G. Nowell

发表

LARGE IGNEOUS PROVINCES AND KIMBERLITES? ORIGIN OF THE DIAMONDIFEROUS AMON KIMBERLITES, BAFFIN ISLAND, ARCTIC CANADA

S. Kurszlaukis, B. Kjarsgaard, S. Tappe, 2011 .

Kimberlites: High H 2 O/CO 2 , MgO-rich, Al- and K-Poor, Silica Undersaturated Magmas

B. Kjarsgaard, D. Pearson, S. Tappe, 2008 .

THE CONTRAST IN TRACE ELEMENT CHEMISTRY AND VOLATILE COMPOSITION BETWEEN FLUID INCLUSIONS IN FIBROUS AND OCTAHEDRAL DIAMONDS

E. Smith, J. Ryder, G. Nowell, 2012 .

Weathering fluxes and sediment provenance on the SW Scottish shelf during the last deglaciation

C. Clark, D. Fabel, J. Howe, 2017, Marine Geology.

Re-Os and HSE in individual base metal sulfide grains: Evaluating micro-analytical procedures using a sulfide reference material

R. Fonseca, A. Luguet, A. Heuser, 2018, Chemical Geology.

Re-Os isotope characteristics of postorogenic lavas: Implications for the nature of young lithospheric mantle and its contribution to basaltic magmas

N. Rogers, C. Hawkesworth, D. Pearson, 2000 .

Constraining the crust and mantle contributions to kimberlite – a multi-phase micro-sampling approach

C. Ottley, D. Pearson, R. Mitchell, 2008 .

Crystallization of megacrysts from kimberlites: Geochemical evidence from high-Cr megacrysts in the Jericho kimberlite

D. Pearson, G. Marković, M. Kopylova, 2008 .

The genesis of kimberlite: geochemical constraints

B. Kjarsgaard, D. Pearson, D. Dowall, 2008 .

Lu-Hf and Re-Os isotopic studies of lamproite genesis

D. Pearson, A. Irving, G. Nowell, 2008 .