Berg Mountains

Berg Group, Berg Mountains, K-Ar Slate (GXV186A) WR 491 10 2... 

Berg-kalk, m. rock time (Geol.) mountain limestone. -kiesel, m. rock flint, chert felsite. -kohle,/. (mineral) coal, -kork, m. mountain cork (a light form of asbestos), -kreide, /. rock lime, -kristall, -krystall, m. rock crystal (transparent quartz), -kupfer, n. native copper, -lasur, /. azurite. -leder, n. mountain leather (a form of asbestos), -maun, m miner. 

Lewis, B., and D. J. Berg. Threads Primer A Guide to Multithreaded Programming. Mountain View, CA SunSoft Press, 1996. 

The upper-crustal inclusions described by Berg (1991) consist of granitic and metamorphic rocks of the basement complex that underlies the Transantarctic Mountains. The metamorphic rocks are primarily quartzites, calc-siUcate gneisses, and pelitic schists some of which contain sillimanite. The upper-crustal inclusions are particularly abundant at sites in the Transantarctic Mountains but also occur at other sites where inclusions are present. 

Kalamarides and Berg (1991) demonstrated graphically that the granulites from the Transantarctic Mountains and the Ross Embayment form separate clusters with only minor overlap in coordinates of AI2O3 vs. P O, SiO vs. FeO, and Ba vs. Ni (not shown). However, the most effective separation of the two suites of samples occurs in coordinates of the initial Sr/ Sr ratios vs. values. 

Fig. 16.9 The values and initial Sr/ Sr ratios at 900 Ma of granulite inclusions in the Cenozoic volcanic rocks in the Ross Embayment and in the Transantarctic Mountains form separate clusters. These differences indicate that the inclusions originated from distinctly different crustal sources that are separated from each other by a discontinuity (Kalamarides et al. 1987). The isotope compositions of oxygen and strontium of the Kirkpatrick Basalt in the Transantarctic Mountains (Hoefs et al. 1980) define a third cluster having low values and high initial Sr/ Sr ratios. The evidence in this diagram implies that a tectonic boundary exists in the deep crust underlying the Transantarctic Mountains and the Ross Embayment. The isotopic data also rule out a connection between the granulite inclusions in the Cenozoic lavas and the Kirkpatrick Basalt of the Transantarctic Mountains (Adapted from Fig. 1 of Kalamarides and Berg (1991))...

Benefits from using superior products, pa)nnent enjoyment of and passion for their work and also for the product, as well as several other aspects are mixed in their motivational configuration (Berg et al. 2010]. The following quote from a mountain-biker illustrates this ... 

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