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I would like to apply for Post Doctoral Mobility for Research in
University of Limerick,
Ireland. In this letter I would like to briey outline the main
motivations of my application to
the concerned authorities and respectful professors to allowin!
me to avail this opportunity
in support of my future career after reali"in! the wider scope
and facilities of research on
earth#uake monitorin!.
I had been researchin! on the topic of $%arth#uake
&eneratin! Mechanism and
%arth#uake 'arnin! (ystem Desi!n) as part of my Ph.D.
dissertation topic since my
under!raduate years with specialists in this *eld. I *rst met
with my *rst supervisor, Dr +m
Prakash Mishra, (enior &eophysicst, &eolo!ical (urvey of
India and one of the !reatest
stalwarts of seismolo!y in India. e identi*ed the fact that I
wanted to pursue this as a full
time research activity. e a!reed and in order to formulate my
need for hi!her study as a
Ph.D. (cholar personally met Dr Mrinal -anti askar, Professor,
%lectronics and /ele0
1ommunication %n!ineerin!, 2adavpur University, -olkata in
+ctober, 3445. /o live with my"est for hard0core research 6oined
2adavpur University as a full time research fellow for
takin! this pro6ect further. Initially in order to be an
eli!ible candidate for Ph.D. in
%n!ineerin!, I took up courses and modules for PhD #uali*cation
e#uivalent to Post
!raduation course related to neural network, fu""y e7pert system
and other rule based
induction methods under 2adavpur University, -olkata. I have
recently submitted my
dissertation on the topic $%arth#uake &eneratin! Mechanism
and %arth#uake 'arnin!
(ystem Desi!n) and time by conductin! a thorou!h and detailed
study of the past and
present earth#uake 8 seismicity catalo!ues as the earth#uake
precursors are found to be
valid in a re!ion which have an anomalous e9ect prior to and
durin! earth#uake. /he
physical analysis of computational models are based on three
aspects which are the
phenomenolo!ical analysis of !eo0scienti*c observations: data
de*nition and validation
throu!h continuous time si!nals from IRI(, U(&(, IMD, (;;R1,
Mo%(, %(; observatories
based on catalo!s , acceleration0time series data, radon count
analysis, satellite ima!e,
earth rotation data and synthetic location data used in
validatin! and testin! earth#uake
models. /he variations of the stress *eld precede the main shock
by days up to months
tri!!er the role of faults in re!ional deformation. In the later
meta0instability sta!es,
instability leadin! to an impendin! earth#uake event is based on
the dynamic variation
associated with meta0instability sta!e is practical indicator of
the e7pansion, accelerated
e7pansion and linka!e of nucleation models that !ive tested
approach for earth#uake
forecastin! called (ystem of !eodynamic monitorin! in localness,
radon behavior models
and rotation of the earth to observe the di9erence in the rate
of acceleration or de0
acceleration of the tectonic plate prior to a me!a0thrust
earth#uake usin! earth rotation
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data for the 34 %ner!y, University of Limerick work in the
!eneral area of
computational modellin! and statistical physics and we have
speci*cally worked in the
modellin! and analysis of earth#uakes. My study on earth#uake
forecast methodolo!y is the
determination of a slip0dependent law, will be hi!hly bene*ted
throu!h my e7perience at UL
via the resources of the University)s Material and (urface
(cience Institute ad interaction
with 1orcoran and 1lancy who have e7perience in computational
modellin! can be met
within the Department, published on ?1lancy > 1orcoran, Phys.
Rev. % 54, 4
