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pro vyhledávání: '"Laura Reiser Wetzel"'
Autor:
Laura Reiser Wetzel
Publikováno v:
Numeracy, Vol 4, Iss 1, p 4 (2011)
The Spreadsheets Across the Curriculum (SSAC) library consists of activities to reinforce or teach quantitative literacy or mathematical concepts and skills in context. Each SSAC “module” consists of a PowerPoint presentation with embedded Excel
Externí odkaz:
https://doaj.org/article/2f32bea2fec74c468ad730c9fe717b96
Autor:
Kelly R. Debure, Laura Reiser Wetzel
Publikováno v:
Journal of College Science Teaching.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Laura Reiser Wetzel, Cliff Frohlich
Publikováno v:
Geophysical Journal International. 171:909-920
SUMMARY This is a global survey of seismic moment release rates (scalar moment/length/time) along five categories of plate boundaries; for shallow earthquakes we evaluate divergent, transcurrent and convergent boundaries; for deep earthquakes we cons
Autor:
Laura Reiser Wetzel
Publikováno v:
Journal of Geoscience Education. 50:404-409
Building stones provide conveniently located and accessible “urban outcrops.” As such, building stones may be used for semester-long student research projects in upper-level geology courses. I present students in my Earth Materials class with a s
Publikováno v:
Journal of Volcanology and Geothermal Research. 110:319-341
Coordinated geochemical and hydrological calculations guide our understanding of the composition, fluid flow patterns, and thermal structure of near-ridge oceanic crust. The case study presented here illustrates geochemical and thermal changes taking
Autor:
Laura Reiser Wetzel, Everett L. Shock
Publikováno v:
Journal of Geophysical Research: Solid Earth. 105:8319-8340
Submarine hydrothermal vent fluid compositions may be controlled by peridotite-seawater or basalt-seawater reactions. Previous studies of slow-spreading ridges indicate that in addition to basalts, peridotites often play a prominent role in the const
Publikováno v:
Nature. 362:235-237
MIGRATING non-transform offsets, which occur along mid-ocean ridges when a propagating segment gradually elongates and takes over spreading from a neighbouring 'doomed' rift segment1–3, represent a significant modification of the plate tectonic par