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Collagen's success as the principal structural element in load-bearing, connective tissue has motivated the development of numerous engineering approaches designed to recapitulate native fibril morphology and strength.
The design strategy should ensure structural integrity by requiring the composite product, particularly a principal structural element, to be damage tolerant.
Apolipoprotein B is the protein that constitutes the principal structural element of lipoprotein particles for very-low-density lipoprotein (VLDL), intermediate-density lipoprotein (IDL), and LDL.
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Fig. 1 Well locations and principal structural elements in the Danish area.
However, the principal structural elements associated with the driving force for non-volcanic seismic swarms and hydration of the mantle wedge and overlying plate are less well documented because of a lack of high-resolution seismic structures, even though this knowledge is crucial in assessing the mechanisms of non-volcanic seismic swarms.
CKs are the principal structural elements of intracellular microfilaments.
As the principal structural elements, laminin and collagen IV form distinct networks [ 81] which become noncovalently interconnected by mono- or oligomeric nidogen [ 41, 82, 83] and perlecan, able to form irregular polymers [ 74, 84] and 1(b)).
CKs, which are now called keratins, are the principal structural elements of the cytoskeleton (keratin filaments) of epithelial cells, including bronchial epithelial cells, and have been classified into 20 subtypes based on differences in the molecular mass and isoelectric point as determined by 2-dimensional electrophoresis [ 20, 21].
This carbohydrate macromolecule is the principal structural component of the cell wall of most plants.
Notochord, flexible rodlike structure of mesodermal cells that is the principal longitudinal structural element of chordates and of the early embryo of vertebrates, in both of which it plays an organizational role in nervous system development.
To investigate the principal seismic structural elements linked to the non-volcanic seismic swarm and subduction complex associated with the Philippine Sea slab, we deployed a temporary, dense linear array consisting of 86 portable seismic stations extending 100 km, from the southern to the northern edge of the western Kii Peninsula, which crosscuts the Wakayama region (Figure 1).
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