (Imperial College London)H-Index: 31
Last. Matthew J. Brzozowski (NU: Nanjing University)H-Index: 1
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