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The geochemistry and petrogenesis of the Paleoproterozoic du Chef dyke swarm, Québec, Canada

Kerr, Andrew C., McDonald, Iain, Ernst, Richard E., Hughes, Hannah S. R., Minifie, Matthew J., Ciborowski, T. Jake R.

A mantle plume origin for the Palaeoproterozoic Circum-Superior Large Igneous Province

Ciborowski, T. Jake R., Kerr, Andrew C., Ernst, Richard E., Baragar, Bob, Millar, Ian L., Minifie, Matthew J.

The early proterozoic Matachewan Large Igneous Province: geochemistry, petrogenesis and implications for Earth evolution

Ciborowski, T. Jake R., Ernst, Richard E., McDonald, Iain, Minifie, Matthew J., Harlan, Stephen S., Millar, Ian L., Kerr, Andrew C.

a source mantle potential temperature of c. 1500–1550C. Comparison of these mantle potential

Magnetized Kerr–Newman–Taub-NUT spacetimes

Ghezelbash M., Siahaan H.M.

Magnetized Kerr–Newman–Taub-NUT spacetimes

Adducts AnC60Hn: Electro-optical properties and quantum chemical calculation data

Yevlampieva N.P., Sheka E.F.

Experimental studies of electro-optical Kerr effect in solution detect variations in the molecular

Zero mass limit of Kerr spacetime is a wormhole

Gibbons G., Volkov M.

in the literature, the zero mass limit of Kerr spacetime is not flat Minkowski space but a spacetime whose geometry

Kerr-bolt spacetimes and KERR/CFT correspondence

Ghezelbash A.M.

Kerr-bolt spacetimes and KERR/CFT correspondence

The complements of lower cones of degrees and the degree spectra of structures

Andrews U., Cai M., Kalimullin I., Lempp S., Miller J., Montalbán A.

Computably enumerable (c.e.) sets

Black holes and particles with zero or negative energy

Grib A., Pavlov Y.

Kerr metric

Nondensity of double bubbles in the D.C.E. degrees

Andrews U., Kuyper R., Lempp S., Soskova M., Yamaleev M.

bubbles” are not downward dense in the d.c.e. degrees. Here, a pair of d.c.e. degrees d1 > d2 > 0 forms a

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