Cracking the New GRE (2012 Edition) by Princeton Review

By Princeton Review

If you must comprehend it, it’s during this book.

Cracking the recent GRE, 2012 variation has been thoroughly revised and up to date for the adjustments coming to the GRE in August 2011. It includes: 

   • Access to four full-length perform tests (2 within the booklet and a pair of online)
   • Practice questions with targeted motives for each query
   • Key strategies for fixing textual content Completions, Sentence Equivalents, Numeric access, Quantitative Comparisons, and extra
   • Thorough overview of all GRE issues, together with every thing at the new GRE

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Extra resources for Cracking the New GRE (2012 Edition)

Example text

Such a texture is called intergranular texture. Equigranular Textures Equigranular textures are more common in plutonic rocks. Such overall textural terms as panidiomorphic granular, hypidiomorphic granular, and allotriomorphic granular are used when the bulk of the constituent grains are euhedral, subhedral, or anhedral, respectively. In large mafic (defined later) plutonic intrusions, layered structure on field to microscopic scales is common. Such rocks are called cumulates, and a whole range of textural terms are used to describe such rocks (described in a later chapter).

I components. 1 ns ity osit y 2 3 4 Upper Mantle Dike width = 1m de visc Pressure (GPa) 1 cm Dike width = 1 Moho 0 2 4 6 8 Viscosity (Pa-s) 10 10 10 2 103 104 105 10 6 Velocity (cm/s) Fig. 9 Density and viscosity of tholeiitic basalt magma as a function of pressure (based on Kushiro 1980) High-pressure measurements of density and viscosity have been very few (Fig. 9). 5 g/cm3 at a pressure of 3 GPa, whereas viscosity decreases drastically. Earlier we noted that densities of magmas are generally less than those of mantle minerals.

Aphanitic. The texture is called aphanitic if the rock is very fine grained so that individual grains are not discernible. Phaneritic. This term refers to coarsely crystallized texture. Porphyritic. Porphyritic texture is defined by the presence of conspicuously large crystals set in a groundmass of finergrained minerals or glass or a mixture of glass and finer crystals. If the phenocrysts form clusters, then the texture is called glommeroporphyritic texture. Aphyric. When a rock lacks any distinct phenocrysts, its texture is described as aphyric.

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