Chris Jenkins is located at GMEG Science Center in Spokane, WA. Chris received a MSc in Earth Science from the University of Toronto in 2017 and a PhD in Earth Science from Carleton University in 2021. Since joining the USGS in 2016, Chris specializes in studying magmatic ore deposits using igneous petrology, numerical modeling, and geostatistics.
Professional Experience
2022 - Present, Mendenhall Postdoctoral Fellow, Geology Minerals Energy and Geophysics Science Center, Spokane, WA.
2016 - 2022, Physical science technician, Geology Minerals Energy and Geophysics Science Center, Spokane, WA.
Education and Certifications
PhD Earth Sciences, Carleton University, 2021
MSc Earth Sciences, University of Toronto, 2017
BSc Geology, Eastern Washington University, 2015
Affiliations and Memberships*
2014 - Present: Society of Economic Geologists
2014 - Present: American Mineralogical Society
2013 - Present: Geological Society of America
Science and Products
Geochemistry of rocks and rock fabric data near the hanging wall contact to the Reef Package, Stillwater Complex, Montana, USA
Titanium-vanadium deposits hosted in mafic-ultramafic layered intrusions and massif anorthosite intrusions from around the world
Missouri Breaks Project, Montana - Digitized aeromagnetic data
A novel origin for PGE reefs: A case study of the J-M Reef
Origin of the J-M Reef and Lower Banded series, Stillwater Complex, Montana, USA
The nature and composition of the J-M Reef, Stillwater Complex, Montana, USA
Science and Products
- Data
Geochemistry of rocks and rock fabric data near the hanging wall contact to the Reef Package, Stillwater Complex, Montana, USA
The Reef Package is a sequence of coarse-grained cumulates that host the J-M Reef Pd-Pt deposit in the Stillwater Complex of Montana. The top of the Reef Package marks the top of economic-grade platinum-group element mineralization and is identified by a distinct change in rock fabric, from the coarse-grained rocks of the Reef Package to finer-grained cumulates in the hanging wall. This dataset taTitanium-vanadium deposits hosted in mafic-ultramafic layered intrusions and massif anorthosite intrusions from around the world
This data release includes four .csv files and one Esri shapefile which contain data on titanium-vanadium deposits hosted in mafic-ultramafic layered intrusions and massif anorthosite intrusions from around the world. Some of the data was used to create a grade and tonnage model for titanium-vanadium deposits hosted in mafic-ultramafic layered intrusions. Only deposits with reported grade and tonnMissouri Breaks Project, Montana - Digitized aeromagnetic data
From February 12 to March 8, 1981, EG and G Geometrics conducted an aeromagnetic survey in Montana for Anaconda Copper Company. A Piper Navajo aircraft was used to conducted the survey. The survey was flown along north-south flightlines spaced 660 feet at a nominal height of 450 feet above the terrain. Five uniformly spaced east-west tie-lines were also flown. During processing, the International - Publications
A novel origin for PGE reefs: A case study of the J-M Reef
The origin of meter scale stratiform layers of disseminated sulfides in enriched platinum group element (PGE) tenors and grades, called reef-type deposits, are the world’s most significant source of PGEs. Their origin in layered mafic intrusions remains debated, but in general, most researchers favor an orthomagmatic origin for reef-type deposits and agree that their formation requires the equilibOrigin of the J-M Reef and Lower Banded series, Stillwater Complex, Montana, USA
The origin and parental magma for layered cumulates in the Lower Banded series (LBS) and the J-M Reef Pd-Pt deposit of the Stillwater Complex remains poorly constrained. We present whole-rock lithogeochemistry and mineral chemistry from LBS rocks collected from drill holes and surface samples from the Mountain View area of the complex that in total span nearly the entirety of the LBS stratigraphy.The nature and composition of the J-M Reef, Stillwater Complex, Montana, USA
In this contribution, we analyze 30 years of mine development data and quantitatively identify the processes that control the grade and tenor of the mineralized rock. An assay database of more than 60,000 samples was used to examine variations in ore grade and tenor of the sulfide mineralization in the J-M reef horizon of the Stillwater Complex along the strike and down the dip of the deposit in t
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government