Carlin J. Green
Carlin Green is a Geologist with the USGS Geology, Energy & Minerals (GEM) Science Center in Reston, VA.
Carlin began his career at the USGS as a student while studying the mineralogy of iron resources in the Lake Superior region. He earned his Master’s degree in Earth Systems Science from George Mason University in 2017. Presently, his work focuses on the mineralogical characterization of critical element resources and mineral resource assessments.
Professional Experience
2018 - Present: Geologist, USGS, Reston VA
2015 - 2017: Pathways Student, USGS, Reston VA
Education and Certifications
M.S. Earth Systems Science, George Mason University, 2017
B.S. Geology, George Mason University, 2015
Science and Products
Filter Total Items: 25
Chemistry, morphology, modal mineralogy, and photomicrographs of amphiboles and other minerals in the Ironwood Iron-Formation, Gogebic Iron Range, Wisconsin, USA Chemistry, morphology, modal mineralogy, and photomicrographs of amphiboles and other minerals in the Ironwood Iron-Formation, Gogebic Iron Range, Wisconsin, USA
The Ironwood Iron-Formation, part of the Gogebic Iron Range in Wisconsin, is a Paleoproterozoic Superior-type banded iron formation (BIF) with substantial iron resource potential. The development of a Mesoproterozoic contact metamorphic aureole related to the emplacement of the Mellen Intrusive Complex resulted in the production of a variety of silicate minerals in the western portion of...
Science and Products
Filter Total Items: 25
Chemistry, morphology, modal mineralogy, and photomicrographs of amphiboles and other minerals in the Ironwood Iron-Formation, Gogebic Iron Range, Wisconsin, USA Chemistry, morphology, modal mineralogy, and photomicrographs of amphiboles and other minerals in the Ironwood Iron-Formation, Gogebic Iron Range, Wisconsin, USA
The Ironwood Iron-Formation, part of the Gogebic Iron Range in Wisconsin, is a Paleoproterozoic Superior-type banded iron formation (BIF) with substantial iron resource potential. The development of a Mesoproterozoic contact metamorphic aureole related to the emplacement of the Mellen Intrusive Complex resulted in the production of a variety of silicate minerals in the western portion of...