Scholarly Communications Brown Bag & Workshop for Librarians

This brown bag / workshop will provide liaison librarians with the opportunity to learn and discuss the value of scholarly communications & outreach efforts at Wayne State, as well as see the new scholarly communications / open access presentation targeted towards faculty that was developed by the Scholarly Communications Team

Student Fact Book, Fall 2002, Twenty-Sixth Annual Edition, Wright State University

The student fact book has general demographic information on all students enrolled at Wright State University for Fall Quarter, 2002

Scholarly Communications Outreach: A Workshop for Librarians

This workshop will help liaison librarians in their scholarly communications and open access outreach efforts with faculty. Workshop will incorporate current videos created by BePress on outreach and discussion of these videos, and teach librarians the process behind adding faculty contributions to DigitalCommons@WSU, focusing on how to conduct permissions and rights checks for faculty publications that may be good additions to DigitalCommons@WSU and the deposit process

Analyze the Tranmissivity for Pumping Well testing with Single and Observation Well

In general, for determining aquifer parameters pumping test conducted on the production well, since in Erbil catchment area observation wells are not exist. In the present study steady state pumping test method using single well was used to estimate the tranmissivity of the aquifer. For this purpose pumping test conducted on a single production pumping well at the specific area which is located at the QATAWI area near Erbil city. The results of transmissivity obtained from single well pumping test data compared with that obtained from observation well. The value of Transmissivity calculated from the field data via pumping test on single pumping well equal to 13.05 m/day however its value obtained from observation well equal to 197.7 m/day. It was observed that there are differences between the results of transmisivity of the aquifer using single pumping well and observation well. It is result using observation well is higher than observation well; this is mostly due to the losses that are available within the pumping well. To get a real value of transmissivity of the aquifer the pumping test should be conducted on an observation well or adjustment of the data after single well testing

Highly refractory Archaean peridotite cumulates: Petrology and geochemistry of the Seqi Ultramafic Complex, SW Greenland

This paper investigates the petrogenesis of the Seqi Ultramafic Complex, which covers a total area of approximately 0.5 km2. The ultramafic rocks are hosted by tonalitic orthogneiss of the ca. 3000 Ma Akia terrane with crosscutting granitoid sheets providing an absolute minimum age of 2978 ± 8 Ma for the Seqi Ultramafic Complex. The Seqi rocks represent a broad range of olivine-dominated plutonic rocks with varying modal amounts of chromite, orthopyroxene and amphibole, i.e. various types of dunite (s.s.), peridotite (s.l.), as well as chromitite. The Seqi Ultramafic Complex is characterised primarily by refractory dunite, with highly forsteritic olivine with core compositions having Mg# ranging from about 91 to 93. The overall high modal contents, as well as the specific compositions, of chromite rule out that these rocks represent a fragment of Earth’s mantle. The occurrence of stratiform chromitite bands in peridotite, thin chromite layers in dunite and poikilitic orthopyroxene in peridotite instead supports the interpretation that the Seqi Ultramafic Complex represents the remnant of a fragmented layered complex or a magma conduit, which was subsequently broken up and entrained during the formation of the regional continental crust. Integrating all of the characteristics of the Seqi Ultramafic Complex points to formation of these highly refractory peridotites from an extremely magnesian (Mg# ~ 80), near-anhydrous magma, as olivine-dominated cumulates with high modal contents of chromite. It is noted that the Seqi cumulates were derived from a mantle source by extreme degrees of partial melting (>40%). This mantle source could potentially represent the precursor for the sub-continental lithospheric mantle (SCLM) in this region, which has previously been shown to be ultra-depleted. The Seqi Ultramafic Complex, as well as similar peridotite bodies in the Fiskefjord region, may thus constitute the earliest cumulates that formed during the large-scale melting event(s), which resulted in the ultra depleted cratonic keel under the North Atlantic Craton. Hence, a better understanding of such Archaean ultramafic complexes may provide constraints on the geodynamic setting of Earth’s first continents and the corresponding SCLM.Department of Geological Sciences, Stanford University, 450 Serra Mall, Stanford, CA 94305, USA Department of Earth & Planetary Sciences, McGill University, Quebec, Canada Department of Geology, Lund University, Sölvegatan 12, 223 62 Lund, Sweden School of Earth and Ocean Sciences, Cardiff University, Main Building, Cardiff CF10 3AT, United Kingdom College of Science, University of Derby, Derby, DE22 1GB, U

Student Fact Book, Fall 1996, Wright State University

The student fact book has general demographic information on all students enrolled at Wright State University for Fall Quarter, 1996

Student Fact Book, Fall 2012, Thirty-Sixth Annual Edition, Wright State University

The student fact book has general demographic information on all students enrolled at Wright State University for Fall Quarter, 2012