Tag Archives: Metal

New publications from my research group (02/06/14)

Posted on February 6, 2014 by stevepiercey

It’s been a while since I’ve updated this blog. The combination of fieldwork, teaching, and just being generally busy, hasn’t provided much time for extra-curricular writing. I’m taking a bit of a departure from previous posts, and just providing an … Continue reading →

Posted in Analytical Geochemistry, Appalachians, Economic Geology, Exploration Geochemistry, Geochemistry, Geology, Gold, Gold Deposits, Lead, Lithogeochemistry, Mineral Resources, Quality Control, Seafloor Massive Sulfides, Volcanogenic Massive Sulfides, Zinc | Tagged , , , , , , , , , , , , | Leave a comment

Noble Metals, Subcontinental Lithosphere, and Ni-Cu-PGE Deposits

Posted on May 28, 2013 by stevepiercey

Recent research by Kamenetsky et al. published in Geology provides insight into the nature of the parental magmas potentially responsible for the formation of nickel-copper-platinum group element (Ni-Cu-PGE) deposits in intra-plate environments.  Previous researchers have illustrated the importance of the … Continue reading →

Posted in Copper, Economic Geology, Geochemistry, Geology, Layered intrusions, Magmatic Sulfides, Mineral Resources, Nickel, Platinum Group Elements, Recently Published | Tagged , , , , , , , , , , , , | Leave a comment

Classic papers in Economic Geology: Campbell and Naldrett (1979) – The Influence of Silicate-Sulfide Ratios on the Geochemistry of Magmatic Sulfides

Posted on May 15, 2013 by stevepiercey

Magmatic sulfide deposits are critical sources of nickel (Ni), copper (Cu), and platinum group elements (PGE) globally.  These deposits form from the segregation of a sulfide liquid from a silicate liquid, similar to oil separating from water, due to the … Continue reading →

Posted in Classic Papers, Copper, Economic Geology, Geochemistry, Geology, Layered intrusions, Magmatic Sulfides, Mineral Resources, Nickel, Platinum Group Elements | Tagged , , , , , , , , , | 2 Comments

Classic papers in Economic Geology: Fallick et al. (2001) – Bacteria were responsible for the magnitude of the world-class hydrothermal base metal base metal sulfide deposit at Navan, Ireland

Posted on April 30, 2013 by stevepiercey

Irish-type zinc-lead deposits represent a distinctive sub-class of the carbonate-hosted zinc-lead deposit family, having geological features and genetic models that are hybrids between sedimentary exhalative (SEDEX; also known as clastic zinc-lead deposits) and Mississippi Valley-type (MVT) deposits.  They are important … Continue reading →

Posted in Bacteria, Biogeochemistry, Carbonate-hosted deposits, Classic Papers, Economic Geology, Geochemistry, Geology, Geophysics, Ireland, Irish-type deposits, Lead, Mineral Resources, Seafloor, Seafloor Massive Sulfides, Sedimentary exhalative deposits, Sedimentology, Stable Isotopes, Zinc | Tagged , , , , , , , , , , , , , | Leave a comment

The origin of banding in banded iron formations (BIF)

Posted on April 16, 2013 by stevepiercey

Banded iron formations (BIF) and iron ore are globally important resources of iron that have very distinctive textures.  Well-preserved BIF contain iron-rich bands consisting of iron oxides (e.g., hematite, magnetite), iron silicates (e.g., stilpnomelane), and iron oxyhydroxides (e.g., greenalite), that … Continue reading →

Posted in Banded Iron Formations, Economic Geology, Geology, Iron Ore, Mineral Resources, Submarine Volcanism | Tagged , , , , , , , | 2 Comments