**3. Conclusion**

It is proved that Amount and direction of velocity vectors or strain rate is proportional; to the quality and quantity of the stress impending. Shorter vectors signify of stored seismic energy at the reservoir of stratum. And hence characterizes of shallow focus expectation. An III vector of medium size signifies of outbreak stress drop at medium depth. All the vectors aligned in one direction and with same magnitude it is characteristic of stress line (tangential or radial perpendicular to the vectors observed At right angle to the vectors pattern observed at one region there lies the region of perpendicular stress viz. Tangential –to radial and vice versa. Vectors at these two region shows perpendicularity in relation. Velocity vectors of shorter size in general characterizes of foreshocks of seismicity at the region. Whereas larger size signifies greater magnitude of seismicity as in china 1996 with 7.5 Mw. Expectation of epicenter and focus lies better at the terminal point of

*Stress-Strain Relationship: Postulated Concept to Understand Genetic Mechanism Associated… DOI: http://dx.doi.org/10.5772/intechopen.97377*

**Figure 16.** *Electrical schematic of PCB simulation.*

smaller velocity vectors. Smaller vectors are characteristics of higher magnitude and Intensity of seismicity at the place of observation. If any motion occurs at source of waves then some surface currents are induced on some parts of the earth since the earth includes inhomogeneous materials; i.e., including conducting and/or non conducting bodies and/or free spaces, etc. in some locations. If any part of these materials makes a deviation then those surface currents variate with respect to time.

The assumption for the fact gives the result below: The Lorentz's forces, which are applied on variating currents due to the geo electromagnetic field appear at least. A new force [2] additional to Lorentz's force has to be observed due to the irregularities, too. This additional force has to have a very small magnitude around source of waves, but it has to have an irregularly and non-smoothly deviating character, so it propagates with increasing-decreasing in magnitude with some periods according to some transfer rules of forces in bodies. The modernized physical mechanism beyond the earthquake phenomena is explained with the above mentioned approach. The fact behind the earthquake phenomenon is postulated. Restrictions at the use of some specific frequency values are necessary to the frequency spectrum used in systems all around the earth to realize a successful prediction.

#### **Acknowledgements**

I give my gratitude and obligation are bid to Author cited in the reference section for their prior and later permission for theirs; reference figure and data viz.; Dr. E. Holt; Stony Brook University New York.

**3. Conclusion**

**Figure 15**.

**132**

**Figure 14.**

*Initial electrical schematic.*

It is proved that Amount and direction of velocity vectors or strain rate is proportional; to the quality and quantity of the stress impending. Shorter vectors signify of stored seismic energy at the reservoir of stratum. And hence characterizes of shallow focus expectation. An III vector of medium size signifies of outbreak stress drop at medium depth. All the vectors aligned in one direction and with same magnitude it is characteristic of stress line (tangential or radial perpendicular to the vectors observed At right angle to the vectors pattern observed at one region there lies the region of perpendicular stress viz. Tangential –to radial and vice versa. Vectors at these two region shows perpendicularity in relation. Velocity vectors of shorter size in general characterizes of foreshocks of seismicity at the region. Whereas larger size signifies greater magnitude of seismicity as in china 1996 with 7.5 Mw. Expectation of epicenter and focus lies better at the terminal point of

*Double-sided PCB layout (the bottom layer is a large area grounding).*

*Computational Optimization Techniques and Applications*

I offer my special thanks and gratitude to Wiley publications for citing the mathematical equations for principal section of paper. I must acknowledge to Dr. P. V.S. Raju, Head, Department of Centre for Ocean and atmospheric Sciences and Technology amity University Jaipur India, support to carry out the research.

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*DOI: http://dx.doi.org/10.5772/intechopen.97377*

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