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RReedduucciinngg EEaarrtthhqquuaakkee LLoosssseess iinn tthhee EExxtteennddeedd MMeeddiitteerrrraanneeaann RReeggiioonn
UUNNEESSCCOO--RREELLEEMMRR
XXXXXXVV IInntteerrnnaattiioonnaall WWoorrkksshhoopp
28-31 October 2013
Fuengirola (Malaga), Spain
RReedduucciinngg EEaarrtthhqquuaakkee LLoosssseess iinn tthhee EExxtteennddeedd MMeeddiitteerrrraanneeaann RReeggiioonn
UUNNEESSCCOO--RREELLEEMMRR XXXXXXVV IInntteerrnnaattiioonnaall WWoorrkksshhoopp
28-31 October 2013
Fuengirola (Malaga), Spain
SC/DRR/2013/1 Paris, France. October 2013
Original: English
United Nations Educational, Scientific and Cultural Organization – UNESCO U.S. Geological Survey – USGS Real Instituto y Observatorio de la Armada in San Fernando – ROA Network of European Research Infrastructures for Earthquake Risk Assessment and Mitigation – NERA
Editorial coordinators: Frederick Simon
Jose Martín Davila Jair Torres
Cover photo credit: Badaoui Rouhban
For further information, please contact:
Cross-Cutting Thematic Unit on Disaster Risk Reduction Natural Science Sector UNESCO 1, rue Miollis 75732 Paris cedex 15 France Phone: + 33-1-45 68 41 22 Fax: + 33-1-45 68 58 21 E-mail: [email protected]
The authors are responsible for the choice and presentation of facts contained in this publication and for the opinions expressed therein, which are not necessarily those of UNESCO and do not commit the Organization. The designations employed and the presentation of the material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries.
© UNESCO 2013 Printed in Spain
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abilistic modces occurres of two see p-value, ebetween 0.7nd 1.43 ± 0.
odified Bath of the accu of energy 80% of the
g 4.8, Bulladimension Dio, as the re, we havevent, 58% arthquakes.
the correlaed, and the
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atistical aS
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eismicity paexplaining th77 ± 0.05 a10, showing
h’s law is usumulated eis released
e total eners 2002, andD2 is estimaratio of the
e obtained afor the La .
ations betwAki’s relatio
Workshop ended Mediterra
nalysis ofSouth and
amdache(1),
ent Etudes ent of Physi
ed to analyzh and Soutrameters: the tempora
and 1.18 ± 0g broad reg
sed to analnergy is reld during thrgy is releasd an 87% dated using
e slip occura slip ratio ePaca 2005
ween the fron D=3b/c is
anean Region (R
f some aft Southeas
J.A. Peláez
et Surveillacs, Univers
ze the spatitheastern Sthe b-value l decay rate0.10. The cimes of the
yze the eneeased in the aftershocsed during
during the mthe correlat
rred on primequal to 71
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ractal dimes discussed
RELEMR): Fuen
ershock sstern Spai
z(2) and A. T
ance Sismiqsity of Jaén,
io-temporalSpain. This
of the freqe of aftersh
computed p-e temporal d
ergy partitiohe main shock sequencthe mbLg 4.
mbLg 4.8, La tion integramary fault s% for the Mthe Lorca 2
ension, the d as well.
ngirola (Malaga)
sequencesin
Talbi(1)
que, CRAAG Jaén, Spai
behavior ostudy focu
quency-maghocks. The -values ran
decay of afte
oning. It suock, and once. For exa.8, Mula 19Paca 2005
al, and then segment toMula 1999, 2011, and 6
b-value an
), Spain 2013
s in
G. in
of eleven aftuses mainlygnitude distcomputed bge betweenershocks.
ggests thatly a relative
ample, we o999, an 88%5, earthquak
used to deo the total s
61% for th63% for the
nd the p-va
22
tershock y on the tribution, b-values n 0.75 ±
t a large ely small obtained % during kes. The erive the slip. For e Bullas e Gador
alue are
XXXV UNEReducing
De
Algeria Europedestrucaccelercurrentland contype, earecordsderive a The coattenuaBoore Tanakaaccordi Spectraconstituhomogedata onmodel. The obtto 0.32larger mspectragood ag
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rivation of
Cent
is located an plate.
ctive moderarographs nely a very ricntains inforarthquake a
s (2<Ms<6.9an attenuati
nsidered sation, and ge(1981), is
a, 1992]. Tng to magn
al attenuatiouted of Aleneously prnly, called lo
tained resu (regional
magnitude aal acceleratiogreement w
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tre National
on the norNorthern Aate-to-stronetwork (335ch data banrmation regand station9 and 7< Dion relations
pectral atteeological sita two-step
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lts show thadata), and and lower dons are stu
with classica
Workshop ended Mediterra
attenuatioegional str
Na
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rthern edgeAlgeria is ng earthqua5 stations), nk. From tharding the s locationshypo <160 Kship for Alg
enuation mote conditionp inversionation modeocentrale dis
re derived fong motionTwo models, and the s
at the PGA the local m
distance. Thdied and do
al published
anean Region (R
on relatiorong motio
asser Laoua
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s …etc. ActKm). One oeria.
odel accouns. The regr [Fukushiml describesstance, and
from 1155 hn records s are then
second one
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RELEMR): Fuen
n for Algeon databa
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rican plate, seismic arepast. Since arthquakes nk, a strong
(Ms), the tually, the cf the most
nts for georession met
ma and Tas the evolud category o
horizontal c(55%) an
studies, the consider t
deviation derestimates t
values betit any bias. tion attenua
ngirola (Malaga)
eria basedase
nie Parasism
which is cea that exthe installawere recormotion cat
hypocentracatalog conimportant a
ometrical spthod, introd
anaka, 1990ution of spof the site.
componentsnd Europeae first one he whole d
ecreases frothe predicteween obseThe inferre
ation laws.
), Spain 2013
on local a
mique
converging xperienced ation of the Arded and cotalog is esta
al distance, ntains arounapplications
preading, auced by joy0; Fukushi
pectral acce
s. The dataan recordsconsiders A
data called
om 0.33 (loced accelerarved and p
ed regional
23
and
with the several
Algerian onstitute ablished the site
nd 1000 s was to
anelastic yner and ma and eleration
sets are s (45%) Algerian regional
cal data) ation for redicted law is in
XXXV UNEReducing
Quarry
Groundproblempipelineenvironground (NCC) sof the qcompreof Surfaquarry baccordienvironScaled Pressuranalysisdamage
ESCO-RELEMREarthquake Los
y Blasts A
S
d vibrations ms in the ques. Thereformental effevibration
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essional wavace Waves blasts. The ng to the mental effeDistance (
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R International sses in the Exte
AssessmePipelin
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Seismologyof
induced byuarrying indre, a vibratiects of blasmeasuremeof Helwan csts on the ves and the(MASW) aresults demInternationa
ects is 650(SD) relatiot) formula (Amum allowaof 12.5 mm/
Workshop ended Mediterra
nt and Thes, South
Ela A. Moh
y Departmef Astronomy
y blasting iustry and mion control sting in quaents inducecity, Egypt. oil pipelinee shear wavare used to monstrate thal Building m, followi
onship (PPVAir Blast = able chargesec at the c
anean Region (R
eir Enviroeast of He
amed and A
nt, the Natioy and Geop
n the cememay cause sstudy playsarries. Thised by blasThe aim ofs of SUMEve velocity evaluate th
hat, the closCode (IBC
ng the dedV = 440.64152.87 × S
e weight perclosest site
RELEMR): Fuen
onmental Ielwan City
Adel M. E. M
onal Reseaphysics, Egy
ent quarriessevere dams an import research
sting at thef this study ED Companobtained fro
he closest ssest site of C) and theduced Peak4 × SD-1.22
SD-0.071) in dr delay was of the SUM
ngirola (Malaga)
mpacts oy, Egypt
Mohamed
arch Instituteypt
s are one omage to the
ant role in paper pres
e National is to invest
ny. The seom the Mulsite of the twthe two pip
e safe distak Particle V25) in mm/sB. In the ligfound to be
MED pipeline
), Spain 2013
n the Nea
e
of the fundnearby utilithe minimiz
sents the reCement Ctigate the inismic refraclti channel Awo pipelineelines is of ance to avVelocity (PPs and the Aght of the pre 591 m/kg0
es.
24
rby Oil
amental ities and zation of esults of
Company nfluence ction for Analysis
es to the class B,
void any PV) and Air over rediction 0.5 with a
XXXV UNEReducing
Nor
(1)Dep
North AdevastaconsideNorth-Athe besGroup 2000 udiverse Sudan) In this pstudy, bmaps oThen, win termsaccelerinforma Referen Mou
CheJ., KG.FSeis10.1
ESCO-RELEMREarthquake Los
rth African
pt. of Physic(2)Centre
Africa is oating earthqerable econAfrican Sciest seismic hfor Earthqunder the agroup of
.
paper, we bby the grouof North Afrwe describes of the distration. Thesation necess
nce urabit T. Abeddadi A., CKsentini A.,
F., Peresan smic Hazar1007/s1095
R International sses in the Exte
n Group fohaz
Mo
cs and Cente de Reche
C
ne of the quakes, somnomic damaentists to joihazard assuake and Taegis of ICT
North Afric
briefly presup, that aimrica includine the seismotribution of se thematicsary for the
bou EleneanChourak M., Jabour N
A., Romdrd Assessm
50-013-9375
Workshop ended Mediterra
or Earthquzard asses
urad Bezze
tro de Geoferche en AsCRAAG, Bou
most eartme of themage to the rn their effo
sessment aTsunami stuTP (Triestecan countr
ent the nated at produ
ng five counotectonic comaximum dc maps absustainable
n K. M., Aya., ElGabry M., Magrin Ahane N., Vment in No5-2
anean Region (R
uake and Tssment in
eghoud(1)and
física de Évtronomie, Auzaréah, Al
hquake-prom tsunami-trregion. Thurts in ordernd risk mitudies (NAG
e, Italy). It ries (Moroc
ure, missioucing Neo-dntries: Moroontext of Nodisplacemebout earthqe social and
adi A., BenoM. N., Harb
A., MaoucheVaccari F.aorth-Africa,
RELEMR): Fuen
Tsunami sn North Afr
d Assia Har
vora, ECT, UAstrophysiqugiers, Alger
one areas riggering, ins it was imr to capitalizigation of t
GET, previois structure
cco, Algeria
n and objedeterministiocco, Algerorth Africa ant, maximuuake haza
d economic
ouar D., Bebi A., Hfaiede S., Meghnd ZuccoloJournal of
ngirola (Malaga)
studies anrica
rbi(2)
University oue et Géopria
of the Menflicted heaportant andze on any sthe region. ously NASGed as a paa, Tunisia,
ctives of NAc seismic h
ria, Tunisia,and present m velocity, rd constitudevelopme
en Suleman dh M., Husraoui M., O
o E., 2013.f Seismolog
), Spain 2013
nd the seis
of Évora, Pohysique,
editerraneanavy loss of d necessarysynergies aThe North
G) was fourtnership aLibya, Eg
AGET and hazard asse, Libya, andthe maps oand designte importan
ent of North
A.,Bezzegssein H. M.,Ousadou F. Neo-Detergy, accepte
25
smic
ortugal
n. Many life and
y for the iming at African
unded in among a ypt and
the first essment d Egypt. obtained n ground nt basic Africa.
houd M. , Kacem , Panza rministic ed. DOI
XXXV UNEReducing
Propo
The resRC infilinterior type of countrieinspectdevelopvulneraassessmbuildingground methodconstruarea grmediumclassifiehorizonand ovebuildingAnalyticinfill wausing nanalysisBasic Cdesign modifielimit CI considebuildingimplies Assessmain cit KeywoRapid analysis
ESCO-RELEMREarthquake Los
osing an Info
H
Jo
sidential builed frames.frames bou
f constructioes, is not weion and anapment and ability of exment methogs as adeq
motions ad is only ccted betweroups wher
m rise (4-6 sed into regtal irregulaerhangs ongs were ancal computealls to the lanonlinear dias was carri
Capacity Indbase shears to arrive value. A C
eration coug is classifie
that the bment formsties in Jorda
rds assessmens; capacity
R International sses in the Exte
ndexing Mor Existing
Hanan S. Al-
ordan Unive
ilding stock The exteriound masonon, which cell-defined. alysis requiapplication
xisting resod is a rapiduate, in ternd thereforconcerned
een 1990 anrein each astories) heiggular and irities (setba the seisminalyzed to er models
ateral resistaagonal comed out to adex (BCI) war value (c
at the CapCapacity Ind
ld experiened as in nebuilding uns were desigan.
nt; reinforceindex.
Workshop ended Mediterra
Method forg Residen
-Nimry, Sad
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k in Jordan or frames ary panels bcould only Identificatires enormo
n of an indidential stod and yet sirms of humre require fwith the
nd 2005. Barea groupght categorirregular suacks and reic performa
arrive at of the reprance and st
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nce moderaeed for furtnder considgned and u
ed concrete
anean Region (R
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ddam H. Qe
nt of Civil Eence and T
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ous time andexing methone-concretimple evalu
man life safefurther detalocal low
Buildings su is further ries. Under ubcategoriee-entrant c
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resentative tiffness of ttruts. Using
e capacity ced for each ). This wasx (CI) of theelow the limate damagether detailederation coused to eva
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RELEMR): Fuen
ssessmene-Concrete
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ngineering,Technology,
ed by a locawith stiff stoncrete blocksin Jordan a
mically inaded effort. Thhod for rapte building
uation methoety, or thosailed evaluaand mediubject of theclassified each area-
es. The efforners), ve
al buildings parametersbuildings whe represeng SAP2000curves of thbuilding us
s later mode building wmit value inde during and evaluatio
ould experiealuate twent
frames; sto
ngirola (Malaga)
t of Seisme Building
R. Resheid
, Irbid, Jorda
al type of cone-concretes. Seismic and some equate strucis study is pid evaluats in Jordaod that canse that mayation. The um rise ree study areinto low ris
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are examins of the e
were built. ntative buildN, static nohe represensing its capadified using
which is to bdicates thatn earthqua
on whereasence minoty two samp
one-concret
), Spain 2013
mic Vulnergs
dat
an
onstruction e walls whevulnerabilityof the neigctures with concerned ion of the an. The p be used toy be at riskproposed i
esidential b classified se (1-3 stoegory, builde locally dularities (soned. A totalevaluation Contributiondings was monlinear (puntative buildacity curve g five perfobe comparet the buildin
ake and he a higher Cr damage, ple building
te infills; p
26
rability
of weak reas the y of this ghboring detailed with the seismic
roposed o identify k during indexing buildings into two
ories) or ings are ominant
oft story) l of forty method. n of the modeled ushover) dings. A and the
ormance d with a
ng under ence the CI value
if any. gs in two
pushover
XXXV UNEReducing
This proEuropeat An-Nthe Eurand theEUCENcentre collabovisibilitywill be experiegraduatSASPA By deverole willinternata reseathe fieldnetworkactivitie At the preparementionin the encouraacquirinincreas Improveinitiative Note:
ESCO-RELEMREarthquake Los
Jalal Al Dab
oject aims tan Researc
Najah Nationropean Cene Institute fNTRE will lein the fieldrate with UPy of UPDRRfundamenta
ence of IUSSte courses
ARM activitie
eloping a col be fundamtional reseaarch infrastrd of scientifiks of researes will lead U
national leved to respned target wfield of eaage researng and parte their ince
ed competes of genera
ProjeProjeRisk Proje
R International sses in the Exte
Seis
bbeek(1), Pa
to reinforce ch Area. Urnal Universntre for Trafor Advanc
ead UPDRRd of seismiPDRRC to dRC at the nal for the trS in the fielwill represe
es.
omprehensmental in mearch activitieructure and ic technologrchers and UPDRRC to
vel, an enhpond to eawill be pursurthquake echers to coicipating in ntives to co
itiveness oal public aw
ect acronym: SAect full title: "SupMitigation.
ect funded by Eu
Workshop ended Mediterra
smic RiskSAS
aola Ceresa
(1)UPDRR(2)EU
(3)IUSS
the cooperrban Planniity (NNU) in
aining and Rced Study oRC to becomc risk mitigdevise a res
national andraining activld of earthqent a distin
ive researceeting the nes. The prodeveloping
gy and caparesearch in
o a fruitful c
hancement arthquake eued by enhaengineeringompete inteEU Framew
ontinue their
of NNU, crwareness ar
ASPARM pport Action for
uropean Comm
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k MitigatioSPARM Pro
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RC TEAM, UCENTRE, S University
ration with Eing and Disn Palestine Research inof Pavia (Ime a globagation and search stra
d internationvities for stuuake enginguishing fe
h strategy, national socoject activitieg and enhanacity buildinnstitutes. In cooperation
of capabilengineeringancing the . Furthermoernationallywork projecr research a
eation of nre some of t
Strengthening P
ission through t
RELEMR): Fuen
n in Palesoject
o Germagno
Palestine Italy.
y, Italy.
Europe’s nesaster Risk
is coordinan EarthquaUSS) in Itally competitdisaster mtegy capab
nal levels. Tudents and
neering and eature of the
the significacio-economies are idenncing internng, i.e. hum
an internatwith EU.
ity will ensg needs ocapability oore, a highy in terms cts related tactivities in
networks othe expecte
Palestinian-adm
the SEVENTH F
ngirola (Malaga)
stine
oli(2) and Ba
eighbours inReduction
ating the proke Engineealy. The sutive and exp
managemenle of increa
The supportyoung reseengineerin
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ant strengthc challenge
ntified with tational cooan resourcetional frame
sure PS to f the loca
of UPDRRCher visibilityof scientific
to seismic rPS.
of researched results of
ministrated Area
FRAME WORK
), Spain 2013
arbara Borzi
n the contexCenter (UPoject, suppoering (EUCEupporting aperienced rt. EUCENT
asing the scoting action earchers. Tg seismolo
onal vocatio
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operation wies, researchework the p
establish al communi
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centres, pf SASPARM
as capabilities fo
PROGRAMME
27
i(2)
xt of the PDRRC) orted by ENTRE)
action of research TRE will ope and of IUSS
The long gy post-
on of the
PDRRC onal and creating th PS in h policy, roposed
a centre ity. The g activity RRC will ce (e.g., ons) and
promote M.
or Seismic
E.
XXXV UNEReducing
Earthq
Bog
The impin 200commuon-line disastrothreshowarningto be approprdecide EEW syCorpora In additand setestimat
ESCO-RELEMREarthquake Los
quake Ear
azici Univer
plementatio1. Satellitenication bedata from t
ous earthquold time dog algorithmsimplementeriate servo proper acti
ygnal are thation (IGDA
tion, work dtting up of e earthquak
R International sses in the Exte
rly Warnin
rsity, Kaind
on of the eae based atween the rthese statiouakes. A siomain ampls such as Ped as well.
shut-downion based ohe facilities AS). Recent
done over thnew applicke losses in
Workshop ended Mediterra
ng and RaKO
Ali Pina
illi ObservaIst
rthquake eaand fiber remote statins is used imple and itude levels
PRESTo and. The early
n systems on the alarsuch as Faly construct
he last decaations for e
n quasi-real
anean Region (R
pid Post-EOERI, Turk
r and Musta
tory and Eatanbul, Turk
arly warningoptic dataons and theto provide rrobust Earls named ad Virtual Sey warning of the recerm level. Aast Train anted tall build
ades regardearthquake time after a
RELEMR): Fuen
Earthquakkey
afa Erdik
arthquake Rkey
g system (Ea transmisse base statireal time waly Warning as CAV is eismologist
sygnal is eipent facilAmong the nd Tube Tundings, elect
ding the devrapid respo
an earthqua
ngirola (Malaga)
ke Assess
Research In
EEWS) in Ission systeion at KOERarning for e
algorithm, implementerunning unto be com
ities, whichprospective
nnel, Istanbric power p
velopment oonse systeake are elab
), Spain 2013
ment Stud
stitute (KOE
tanbul comms are uRI. The con
emerging pobased on
ed. Regionder Seiscom
mmunicatedh will autome end userbul Gas Dislants.
of new appms that funborated.
28
dies at
ERI),
menced sed for ntinuous otentially
specific nal early mp3 are
d to the matically rs of the tribution
proaches nction to
XXXV UNEReducing
Algeria NasserDirecteuChef deSismiquCentre en GénRue KaDey, AlTel: +21Fax: +2E-mail:
MohamCherchCRAAGBP63 BAlgiers,Tel: +21Fax: +2E-mail:
Cyprus Eleni GDirectoGeolog1415 NTel: +35Fax: +3E-mail: SteliosSenior GGeolog1415 NTel: +35Fax: +3E-mail:
ESCO-RELEMREarthquake Los
a
r Laouami ur de Rechee Division due National deie Parasism
addour Rahiger, Algérie13 21 49 55
213 21 49 5nlaouami@n_laouami@
med Hamdaeur
G Bouzaréah 1, Algeria 1 90 44 54/
21 90 44 58 mhamdachm.hamdach
s
Georgiou Mr ical Survey icosia, Cyp57 224 092
357 223 168director@g
s NicolaidesGeological ical Survey icosia, Cyp57-2240926
357 223 168snicolaides
R International sses in the Exte
erche e Recherch
e Recherchemique, CGSim, BP. 252e. 5 41 5 36
ache
16348
55
Morisseau
Departmenrus 13
873 gsd.moa.gov
s Officer Departmen
rus 60 873 [email protected]
Workshop ended Mediterra
List o
he Aléa
e AppliquéeS 2, Hussein
g om
l.com dz
nt
v.cy
nt
a.gov.cy
anean Region (R
of Partici
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RSECcCB9FTE
RELEMR): Fuen
pants
ordanis DiSeismologisGeological S1415 NicosiCyprus E-mail: idim
Egypt
Hatem OdaPresident National Reand GeophyHelwan Cairo, EgypE-mail: hate
hate
Abuo El-ElaProfessor, Head of SeiNational Reand GeophyE-mail: amin
abuo
El-Sayed MEgyptian GeAuthority 3 Salah SaleAbbasiya, CTel: +202 68E-mail: saye
France
Remy BussSecretary GEuropean-MCentre c/o CEA, BtCentre DAMBruyères le 91297 ArpajFrance Tel: +33 169E-mail: Rem
ngirola (Malaga)
mitriadis st Survey Depa
itriadis@gs
ah
esearch Instysics - NRIA
pt emodah@nremodah@ya
a Amin Mo
smology Deesearch Instysics [email protected]@h
Mohamed Seological Su
em Road Cairo 1151782 8013 edsalem200
su General Mediterranea
. Sâbles M- Ile de Fra
Châtel jon Cedex
9267814 my.BOSSU@
), Spain 2013
partment
sd.moa.gov.
titute of AstrAG
riag.sci.eg ahoo.com
ohamed
epartment, titute of Astr
ci.eg hotmail.com
Salem urvey and M
7, Egypte
00@hotmai
an Seismol
ance
@CEA.FR
29
.cy
ronomy
ronomy
m
Mining
l.com
ogical
XXXV UNEReducing
Gilles MSeismoMediterc/o CEAIle de F91297 AFrance E-mail : Pascal Head oCommisEnergiele-Chât91297 AFrance E-mail : German AngeloSeismoGFZ GeGeoscie14473 PGermanE-mail: Greece FilippoHead oSeismoTechnoCrete School Environ3 RomaCrete, GreeceE-mail:
ESCO-RELEMREarthquake Los
Mazet-Rouxologist of therranean SeiA, Bt. Bard France BruyArpajon Ced
: mazet@em
Roudil f CENALT ssariat à l'Ees Alternativel Arpajon Ced
: pascal.rou
ny
o Strollo ologist (GEOerman Reseences Potsdam Brny strollo@gfz
e
os Vallianatf the Labora
ology ological Edu
of Natural Rnment anou Str., C
e fvallian@ch
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x e Europeansmological Centre DAM
yères le Châdex
msc-csem.o
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dex
OFON) earch Centr
randenburg
z-potsdam.d
tos atory of Geo
ucational Ins
Resources
Chalepa, Ch
hania.teicre
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mique et auLDG Bruyèr
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lias PapadLaboratory oDepartmentNatural ResTechnologicCrete GR-73100 Chania, GRTel: +30-23Email: ilias@
Nikolaos SDirector of Rnstitute of G
National ObLofos NimfoGR-118 10, Athens, Greece E-mail: nme
Israel
Rami HofstHead SeismGeophysicaP.O.B 182, srael
E-mail: ramrami
Vladimir PiSenior ReseSeismology GeophysicaP.O.B 182, srael
E-mail: vlad
Andrei PoloGeophysicaP.O.B 182, srael
E-mail: andr
ngirola (Malaga)
opoulos of Geophyst of Environsources cal Educatio
REECE 10-23028
@chania.tei
. Melis Research Geodynamicbservatory oon,
Thissio,
tetter mology Divisal Institute oLOD 71100
[email protected] hof@yahoo
nsky earcher Division
al Institute oLOD 71100
@seis.mni.
ozov al Institute oLOD 71100
re.user12@
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