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Nature of the Crust Below the Achankovil Shear Zone,India Based on Gravity Data
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作者 Niraj Kumar a.p.singh B.Singh 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期200-201,共2页
Evolutionary history of continents and supercontinents, and their implications on solid earth processes, require an understanding of the growth of the continental crust through time and space.Suture zones are the remn... Evolutionary history of continents and supercontinents, and their implications on solid earth processes, require an understanding of the growth of the continental crust through time and space.Suture zones are the remnant regions inherited by Proterozoic tectonics between amalgamated terranes and the long-lived shear systems are commonly assumed to represent such boundaries.One such often debated is the 展开更多
关键词 SOUTHERN GRANULITE TERRANE Achankovil shear zone TERRANE boundary gravity ANOMALY intracratonic litho-tectonic feature
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ON THE SINGULARITIES OF COMPOSITION OF ENTIRE FUNCTIONS
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作者 a.p.singh R.Sharma 《Analysis in Theory and Applications》 2005年第4期370-376,共7页
Let f be an entire function. A point Zo is called a critical point of f if f′(zo) = O, and f(zo) is called a critical value (or an algebraic singularity) of f. Next a ∈ C is said to be an asymptotic value (or... Let f be an entire function. A point Zo is called a critical point of f if f′(zo) = O, and f(zo) is called a critical value (or an algebraic singularity) of f. Next a ∈ C is said to be an asymptotic value (or a transcendental singularity) of f if there exists a curve Г : [0, 1) → C such that limt→1 F(t) = ∞ and limt→1(f o Г)(t) = a. In this paper we find relations between the asymptotic values of f, 9 and f o 9, relations between critical points of f, 9 and f o 9 and also in the case when the two functions f and 9 are semi-conjugated with another entire function. 展开更多
关键词 asymptotic values critical values entire functions SINGULARITIES wandering domain
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