The composition reported here is the average of two samples: UT2096, UT2109
Changing ideas on the identity and stratigraphic significance of the Sheep Creek tephra beds in Alaska and the Yukon Territory, northwestern North America
|StationID||Latitude||Longitude||Geologist||DateVisited||Age Info||Volcano||Eruption||Location Description||Text Description||Sample ID||Sample Type 1||Sample Type 2||Final Unit||Material||Coeff||SiO2||TiO2||Al2O3||FeOT||MnO||MgO||CaO||Na2O||K2O||P2O5||Total-majors||REF majors||METH majors||Fe2O3/Fe203T orig||FeO/FeOT orig||Volatiles csv||METH volatiles||Cs||Rb||Ba||Sr||La||Ce||Pr||Nd||Sm||Eu||Gd||Tb||Dy||Ho||Er||Tm||Yb||Lu||Y||Zr||Nb||Hf||Ta||Pb||Th||U||Sc||V||Cr||Fe||Co||Ni||Cu||Zn||Ga||Mo||As||Na||K||Ref trace1||METH trace1||Rb||Ba||Sr||La||Ce||Nd||Sm||Eu||Gd||Dy||Er||Yb||Lu||Y||Zr||Nb||Pb||Th||U||Sc||Ti||V||Cr||Ni||Cu||Zn||Ga||Ref trace2||METH trace2||Light csv||Halogen csv||other major csv||other lile csv||other ree csv||other hfse csv||other hpe csv||other tm csv||other misc csv|
|Westgate_2001_Sheep_Creek_Tephra_C_Average||63.6||-138.59998||Westgate, J. A.||-78050--||Sheep Creek tephra (SCt) refers to a family of tephra beds that closely resemble one another in their petrographic and compositional characteristics (Westgate et al. 2007). Sheep Creek-C tephra occurs at Dominion Creek, where it is found on the surface of a forest bed, exactly the same stratigraphic setting as at Ash Bend site. SCt-A (aka Ash Bend tephra) is also at Ash Bend, Yukon. Generic location selected near Dominion Creek, Yukon Territory, Canada. Glass geochemical data reported here is average calculated from analyses of multiple tephra correlated across different stratigraphic locations. Individual sample IDs are noted in the sample description (see Westgate et al. 2007 footnote of table 5).||The composition reported here is the average of two samples: UT2096, UT2109||Westgate_2001_SCt-C||Tephra Fall||Cumulate||Glass||76.82||0.15||13.43||1.05||0.04||0.24||1.28||3.8||3.02||4365||EMP||1.05||Cl=0.19; H2O=5.7||EMP|
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