Big earthquake methodology on minimum receiver concept(2D)

I introduce very nice solution to needs of some geoenvironments via receiver concept designed as minimum on equilateral distance,


Where,

Receiver I;
z1 depth event  between receiver I&receiver II

z2 depth event between receiver I&receiver III


Receiver II;
z1 depth event between receiver II&receiver III
z1 depth event between receiver I&receiver II

Receiver III;
z1 depth event between receiver II&receiver III

z2 depth event between receiver I&receiver III

z1 depth event between receiver III&receiver IV

z2 depth event between receiver III&receiver V


Receiver IV;
z1 depth event between receiver III&receiver IV

z1 depth event between receiver IV&receiver V



Receiver V;
z1 depth event between receiver IV&receiver V

z2 depth event between receiver III&receiver V

Note.I shortly express caused to  big impulse their analysis for some geoenvironment of establishing as a whole oconditions summaried exluding conditions about  sensing z3 depth of Receiver I and Receiver V👍

Summary:
I cite role of a nice cataloging based on depth.At this direction,I underline importance by geoenvironments of points determined considering line/lines detected for 2D modelling.You are right!"not only potential location of a big magnitude but also catching big advantage geoenvironments for all conditions carried-out  (n-1) condition on presentation"


 

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