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The properties of diffusion couples in a ternary system are examined theoretically when one end member is composed of single-phase material and the other end member is composed of two-phase material.
Facies analysis of the Cretaceous Bima Formation in the Gongola Sub –basin of the Northern Benue Trough northeastern Nigeria indicated that the Lower Bima Member is composed of alluvial fan and braided river facies associations.
The total stress in the member is composed of direct axial and bending stresses.
Each member is composed of silicate sheets (Si2O5) bonded to aluminum oxide/hydroxide layers Al2(OH)4 the two types of layers are tightly bonded.
This member is composed of bentonite rich clays, siltstone and some sandstone.
The 200 to 350 foot (60 to 105 m) thick Brushy Basin Member is composed of claystone, mudstone, and siltstone with small amounts of conglomerate and sandstone.
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The core cystine-knot fold, common to all VEGF family members, is composed of approximately 100 amino acids and has a sequence identity of between 30 and 50percentt among family members.
The composite material considered for the members is composed of typical intermediate modulus carbon fibers, Zoltek PX35 [25], combined with the Epikote MGS LR285 resin [26].
The coding sequence of all S H 3-CNL members is composed of two exons separated by an intron ranging from 157 to 272 nucleotides in length.
The middle members are composed of bedded to massive gypsum and red-green mudstone of a coastal and/or continental sabkha environment.
The members are composed of universities, TLOs corporations, organisations, and individuals.
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