Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Eric D. Stewart"'
Publikováno v:
Groundwater. 59:829-838
Arsenic in private drinking water wells is a significant problem across much of eastern Wisconsin, USA. The release mechanism and stratigraphic distribution of sulfide and iron (hydr)oxide sources of arsenic in bedrock aquifers are well understood fo
Publikováno v:
The Journal of Geology. 129:1-31
Up to 2 km of siliciclastic and chemical sedimentary rocks, metamorphosed to greenschist facies, are preserved in the Baraboo Hills of southern Wisconsin. The strata compose two sedimentary...
Publikováno v:
Geological Society, London, Memoirs. 49:75-92
The mantle and crustal sections of the Permian Dun Mountain ophiolite (DMO) in New Zealand9s South Island have similar and potentially related tectonic histories. The mantle section records a four-part sequence of mid-ocean ridge basalt, and boninite
Publikováno v:
Precambrian Research. 314:221-239
The Statherian Baraboo Quartzite (1710–1650 Ma) is present in the Baraboo Ranges, Wisconsin, USA. It is one of several isolated quartzites outcropping across the southern Lake Superior region. Collectively, these quartzites are known as Baraboo int
Publikováno v:
Journal of Petrology. 57:751-776
Autor:
Eric D. Stewart, George Segee-Wright, Latisha Ashley Brengman, Esther K. Stewart, Aurélien Moy, John H. Fournelle
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
William M. Lamb, Lindsey German, Brent V. Miller, Julie Newman, Basil Tikoff, Eric D. Stewart
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Tectonophysics. 588:171-178
Attempts to calibrate mechanical results obtained in triaxial compression experiments using solid media assemblies in a Griggs piston-cylinder apparatus have failed to reveal a dependable relationship between results obtained using a talc assembly an
Publikováno v:
Geology. 38:927-930
A non-North American provenance for the lower Belt Supergroup of North America has been used to support various pre-Rodinian paleogeographic reconstructions. Unlike the lower Belt Supergroup, most upper Belt Supergroup provenance studies have inferre