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In this study, we assumed that the EER formed at shallow, upper-mantle pressures because previously estimated trace element abundances of the EER resemble those of a melt generated in the upper mantle (Korenaga 2009a) and, in particular, the upper few hundred kilometers where clinopyroxene is stable (Boyet and Carlson 2005).
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On the basis of comparisons between computed and estimated traces we have found that the best representation of the simple target is given as follows: (3).
To determine whether mt-miRNA were expressed in low level, we have employed RT-PCR assay to estimate trace amount of miRNA.
This feasibility pilot study used web-search strategies to identify the listed name for telephone numbers and to estimate tracing resources required.
Furthermore, the estimated incompatible trace element ratios of the low-μ142Nd end-member are similar to that of a 4.5 4.4 Ga dense melt that was possibly preserved above the core-mantle boundary.
They estimated the trace element composition of the basal magma ocean using partition coefficients between Mg-perovskite and melt, which were experimentally determined at the uppermost lower-mantle pressures (Corgne et al. 2005).
Boyet and Carlson (2005) and Korenaga (2009a) estimated the trace element composition of the EER based on mass-balance calculations of chondrites, EDR, and continental crust and concluded that the EER would have been generated at upper-mantle conditions.
3.8 triple operator integrals with integrands in Haagerup-like tensor products to estimates trace norms of commutators of functions of almost commuting operators.
This paper presents the results which has been obtained for different SBLOCA break sizes with the best estimate TRACE V5.0 patch 2 thermal hydraulic code and their comparison with those obtained by Westinghouse with NOTRUMP code.
The Universidad Politécnica de Madrid group has verified the low-margin bounding sequences obtained by WEC with the best-estimate TRACE code in order to verify the previous results and also to study the phenomenology of such sequences through a best-estimate code.
The Daumases have crossed the Scottish Highlands (a trip of 1,864 miles, Mr. Daumas estimated) and traced the path of the Tour de France.
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