A5048727897- Geological and Geochemical Analysis
- Geological Studies and Exploration
- Geology and Paleoclimatology Research
- earthquake and tectonic studies
- Geochemistry and Geologic Mapping
- 3D Surveying and Cultural Heritage
- Methane Hydrates and Related Phenomena
- Geological Modeling and Analysis
- High-pressure geophysics and materials
- Mineralogy and Gemology Studies
- Geotourism and Geoheritage Conservation
- Radioactive element chemistry and processing
- Geological and Geophysical Studies Worldwide
- Microbial Community Ecology and Physiology
- Marine and environmental studies
- Education and Critical Thinking Development
- Geochemistry and Elemental Analysis
- Mining and Gasification Technologies
- Geological Formations and Processes Exploration
- Educational Strategies and Epistemologies
- Science Education and Pedagogy
- Hydrocarbon exploration and reservoir analysis
Sonoma State University
2018-2019
ORCID
2018
Stanford University
2015
Trinity University
2012
Ultraslow spreading at mid-ocean ridges limits melting due to on-axis conductive cooling, leading the prediction that peridotites from these are relatively fertile. To test this, we examined abyssal Gakkel Ridge, slowest ridge in global ocean system. Major and trace element concentrations pyroxene olivine minerals reported for 14 dredged peridotite samples Sparsely Magmatic (SMZ) Eastern Volcanic (EVZ) Zones. We observe large compositional variations among same dredge dredges close proximity...
Research Article| August 01, 2012 A detailed record of shallow hydrothermal fluid flow in the Sierra Nevada magmatic arc from low-δ18O skarn garnets Megan E. D'Errico; D'Errico 1Department Geology, Trinity University, San Antonio, Texas 78212, USA *Current address: Department Geological and Environmental Sciences, Stanford Palo Alto, California 94305, Search for other works by this author on: GSW Google Scholar Jade Star Lackey; Lackey † 2Geology Department, Pomona College, Claremont, 91711,...
Endolithic microbial communities survive nutrient and energy deficient conditions while contributing to the weathering of their mineral substrate. This study examined composition fully serpentinized weathered rock from 0.1 6.5 m depth at a site within Khalilovsky massif, Orenburg Region, Southern Ural Mountains, Russia. The includes major content serpentinite family (mostly consisting lizardite chrysotile), magnesium hydrocarbonates (hydromagnesite with lesser amounts hydrotalcite...
In the mantle, base metal sulfides have been proposed as main host for many chalcophile and siderophile elements. This includes elements such Pb, Se, Te, which are often used tracers of processes ranging from planetary accretion to mantle melting. We present in situ measurements these elements, along with As, Sb, Ag, Au, Cl, abyssal peridotite provide constraints on storage mantle. A total 152 11 peridotites 1 pyroxenite Gakkel Southwest Indian ridges were analyzed. The pentlandites, some...