ࡱ> #& !" 'bjbj ;dd308|7`n/ !!!! #v#$#^^^^^^^$b[e_# # ###_!!4_/+/+/+#!!^/+#^/+/+ ThX!p-?'rV:^`07`V2e'etXXpeNY|##/+#####__)###7`####e######### : INVESTIGATIONS OF THE EFFECTS OF TOPOGRAPHIC/BATHYMETRIC MASSES AND CRUSTAL PARAMETERS IN GRAVITY FIELD MODELING Matej Varga1 `ime Sko i2 Tomislav Baai1 1 Faculty of Geodesy, University of Zagreb, Ka ieva 26, Zagreb, Croatia,  HYPERLINK "mailto:mvarga@geof.hr" mvarga@geof.hr 2 Geodezija d.o.o. `ibenik, Petra Preradovia 4, Zagreb, Croatia ABSTRACT Topographic and topoisostatic reductions of gravity field measurements are important in geodesy and geophysics. Reductions filter high frequencies from gravity which are then used in geoid modelling or investigations of the Earths structure. Practical computations of reductions are performed using digital elevation/bathymetric models as input data and some approximation scheme of the Earths structure. The main parameters describing the Earths structure are crustal, mantle and water density, density contrast, and Moho depths. Traditionally, standard global values for parameters are used which in local areas significantly differ from reality. As Earths topography and structure largely varies, it is of interest to know the effects and differences caused by using different input models and parameters describing the Earths topography and structure. Results presented in this paper are topographic and topoisostatic corrections on gravity anomalies and geoid undulations calculated for the wider Croatian area using GTOPO30, GMTED2010, GEBCO2014, SRTM15+ and SRTM30+ digital elevation and bathymetric models and several arbitrarily chosen parameters describing the Earths structure. The study area is suitable because it includes topographic changes from simple and flat to mountainous and complex terrain. Differences between solutions will point out importance of appropriate selection of the input models and crustal scheme. Keywords: gravity reduction, gravity anomaly, geoid undulation, topographic masses, digital elevation models, geoid undulation Introduction Topographic and topoisostatic reductions are used for reduction and filtering of the gravity measurements performed on the Earths surface. In the spectral domain gravity reduction removes short wavelengths caused by topography masses from the gravity signal. According to [1] 2% of the geoid undulation spectrum and 34% of gravity anomalies spectrum is caused by topographic masses. Reduction of topographic masses has three main aspects: selection of the reduction method, selection of the DEM/DBM models and selection of the crustal models (or parameters) of the Earths crust. Reduction method may be Bouguer, topo-isostatic, Helmert, Residual Terrain Modelling (RTM), etc. Crustal models or parameters of the of the Earths crust may be 1, 2 or 3 dimensional, therefore it may be represented with constant density value (crust density 2.67 g/cm3) in 1D, with lateral (surface) density model in 2D or with layered model in 3D. It is of interest to know what differences in modelling of the gravity field cause different digital elevation and crustal models. Theoretical background Earth has layered structure that may be approximated from the very simple (constant values) to the more realistic layered schemes. The most significant layer for gravity field modelling is lithosphere which includes all topographic masses from the surface down to the Mohorovi i discontinuity. Lithosphere consists from the crust and upper mantle. Crust on the continent is from 20-70 km thickness with varying densities from 2.7 to 2.9 g/cm3, whereas crust on the ocean has thickness from 5 to 8 km with average density of 3.0 g/cm3. The mantle is layered below crust and has average density around 3.27 g/cm3. IT is obvious that these average values are best global approximates which can significantly vary regionally and locally. Earths gravitational potential in a point P is [2]:  Where  QUOTE   is gravitational potential of topographic masses,  QUOTE   is Newton gravitational constant,  QUOTE   crustal density,  QUOTE   volume and  QUOTE   distance between two masses. In rectangular coordinate system gravitational potential is:  Where  QUOTE   represents gravity potential of Bouguer plate, while  QUOTE   is terrain correction. In planar approximation Bouguer effect on gravity is  QUOTE  , where  QUOTE   is the height of the computing point. Integral for terrain correction may be calculated by equation [3,4]:  Practical computations of the terrain correction are performed with digital elevation/bathymetric models where Earth topography is divided into prisms and effects in each computational point is calculated as the sum of all prisms inside some radius around the point. For evaluation of the above equations, beside heights H that are taken from the digital elevation models, crustal density  QUOTE   must be approximated and chosen. Objectives and methodology General objective of this study is to investigate and assess differences in gravity field modelling that exist because of the wide possibility of using different input models and parameters. This is done through following steps: Computation of the complete Bouguer effect using different digital elevation models: SRTM3, SRTM15+, SRTM30+ [5], GMTED2010 [6], GEBCO2014 [7] and GTOPO30 [8]. SRTM3 has the highest accuracy therefore its results are taken as reference (most accurate). Computation of the complete Bouguer effect with different constant density values of the Earths crust. Crustal density values for testing were selected as the mean values from geophysical models CRUST1.0 and EPCRUST. Computation of the Airy-Heiskenen topoisostatic effect using different constant values for depth of condensation and crust-mantle density contrast. These analysiss are investigated on geoid undulations and gravity anomalies that are gravity field functionals of particular interest in geodesy and geophysics. Test-area for all computations is the Republic of Croatia. Results Comparison of complete topographic reduction for geoid undulations and gravity anomalies computed with different DEMs is shown in  REF _Ref479694870 \h Table 1. For the study area complete topographic reduction for geoid undulation is around 96 cm indicating huge impact that this reduction may have on computing geoid undulations. In terms of gravity anomalies complete topographic reduction amounts for around 37 52 mGals. Table  SEQ Table \* ARABIC 1. Complete topographic reduction on geoid undulation and gravity anomaly using different DEMs N [m]g [mgal]DEMMaxMinMeanSt. devMaxMinMeanSt.dev.SRTM3 + GEBCO201428.71-2.328.645.35280.9-83.336.250.6SRTM15+32.28-1.539.855.91286.4-83.337.552.2SRTM30+30.05-2.009.055.55289.3-83.138.252.8GMTED201031.04-1.819.435.72285.0-83.337.151.7GEBCO201430.12-1.999.065.56289.1-83.038.453.0GTOPO3029.92-1.969.045.54289.6-83.138.052.5  REF _Ref479695506 \h Table 2 shows differences between reference solution with the most accurate SRTM3 and other DEMs. In terms of geoid undulations range from 1 to 63 cm with mean and standard deviation values from 4 cm to 13 cm. Differences between reference solution in gravity anomalies show that differences of upt to 30 mGals may be expected in reductions. Mean value of differences are around 1-2 mGal. Table  SEQ Table \* ARABIC 2 The differences between complete topographic reduction computed using different DEMs and reference (best) solution computed using SRTM3+GEBCO2014 DEM. N [m]g [mGal]DEMMaxMinMeanSt. devMaxMinMeanSt.dev.SRTM15+0.630.000.130.1020.1-6.71.42.8SRTM30+0.25-0.020.040.0431.1-8.82.03.6GMTED20100.42-0.010.080.0725.6-17.91.02.1GEBCO20140.30-0.010.050.0435.4-9.72.24.0GTOPO300.25-0.050.040.0444.1-21.71.83.7 Table 3. shows the differences between topographic reduction using variable constant crustal densities and standard crustal density 2670 kg/m3. The differences are huge both for gravity anomalies and geoid undulations. For geoid undulation they are approximately are around 40 cm and for gravity anomalies 2 mGals. Table  SEQ Table \* ARABIC 3 Differences between complete topographic reduction computed using variable crustal density values and standard crustal density N [m]g [mGals]  [kg/cm3]MaxMinMeanSt. devMaxMinMeanSt.dev.27901.35-0.250.390.2613.0-6.01.62.528351.86-0.350.540.3617.9-8.32.33.4  REF _Ref481495231 \h Table 4 shows differences between Airy topoisostatic reduction using variable compensation depth and standard crustal depth (27 km). In terms of geoid undulations mean differences are 0.07 for 30 km and 0.34 m for 23 km, whereas in terms of gravity anomalies the differences are 0.3 mGals for 30 km and 1.4 mGals for 23 km. Table  SEQ Table \* ARABIC 4 Differences between Airy topoisostatic reduction computed using variable compensation depths (T) and using standard crustal depth N [m]g [mGals]T [km]MaxMinMeanSt. devMaxMinMeanSt.dev.300.3-0.080.070.062.9-2.20.30.8231.38-0.410.340.313.5-11.21.44.0  REF _Ref481495878 \h Table 5 shows differences between Airy topoisostatic reduction using variable crust-mantle density contrast and standard crust-mantle density contrast 450 kg/cm3. In terms of geoid undulations mean differences are from 0.01 to 0.04 m, whereas in terms of gravity anomalies mean differences are from 0.0 mGals to 0.1 mGals. Table  SEQ Table \* ARABIC 5 Differences between Airy-Heiskanen topoisostatic reduction computed using different constant crust-mantle densities and using standard crust-mantle density contrast NgMaxMinMeanSt. devMaxMinMeanSt.dev.4450.0900.010.010.9-0.30.00.24810.1500.020.021.6-0.50.10.35200.2100.030.032.2-0.60.10.46000.3100.040.053.2-1.00.10.5 Conclusions In this study, topographic and topoisostatic reductions were investigated. Different input models and parameters were used in calculations of reduction on geoid undulations and gravity anomalies. It was found that usage of different DEM/DMB models in reduction may cause differences in geoid undulations from 4 to 10 centimeters and for gravity anomalies for 1 to 2 mGals. From the perspective of improvement in geodetic measurements the effects should be accounted for when selecting a DEM/DMB in gravity field modeling. Another significant effec  2 4 6 8   0 2 4 6 8   " + 5 : O V X h n y #&hh>gh>gB*ph!!!hp.B*ph!!!h hp.B*ph!!! hu"hp.h'b hyhp.h hp.5\jhp.0JUhBhp.0Jjhp.Uhp.hp.5h hp.H* h hp.hp.8 6 4 /1gdygdygdp.#gdp."gdp. gdp. >QL]oen,-456789xjhp.hp.EHUjlhp.hp.EHUjlhp.hp.EHUj*<hp.hp.EHU hp.hp. hhp.jhp.hp.Uh?zy hp.6hA!hp.6h8Thyh h."hp.h'bh hp.5hp. h hp./9\]defghi{|  GHOyljЬhp.hp.EHUjzhp.hp.EHU hhp.j#hp.hp.Uh'bjhp.hp.EHUjhp.hp.EHUj hp.hp.EHUj_hp.hp.EHUjY/hp.hp.EHUjhp.hp.EHU hp.hp.jhp.hp.Uhp.'OPQRST(-/01rstϗό~vqj]jlhp.hp.EHU hT:hp. hp.6hT:hp.6 hc^nhp. hhp.jZhp.hp.Uhljhp.hp.EHUjhp.hp.EHUj{yhp.hp.EHUjRChp.hp.EHUhp.j*hp.hp.EHUjhp.hp.U hp.hp.jhp.hp.EHU$RVaept/"""""""""""####$$ $ $$$$$$$ݷݮ®ݙvv h?zyhu5B*CJaJph#h?zyhp.56B*CJaJph h?zyhp.jhp.UmHnHuhp.mHnHuj hp.Ujhp.Uhl h uRh?zyh?zyh'bhp.jhhp.hp.EHUjhp.hp.U hp.hp.+ Q!R!/"7"##$$$$ $Ifgd?zygdp.gdygd?zy & Fdgd?zygd?zygd?zygdp.$$$H%J%n%%%%&&!&'&-&M&N&X&&&&&&&&&&& ' ' ''''(((((((((I)J)K)O)*˸˯˫ïä˙v h?zyh. 5B*CJaJph#h?zyhp.56B*CJaJphh?zyhp.CJaJ h0hp.h\fhp.mHnHujhp.Ujhp.Uhp.h?zyhp.B*CJaJph h?zyhp.5B*CJaJph h?zyhp.h?zyhp.56.$$$$%%%&%.%8%H%J%n%z%yyyyyyyyytyyFf $Ifgd?zy|kd$$Ifl9F  ccc t6    44 lBapyt z%%%%%%%%%%%%%&&&&&&!&'&-&2&7&=&C&H&M&Ff8Ff' $Ifgd?zyM&N&X&^&d&i&n&t&z&&&&&&&&&&&&&&&&&&&FfkFfZ $Ifgd?zyFfI&&&&&&&((I)J)P)* $$Ifa$gd $$Ifa$gd $gdp.gdp.Ff| $Ifgd?zy ******r*t*****0+2+F++++++,.,/,l-m-s-t-------....$.&.*.,.ܸɸɸɸɸɸɥyg#h?zyh. 56B*CJaJphh?zyhp.56CJaJhOebmHnHuhp.mHnHujhp.Uh\fhp.h?zyhp.B*CJaJph h?zyhp.5B*CJaJph h?zyhp.h?zyhp.5CJaJ h?zyh. 5B*CJaJph#h?zyhp.56B*CJaJph(***&*.*8*H*P*X*b*r*t*~rffffrrrraFf $$Ifa$gd $$Ifa$gd kd$$IfTl9F^'ccc t6    44 lBapyt T t**************+ ++ +(+0+2+F+P+\+f+p+FfFf $$Ifa$gd $$Ifa$gd p+z+++++++++++++++, ,,,, ,&,*,.,/,FfFf $$Ifa$gd Ff $$Ifa$gd /,0,l-m-..&.<.>.V.^.[kd8$$IfTl,Fgccc t6    44 lBapyt T $$Ifa$gd $$Ifa$gd $gdp.gdp. ,.6.8.:.<.>.D.P.R.T.V...//^/`/b/d/////// 00011111˺җˈˈ˄|q|h|d`dd\Tjhp.Uhp.hJmhuh@(mHnHujh@(Ujh@(Uh@(h?zyhp.B*CJaJph h?zyhp.5B*CJaJph#h?zyh. 5B*CJH*aJph h?zyh\f5B*CJaJph h?zyhp.h?zyhp.5CJaJ h?zyh"15B*CJaJph h?zyh. 5B*CJaJph ^.f.p...............////&/0/:/D/Ff $$Ifa$gd Ff $$Ifa$gd $$Ifa$gd D/N/V/^/`/b/111112 $$Ifa$gd $$Ifa$gd $gdp.gd@(Ff $$Ifa$gd 1,1-1.1/11111111222222$2&2z2|222222$3&3(3T3V3X3ƵƵƎ}}n}njb^Sbj hUhjhUhh?zyhp.B*CJaJph h?zyhp.5B*CJaJph#h?zyhdu56B*CJaJph h?zyhp.h?zyhp.56CJaJ h?zyh"15B*CJaJph#h?zyhp.56B*CJaJphh?zyhp.CJaJhOebhduhp.mHnHujhp.Uhp. 22&2.262@2P2X2`2j2z2|2~rffffrrrraFf1 $$Ifa$gd $$Ifa$gd kd$$IfTl,FCccc t6    44 lBapyt T |2222222222222222333"3$3&344gddugdFgdp.Ff_ FfH $Ifgd $$Ifa$gd X3d3f3h3j33M4N4444444444444 5555L5T5z55555566 6b6d6ȿиЯЗ~m\~ h?zyhp.5B*CJaJph h?zyh5B*CJaJph h?zyhp.#h?zyhp.56B*CJaJphh?zyhp.B*CJaJphhmHnHuhOebmHnHu hp.hp.hp.mHnHujhp.Uhp.hduhdumH sH hhH*hFjhUhmHnHuh$455566666(686@6akd $$IfTlF f'f f t6    44 lBapyt T $$Ifa$gd $$Ifa$gd gd @6H6R6b6d6l6v6z66666666666666666777FfFf1Ff $$Ifa$gd d6l6666677L7N7V77777778899:tVuuuuugvovtvvvvvvx:yDyFyjy"zzŽͽͻͳūųzskshzh?zy] hzh?zyhzh mH sH hzh?zymH sH hzhymH sH hQomH sH h+e#mH sH hOebmH sH h>gmH sH UhV'mH sH h'bmH sH hTghmH sH hp. h?zyhp.h?zyhp.B*CJaJph h?zyhp.5B*CJaJph*77 7*727<7D7L7N7V7`7d7n7x7777777789VuvvgdQo%gdp.gdp.Ff6Ff $$Ifa$gd t is the effect of the constant crustal density. The differences that may arise while using different constants in geoid undulations are more than 30 cm while in gravity anomalies it is more than 2 mGals. For geophysical purposes, constants used in Airy reduction are also affecting solutions, especially selection of the compensation depth. Finally, topographic and topoisostatic reduction is a crucial step in processing of the highly quality gravity measurements, investigation of the Earths crust and determination of the precise geoid model. Therefore, the most precise DEM/DBM and crustal parameters for the research and particular computation area have to be carefully selected. REFERENCES [1] Schwarz, K. P., Data types and their spectral properties, International summer school on local gravity eld approximation, Beijing, China, 1984. [2] Hofmann-Wellenhof, B. and H. Moritz, Physical Geodesy, Springer Verlag, 2005. [3] Forsberg, R., A study of terrain reductions, density anomalies and geophysical inversion methods in gravity field modelling (No. OSU/DGSS-355). Ohio State Univ Columbus Dept Of Geodetic Science and Surveying, 1984. [4] Nagy, D., The gravitational attraction of a right rectangular prism. Geophysics, vol. 31/issue 2, pp 362-371, 1966. [5] USGS, Shuttle Radar Topography mission,  HYPERLINK "https://earthexplorer.usgs.gov" https://earthexplorer.usgs.gov, 2017. [6] Danielson, J. J., Gesch, D. B., Global multi-resolution terrain elevation data 2010 (GMTED2010) (No. 2011-1073), US Geological Survey, 2011. [7] Weatherall, P., Marks, K. M., Jakobsson, M., Schmitt, T., Tani, S., Arndt, J. E., ..., Wigley, R., A new digital bathymetric model of the world's oceans, Earth and Space Science, vol. 2/issue 8, pp 331-345, 2015. [8] USGS, 2017, Global 30 Arc-Second Elevation Data Set GTOPO30,  HYPERLINK "https://earthexplorer.usgs.gov" https://earthexplorer.usgs.gov.     17th International Multidisciplinary Scientific GeoConference SGEM 2017  HYPERLINK "http://www.sgem.org" www.sgem.orgvvxFy~zzw{||q}s}t}v}w}y}z}|}}}}}gdQogdQogdQo $a$gdygd}9gd9 $a$gd?zygdy%gdVb zzzzzzzzzzzzzzzz{!{"{#{O{P{n{o{u{v{w{x{y{{{{ôåtct\U\N hzhs hzhGjy hzh g hzh@0JmH nH sH tH hzh@mH nH sH tH %jhzh@UmH nH sH tH hzh>mH nH sH tH hzhG#mH nH sH tH hzhlmH nH sH tH hzhsmH nH sH tH $hzh?zyCJaJmH nH sH tH  hzhzh hzh?zyhzh?zy]{{{{|||| | |||||||||||||||||||| }!}"}#}麧zc-jhzh?zyCJUaJmH nH sH tH  hzhG#$h>hG#CJaJmH nH sH tH $hzhGjyCJaJmH nH sH tH $hzhG#CJaJmH nH sH tH  hzh hzh hzh g hzhshzhs] #}O}P}n}o}p}q}r}t}u}w}x}z}{}}}~}}}}}}}}}}}}}}}֮{wpd`XTXMX h:h:h:jh:Uh heS(h 5mHsH hpT\h hheS(hW hW H*h&hW hs$jhs$U$hzh`pCJaJmH nH sH tH $hzhG#CJaJmH nH sH tH (hzh?zy0JCJaJmH nH sH tH -jhzh?zyCJUaJmH nH sH tH $hzh?zyCJaJmH nH sH tH  Section Name }!"#$%&'$hzh`pCJaJmH nH sH tH hs$h}h:h h#h hpT\h#h#hdU  !"#$%&' $a$gdygdQogdQogdQo 9 0&P 1h:p. A!"#$%SS *<Dd H4  3 A"4 á4 16V=Gvρdvl ,b'qdt5@PLZ,Dn'qdt5@PLZ,PNG  IHDRTsRGB pHYsttfxYIDATx^\=V0,l 'XNihL M:J4PB& (`Bf$ٖ-=E'7!4Fcy___\)!#%e.@$uP()$@r +)$@r +)$@r +)$@r +)$@r +)$@r +)$@r +)$@r +)$@r +)$@r +)$@r +)$@ yoD+ï}pybuOPҬ"חjIX=~z2P 7ej@2~{i[B|op+Ffy_Cb?R gopRweO "bŠFkUUеӥ4҆ϝ9p4T v+Yۨt?1nKS"ٱv#H] t]t Dj?m4 ="ڷo$ooaU>J߼b+&hKa6o= Kjw) )-V9:)wEu[\[z\D:Sޔ1Zl3؅n2QC /OCɳD.BTsQ%کa2IZ!%$o'ZKQQ֗Kjƭ_:ܝ5.Z/ i|nBUJyUmaimD^|- O)sLA` {+A$dR/1F~7&xq%XU/y1PQK J෨7q-}o(y<_)؅4{"SWr]IENDB`0Dd .  3 A". ÷. 16VbRtXnC_.n<n&tXnC_PNG  IHDR !fsRGB pHYsttfxIDAT8Oc?5 %hH@oKCHmG0@eݞ`RPV" g5 iigڶ`QV a,F؀^Qq5'P]-ܙ2jB)]P UP= h+@3o{76PԿh¡ ^xc /Y5IENDB`0Dd .  3 A". ÷. 16VbRtXnC_.mn&tXnC_PNG  IHDR !fsRGB pHYsttfxIDAT8Oc?5 %hH@oKCHmG0@eݞ`RPV" g5 iigڶ`QV a,F؀^Qq5'P]-ܙ2jB)]P UP= h+@3o{76PԿh¡ ^xc /Y5IENDB`0Dd .  3 A". ÷. 16GbUPEɂf ;T >1n)PEɂf ;T >PNG  IHDR !fsRGB pHYsttfxIDAT8O 0 R@ }u]6`ģaԎ *?"8X@ĩ!E^J 빚_7z^ Zcl]Q IIҸ.%̗+JW9lj ~fncn 4/{z9'uMϻ\k{ޥqUNӠ1-yJ D32p5+IENDB`0Dd .  3 A". ÷. 16GbUPEɂf ;T >1Tn)PEɂf ;T >PNG  IHDR !fsRGB pHYsttfxIDAT8O 0 R@ }u]6`ģaԎ *?"8X@ĩ!E^J 빚_7z^ Zcl]Q IIҸ.%̗+JW9lj ~fncn 4/{z9'uMϻ\k{ޥqUNӠ1-yJ D32p5+IENDB`0Dd .  3 A". ø. 16ρbU.(rP1n).(rPPNG  IHDR !b%XsRGB pHYsttfxIDAT8Oc?!DHH~Th p*3њҷS-0C4Մ` V@^60E T f Qpgc Va*s16-UX9(EB`E`$:pO& k*IK@ t" ,&f10!y x`s вO|(<`K!#1IENDB`0Dd .  3 A". ø. 16ρbU.(rP1/n).(rPPNG  IHDR !b%XsRGB pHYsttfxIDAT8Oc?!DHH~Th p*3њҷS-0C4Մ` V@^60E T f Qpgc Va*s16-UX9(EB`E`$:pO& k*IK@ t" ,&f10!y x`s вO|(<`K!#1IENDB` 1Dd .  3 A". ø. 16dvb33zhIUoLB`n33zhIUoLPNG  IHDR!kGsRGB pHYsttfx%IDATHKU10 Ex@Y`Cx]݅ | wP<㹑$'?^40V`AӸ뾈 16dvb33zhIUoLOn33zhIUoLPNG  IHDR!kGsRGB pHYsttfx%IDATHKU10 Ex@Y`Cx]݅ | wP<㹑$'?^40V`AӸ뾈 16l b(A>_ok&?\n\nA>_ok&?\nPNG  IHDR!&sRGB pHYsttfxIDAT(Sc?`Bo8ܙhnOrӶh&x{1+-Uu0#Ls P~l]^ :j*иU?4PQ4QtQRH@`56S4J}DVZ/7IENDB`w0Dd T.   3 A". ÷. 16l b(A>_ok&?\nnA>_ok&?\nPNG  IHDR!&sRGB pHYsttfxIDAT(Sc?`Bo8ܙhnOrӶh&x{1+-Uu0#Ls P~l]^ :j*иU?4PQ4QtQRH@`56S4J}DVZ/7IENDB`WDd %\E   3 A"UE OE 16V=V1 + V2=dxdy0hp1ldxdydz+ dxdyhph1ldxdydz , bMk~ljJ#nMk~ljPNG  IHDR]sRGB pHYsttfxIDATx^];Z< )XY&m:&%](.-MdVGf/WCl0#]]J @,\wT @`,?@@,X3@@#Kt@Xp t`  K , `  %X:ƫ~{ž~"QFD|xX]@D $ՏۇX`ql%Ȧ)'[;οΨ!hY(y|8}>]YϢ^>oéԀ =f8 pS K` "ٕ0(ǯo /\ #D T%  'A7>BJV?_W s!/5u$O,\H쌀 X9g> 3X<ݬقt!8@@ ;&Ԯ\>})cmW߅'YZ-'X20$@oOoWү$\OlhXK<mWS6޼=|TkeAЇ',.u%pA y"@}*[HAˀ%! OXvu% #-p2]xh*QT@}BTHEk-j0C '@X-j0C ' v8AY'Y_#c]iȏ@!pL'yB@U7⑪f4uy` .d@t=/A%L xRaIK`BrB;F| uՌG*V̞d-#n `KGd#UkI7YIPa Ay_,xRj2# ⑪$ȢR`B5F|$r@`g In?`:ZTKœ K-:L=[橐]Sʠ a 2h U9%ovK3OJMoSER@*-, ɐ{k' Qd>'#$ J(|( YLɓ.o!I&穘 6IwNС$ݞf~ WGC UD N3فTt$ht)v|Aa2F`>XV$fbDqzE|XL%$Ι󡄧&QnvQ,*I&͞b1?^"l4WWe7T\^!ŏJjMj-ǽ@q=AjR"MWqyÛH\(V5WU/bGaLYnu}o(}cѯDBwp0 }j)/%BPɬV&FvNƫxRAh'+kR:,; ^cG#EmTe|s ^Qe}[ w_^THsM 6 δLǫx:H+{R-3ŬGe PE&1 5.7B,Gx>L8W^ŬsniҚ xeA*{[l(Yn$,4dϖTq48 ʼn&~}73F'BthTTH_8$ւ:& ^4,Gxk#G t3JQ-lx1U*K0TEd[ѕX9;o]e?Oin/K0XH ^#ZweG*11 >A9l>Jܫ/t[N0`)EuK Yȷ]~˼ɣћiWHBLlHUl3E1Y[ ^;i-{Q!Kݱ"wV]eFO) jD(j #_S(n)MaUxpXqob(XbO>=t-qjLVdvf«xR̝`9-S% kO7K5Պd:1mƟ:M5n)N"Bx|=@*lx%3$x"Eqٛ#%@om!zRM5J6l .ϘdG*UIWT>+QV~UKXx\{1"E"t|M2 R#ZSGTG[)%V iƼT!{vTyu|ږZT&G|"&H?͠fl(s;Y5%vw&/⑪9p;HK0nU+g՛qduDۨx uZ"N!w}o2+⑪f5RU(!柤k״\؃i|oN(H63E' oh=4E Pi8_y%Y!TciX"+(ݡЦSCCSk1 ,AhD! 05` b7@]k\IzO( GC0={l, O*\ӝN{z{ʼ`t^1␅t5cOB!PFt0T>oyvr,mUⵛ׹WtCv%L*1`- |ه51ZTkk\ֵ-s^4?>rAe}λ#'7pnY9b ^O*b|HȘm癶TZ@d]A̰@uOI;ffL@uMtzRJc$ &(S4n:;n䤝&<;Byx5e_Ԝ nE1b-cWҍidK06sԘ!Wy?ܿ]?~C?]UӳU)&ϱȖ B*>C)f)S^kK` RA[ xגg#;ԟX>K_ͪ\lԡKq bNUHC*(H& s!9.K?UU#geU&TV3k"K;jT"nj8Ԉ6Τ)qP zH]C BU #qq`w*$TJ1R7B TӨB`MbluKWzIÐݰ)%0 ɀ2g C!y""pK`M U=WIENDB`22Dd E0   3 A"0 0 16V1 bAf4xzJ?WKuznmAf4xzJ?WKPNG  IHDR![BlsRGB pHYsttfxIDATHKc?选t- 0m4HllOg0o`{ߞ`mq(DJTt*fK6[kl56e0GH3 8&`91 IMP9ĖYVJ 3ܙ_0aa Hxha"lލiӝ5 vh  hq A %hHBODiCq$$80m3(K;00\uf5J^ʁܭf$~|4=mbIENDB`22Dd E0  3 A"0 0 16V1 bAf4xzJ?WKunmAf4xzJ?WKPNG  IHDR![BlsRGB pHYsttfxIDATHKc?选t- 0m4HllOg0o`{ߞ`mq(DJTt*fK6[kl56e0GH3 8&`91 IMP9ĖYVJ 3ܙ_0aa Hxha"lލiӝ5 vh  hq A %hHBODiCq$$80m3(K;00\uf5J^ʁܭf$~|4=mbIENDB`(2Dd E0  3 A "0 0 16V2buӸ%_35U$7kFncuӸ%_35U$7PNG  IHDR!=sRGB pHYsttfxIDATHK :t^ܠ౽u Fw g>|!Z";QɜtBPTΚKśPYzսOscPs9[*eARb Iq4űN{lˎɱ=M:M 6 "-Dp 5f$&BLjrĮm _ r=Q`l J`Y:U RqmIENDB`(2Dd E0  3 A "0 0 16V2buӸ%_35U$7knncuӸ%_35U$7PNG  IHDR!=sRGB pHYsttfxIDATHK :t^ܠ౽u Fw g>|!Z";QɜtBPTΚKśPYzսOscPs9[*eARb Iq4űN{lˎɱ=M:M 6 "-Dp 5f$&BLjrĮm _ r=Q`l J`Y:U RqmIENDB`)6Dd 1  3 A "~1 x1 16δgB=2πGρhpb=Z)gCn=Z)gPNG  IHDR}$+cMsRGB pHYsttfxIDAThC1v1Ÿ8Ma9ĺGH&Ф~IΌfّ(V^[Ҍ>5NSSt5%PA^!P&j{^@U{eVWeZ^!P&j{^@LۧYx^er_W2,{eӴxݴn+jVG\hxn$/?!Ng7y8{fe܂! dNX7Q\B45Unfd5Zҙ5lM]ergGY?̻GvhVټC%ǼyEХZdx8C;^Qڂ7u0O娌:b7 LܹGIns2C!QO+'(;Uڦ-85!8W!t=l0HR≊kIl#dESUSG5o_}W-FRt70BYe53+&b{=Lg />;-Wk_1ј׽ 5OߐaK9W7_k8.GuV3Q-I#`X%"ʡ]'*來SDh*,ipɍTw w!, Z ^ʓ[in$-N؉E !d> dsbXrZضpa:LGC;ٻr6š̄V`Q-|Lτւ*iQ(m+ZTj&N?xiB|flA,q'HUޖU]a`s]kp8Pj3#R;MwrWמė^GDsN"waoy&uB$IENDB`)6Dd 1  3 A "~1 x1 16δgB=2πGρhpb=Z)gyn=Z)gPNG  IHDR}$+cMsRGB pHYsttfxIDAThC1v1Ÿ8Ma9ĺGH&Ф~IΌfّ(V^[Ҍ>5NSSt5%PA^!P&j{^@U{eVWeZ^!P&j{^@LۧYx^er_W2,{eӴxݴn+jVG\hxn$/?!Ng7y8{fe܂! dNX7Q\B45Unfd5Zҙ5lM]ergGY?̻GvhVټC%ǼyEХZdx8C;^Qڂ7u0O娌:b7 LܹGIns2C!QO+'(;Uڦ-85!8W!t=l0HR≊kIl#dESUSG5o_}W-FRt70BYe53+&b{=Lg />;-Wk_1ј׽ 5OߐaK9W7_k8.GuV3Q-I#`X%"ʡ]'*來SDh*,ipɍTw w!, Z ^ʓ[in$-N؉E !d> dsbXrZضpa:LGC;ٻr6š̄V`Q-|Lτւ*iQ(m+ZTj&N?xiB|flA,q'HUޖU]a`s]kp8Pj3#R;MwrWמė^GDsN"waoy&uB$IENDB`[2Dd E0  3 A "0 0 16hpbDŽl ]OtnDŽl ]OtPNG  IHDR$SsRGB pHYsttfx*IDATHKU;@Ϣ Jlhʖ .8oVJY+n~][~[~@6-7joVdkoeorNep~_&tyEk~X/8B FSJ]h~2&}z2pFPoV^)?U[IX}+|w*pv^dfN~sf黂NAF:!tO7Z껍8i(xH.oک 16hpbDŽl ]OtCnDŽl ]OtPNG  IHDR$SsRGB pHYsttfx*IDATHKU;@Ϣ Jlhʖ .8oVJY+n~][~[~@6-7joVdkoeorNep~_&tyEk~X/8B FSJ]h~2&}z2pFPoV^)?U[IX}+|w*pv^dfN~sf黂NAF:!tO7Z껍8i(xH.oک 16δgtc=|||xlny+r+ylnx+r-zarctanxyzr|x1x2|y1y2|z1z2 .b y,Ox+ n y,Ox+PNG  IHDR3Ӽ sRGB pHYsttfx IDATx^]=v8,y>skWiIl2]"m*7+ >HS' |>{@?*4@ 03@30 qc f{fu n ql.@č9 @13C=@7@`fg6`P|Hg~}{yC"4 }:c KD Z~~lUkm~R7璵OUL4W}s/jrj3u=!@`_/6]$Ք_7͕ϽlvS^a I@Bϋ.MO//o( 0{.#=GzE(/>Ql?}g!"^nmrGWU/wU8! R?Z⋒9ow__)9 <~\s'V6ZK~}ͥm[s ՛60NhUoJK4ٍ*De82ۯZlG.we)[ IzPy]EV_-F=Eo:قc!@D -PS$'R9ϑ{6OKr?zثh2 #nezMoƧGA*-aQ ZI`+ yãbv =cš"r<_{@7vB?m?me\ZVp^y9K\ XNvY7l_-&UV)lE'/Ozel2^2 O/qJA29 DBO O>voraYM4#j8PEW+s ,jnc{2x=svVow뻷oܓ<_$'>X/E+f6OM}3yEt=iSn݌9en'^A[+ZqiQQCKADUkl7 u^{h p*J.g { dduРbЅV,;q+߈MZSe5fj2ݗ)m&l'e}rȵv_&bUͭؓ?ʭDjO,M*I _i]H'E W2K*i%Cn9V+ZɶcuJ+#3 ۅxV}"36̫rlZ^;K&C.ctȉ!B[77?PT2{w|yYP(G,tgn@%IyVP PYTYα$Cեt)0bGy_%uJ~*V4?z)3ZTΠ<?4&"u1X*NKBk2r9?ʒS6SH002+\ɤҎKO328褝6)$ ̟LrY`Zdve-}+u˵:kV,ӪL΄ DNCRNKdz/-#:I"lO<4L o΃jqĭ߾XYֺ^$NVgd̀3Ptjp~ -G&fIr„'JI)W/wwέ"dOMa 'nn2RY`_B{ި!VqɮKi͜ 9cv_| {KX`)+]Ԁ0ƴdDO̸ǭ)E=Fx/. "aZ'?6Nx}aw>^I2[r#ҧ~K)̐V K,rA+vt`MI@c Ꞑ'OGNRaPNT94 jԓ+_33! " vC/QIҟwLM"$\͞fK<kUC8,"[C-͊S |O\ 4E⎹ݤ+.م-3_DYz( 2ZV|a! (tfj*R,lA弿.s"tsCUAFŻ(017AɒoRr4.2'{֬[訥' iK-`yu8G7$'!^YWOt-"ܚB8;boZmG8ݔݙc8]osci(hzxlNS:4@zWK3趋WǴm pPAG@g;a](вcXI3Er vC\!/T%@UXE=Zkᚮl!l!ĝ '$#37moRaJZTMq9_d)#QQ~2B/pn3l!<#a5ckf@$1@`O$șWkOzMO,{zc)"+vu:Oga),*Zӓ2@ b(%z8Ă@ ߰y3IENDB`0Dd .  3 A". ø. 16ρbU.(rP1mn).(rPPNG  IHDR !b%XsRGB pHYsttfxIDAT8Oc?!DHH~Th p*3њҷS-0C4Մ` V@^60E T f Qpgc Va*s16-UX9(EB`E`$:pO& k*IK@ t" ,&f10!y x`s вO|(<`K!#1IENDB`0Dd .  3 A". ø. 16ρbU.(rP1n).(rPPNG  IHDR !b%XsRGB pHYsttfxIDAT8Oc?!DHH~Th p*3њҷS-0C4Մ` V@^60E T f Qpgc Va*s16-UX9(EB`E`$:pO& k*IK@ t" ,&f10!y x`s вO|(<`K!#1IENDB`}DyK _Ref479694870$$If!vh#v #v #v :V l9 t6,59/ Bpyt $$If!v h#v #v#v#v#vT#v#v#v#v T:V l9 t6,,, 5 / B pZyt kd$$Ifl9  WI BCCCCBBBB t6$$$$44 lB apZyt $$If!v h#v #v#v#v#vT#v#v#v#v T:V l9 t6,, 5 9/ B pZyt kd.$$Ifl9  WI cccccBBBB t6$$$$44 lB apZyt $$If!v h#v #v#v#v#vT#v#v#v#v T:V l9 t6,, 5 9/ B pZyt kd?$$Ifl9  WI cccccBBBB t6$$$$44 lB apZyt $$If!v h#v #v#v#v#vT#v#v#v#v T:V l9 t6,, 5 9/ B pZyt kdP$$Ifl9  WI cccccBBBB t6$$$$44 lB apZyt $$If!v h#v #v#v#v#vT#v#v#v#v T:V l9 t6,, 5 9/ B pZyt kda$$Ifl9  WI cccccBBBB t6$$$$44 lB apZyt $$If!v h#v #v#v#v#vT#v#v#v#v T:V l9 t6,, 5 9/ B pZyt kdr$$Ifl9  WI cccccBBBB t6$$$$44 lB apZyt $$If!v h#v #v#v#v#vT#v#v#v#v T:V l9 t6,, 5 9/ B pZyt kd$$Ifl9  WI cccccBBBB t6$$$$44 lB apZyt }DyK _Ref479695506$$If!vh#v#v #v :V l9 t6,59/ Bpyt T$$If!v h#v#v#v#v #vo#v#v#v #v o:V l9 t6,,, 5 / B pZyt Tkd$$IfTl9 - ^'BCCCCBBBB t6$$$$44 lB apZyt T$$If!v h#v#v#v#v #vo#v#v#v #v o:V l9 t6, 5 9 / B pZyt Tkd$$IfTl9 - ^'ccccccccc t6$$$$44 lB apZyt T$$If!v h#v#v#v#v #vo#v#v#v #v o:V l9 t6, 5 9 / B pZyt Tkd$$IfTl9 - ^'ccccccccc t6$$$$44 lB apZyt T$$If!v h#v#v#v#v #vo#v#v#v #v o:V l9 t6, 5 9 / B pZyt Tkd$$IfTl9 - ^'ccccccccc t6$$$$44 lB apZyt T$$If!v h#v#v#v#v #vo#v#v#v #v o:V l9 t6, 5 9 / B pZyt Tkd $$IfTl9 - ^'ccccccccc t6$$$$44 lB apZyt T$$If!v h#v#v#v#v #vo#v#v#v #v o:V l9 t6, 5 9 / B pZyt Tkd!$$IfTl9 - ^'ccccccccc t6$$$$44 lB apZyt T$$If!vh#v#vm #v* :V l, t6,59/ Bpyt T$$If!v h#v#v#v#v#vT#v#v`#v#v T:V l, t6,, 5 9/ B pZyt Tkd$$IfTl, g XcCCCCBBBB t6$$$$44 lB apZyt T$$If!v h#v#v#v#v#vT#v#v`#v#v T:V l, t6, 5 9 / B pZyt Tkd$$IfTl, g Xccccccccc t6$$$$44 lB apZyt T$$If!v h#v#v#v#v#vT#v#v`#v#v T:V l, t6, 5 9 / B pZyt Tkd$$IfTl, g Xccccccccc t6$$$$44 lB apZyt T}DyK _Ref481495231$$If!vh#vB#vm #v :V l, t6,59/ Bpyt T$$If!v h#vB#v#v#v#vT#v#v#v#v T:V l, t6,,, 5 9/ B pZyt Tkd.$$IfTl, Z CbCCCCBBBB t6$$$$44 lB apZyt T$$If!v h#vB#v#v#v#vT#v#v#v#v T:V l, t6,5 9 / B pZyt TkdQ$$IfTl, Z Ccccccbbbb t6$$$$44 lB apZyt T$$If!v h#vB#v#v#v#vT#v#v#v#v T:V l, t6,5 9 / B pZyt Tkdh $$IfTl, Z Ccccccbbbb t6$$$$44 lB apZyt T}DyK _Ref481495878$$If!vh#v'#v5 #v* :V l t6,5'5 5 9/ Bpyt T5$$If!v h#v'#v#v`#v#v_#v#v`#v#v T:V l t6, 5'5_5;55_5]5;55 ;9 / B pZyt Tkd $$IfTl ? tf'f_f;ff_f]f;ff; t6$$$$44 lB apZyt T5$$If!v h#v'#v#v`#v#v_#v#v`#v#v T:V l t6, 5'5_5;55_5]5;55 ;9 / B pZyt Tkd$$IfTl ? tf'f_f;ff_f]f;ff; t6$$$$44 lB apZyt T5$$If!v h#v'#v#v`#v#v_#v#v`#v#v T:V l t6, 5'5_5;55_5]5;55 ;9 / B pZyt TkdQ$$IfTl ? tf'f_f;ff_f]f;ff; t6$$$$44 lB apZyt T5$$If!v h#v'#v#v`#v#v_#v#v`#v#v T:V l t6, 5'5_5;55_5]5;55 ;9 / B pZyt Tkd$$IfTl ? tf'f_f;ff_f]f;ff; t6$$$$44 lB apZyt T5$$If!v h#v'#v#v`#v#v_#v#v`#v#v T:V l t6, 5'5_5;55_5]5;55 ;9 / B pZyt Tkd$$IfTl ? tf'f_f;ff_f]f;ff; t6$$$$44 lB apZyt T,v666666666vvvvvvvvv666666>666666666666666666666666666666666666666666666666hH66666666666666666666666666666666666666666666666666666666666666666p62 0@P`p2 0@P`p 0@P`p 0@P`p 0@P`p 0@P`p 0@P`p8XV~ 0@ 0@ 0@ 0@ 0@ 0@ 0@ 0@ 0@ 0@ 0@ 0@ 0@ 0@666 OJPJQJ_HmH nH sH tH V`V QoNormal $xa$$CJOJPJQJ_HaJmH sH tH 2@Q2 'y Heading 1@&2@2 )y Heading 2@&2@!2 y Heading 3@&rrO Heading 4 $ & Fd((@&a$%6CJOJPJQJ]aJmHnHuDA D Default Paragraph FontRi@R 0 Table Normal4 l4a (k ( 0No List 6U`6 0 Hyperlink >*B*ph$$ Ostyle7T/T O Affiliation$a$OJPJQJ_HmH sH tH \^"\ ^ Normal (Web)ddd[$\$CJOJPJQJaJ*W 1*  ^`Strong5\H@BH E List Paragraph ^m$PJ4 @R4 B2Footer  p#.)a. B2 Page Number4@r4 B2Header  p#ZBZ = Body Text$da$OJPJQJaJmH sH tH >> = reference^`.X . #h@Emphasis6]L/L rstyle531#5CJOJQJ\^JaJo(ph/ thpsZ/Z QoDefault 7$8$H$%B*CJ^J_HaJmH phsH tH  Qop Table Grid7:V0 CJOJPJQJ^JaJmHsHV"@V h0Caption x#6B*CJPJ]aJmH phDTjsH >>@> !n_\Title $dhx@&a$5P/P n_\ Title Char#5CJOJPJQJaJmH sH tH .O". $Taautori"5\:O2: &D autori_opis#CJ]T/AT "Ta autori Char&5CJOJPJQJ\aJmH sH tH LORL (a]abstract_introduction%5;\/a\ #Dautori_opis Char#CJOJPJQJ]aJmH sH tH Z/qZ yHeading 1 Char&5;CJOJPJQJaJmH sH tH r/r %a]abstract_introduction Char&5;CJOJPJQJaJmH sH tH Z/Z yHeading 2 Char&5;CJOJPJQJaJmH sH tH */* > highlight<s!< ?zy0MentionB*ph+Wq PK![Content_Types].xmlN0EH-J@%ǎǢ|ș$زULTB l,3;rØJB+$G]7O٭VGRU1a$N% ʣꂣKЛjVkUDRKQj/dR*SxMPsʧJ5$4vq^WCʽ D{>̳`3REB=꽻Ut Qy@֐\.X7<:+& 0h @>nƭBVqu ѡ{5kP?O&Cנ Aw0kPo۵(h[5($=CVs]mY2zw`nKDC]j%KXK 'P@$I=Y%C%gx'$!V(ekڤք'Qt!x7xbJ7 o߼W_y|nʒ;Fido/_1z/L?>o_;9:33`=—S,FĔ觑@)R8elmEv|!ո/,Ә%qh|'1:`ij.̳u'k CZ^WcK0'E8S߱sˮdΙ`K}A"NșM1I/AeހQתGF@A~eh-QR9C 5 ~d"9 0exp<^!͸~J7䒜t L䈝c\)Ic8E&]Sf~@Aw?'r3Ȱ&2@7k}̬naWJ}N1XGVh`L%Z`=`VKb*X=z%"sI<&n| .qc:?7/N<Z*`]u-]e|aѸ¾|mH{m3CԚ .ÕnAr)[;-ݑ$$`:Ʊ>NVl%kv:Ns _OuCX=mO4m's߸d|0n;pt2e}:zOrgI( 'B='8\L`"Ǚ 4F+8JI$rՑVLvVxNN";fVYx-,JfV<+k>hP!aLfh:HHX WQXt,:JU{,Z BpB)sֻڙӇiE4(=U\.O. +x"aMB[F7x"ytѫиK-zz>F>75eo5C9Z%c7ܼ%6M2ˊ 9B" N "1(IzZ~>Yr]H+9pd\4n(Kg\V$=]B,lוDA=eX)Ly5ot e㈮bW3gp : j$/g*QjZTa!e9#i5*j5ö fE`514g{7vnO(^ ,j~V9;kvv"adV݊oTAn7jah+y^@ARhW.GMuO "/e5[s󿬅`Z'WfPt~f}kA'0z|>ܙ|Uw{@՘tAm'`4T֠2j ۣhvWwA9 ZNU+Awvhv36V`^PK! ѐ'theme/theme/_rels/themeManager.xml.relsM 0wooӺ&݈Э5 6?$Q ,.aic21h:qm@RN;d`o7gK(M&$R(.1r'JЊT8V"AȻHu}|$b{P8g/]QAsم(#L[PK-![Content_Types].xmlPK-!֧6 0_rels/.relsPK-!kytheme/theme/themeManager.xmlPK-!g theme/theme/theme1.xmlPK-! ѐ' theme/theme/_rels/themeManager.xml.relsPK] 0 U9O$*,.1X3d6z{#}}' !"$).147@ABE$z%M&&*t*p+/,^.D/2|24@67v'#%&'(*+,-/023568?F ,68\fh{GQS !!!!f"|"~"###%%%-.0./0000X###4#T#T###t#t#    4 XXUwX@ @H 0(  0(  B S  ? _Ref479694870 _Ref479695506 _Ref481495231 _Ref481495878`"$0"%0~%&+-4<Gu  ,9\i{GTkmoshm36=BPRTXc e g l !"!B!O!6";"N"S""" # # ##>#D#####$$$$3%<%=%J%%%%%%%&& (())1*>*,(,----O.T...../ /%/+/203050608090;0<0>0?000,9\i{GT!"!##20300,9\i{GT!"!##_,d,--------////////203050608090;0<0>0?0?0@0A0D0R0c0o0}0000000000,9\i{GT!"!##_,d,--------////////2030305060608090;0<0>0?0o0}000000000000000|j ]}x ~T޴>8J@d|b8"7dp!&rrPxYy8ip>߬  wPjM#P_@K*1&:z"_>NS\>@@q>`AjFH-\JȀL<_S(ZV{.E^`.^`.^`.^`. ^`OJQJo( ^`OJQJo( ^`OJQJo( ^`OJQJo(hh^h`. hh^h`OJQJo(^`OJPJQJ^Jo(-^`OJQJ^Jo(hHop^p`OJQJo(hH@ ^@ `OJQJo(hH^`OJQJ^Jo(hHo^`OJQJo(hH^`OJQJo(hH^`OJQJ^Jo(hHoP^P`OJQJo(hH^`o(.^`.pLp^p`L.@ @ ^@ `.^`.L^`L.^`.^`.PLP^P`L.^`o(.^`OJQJ^Jo(o p^p`OJQJo( @ ^@ `OJQJo(^`OJQJ^Jo(o ^`OJQJo( ^`OJQJo(^`OJQJ^Jo(o P^P`OJQJo(^`5CJOJPJQJo(. ^`hH. pL^p`LhH. @ ^@ `hH. ^`hH. L^`LhH. ^`hH. ^`hH. PL^P`LhH.h^h`.P^`P..^`...x^`x.... ^` .....  X^ `X ......  ^ `....... 8^`8........ `^``.........8^8`OJPJQJ^Jo(-^`OJQJ^Jo(o  ^ `OJQJo(  ^ `OJQJo(x^x`OJQJ^Jo(o H^H`OJQJo( ^`OJQJo(^`OJQJ^Jo(o ^`OJQJo(h^`OJQJo(hHh^`OJQJ^Jo(hHohp^p`OJQJo(hHh@ ^@ `OJQJo(hHh^`OJQJ^Jo(hHoh^`OJQJo(hHh^`OJQJo(hHh^`OJQJ^Jo(hHohP^P`OJQJo(hH ^`5PJo(.hhhhhhhh ^`OJQJo(^`OJQJ^Jo(o p^p`OJQJo( @ ^@ `OJQJo(^`OJQJ^Jo(o ^`OJQJo( ^`OJQJo(^`OJQJ^Jo(o P^P`OJQJo(h^`OJQJo(hHh^`OJQJ^Jo(hHohp^p`OJQJo(hHh@ ^@ `OJQJo(hHh^`OJQJ^Jo(hHoh^`OJQJo(hHh^`OJQJo(hHh^`OJQJ^Jo(hHohP^P`OJQJo(hHh^`56hH.h ^`hH.h pL^p`LhH.h @ ^@ `hH.h ^`hH.h L^`LhH.h ^`hH.h ^`hH.h PL^P`LhH.;@`789;<B*CJH*OJQJS*TX^JaJo(ph.G h^ `56789;<B*CJH*OJQJS*TX\]^JaJo(ph.G`56789;<B*CJH*OJQJS*TX\]^JaJo(ph)#h`h56CJOJQJ\]^JaJo()@  ^@ o(x^o(()H^o(()^o(()^o(()h ^`hH.h ^`hH.h pL^p`LhH.h @ ^@ `hH.h ^`hH.h L^`LhH.h ^`hH.h ^`hH.h PL^P`LhH.^`OJPJQJ^Jo(^`OJQJ^Jo(hHop^p`OJQJo(hH@ ^@ `OJQJo(hH^`OJQJ^Jo(hHo^`OJQJo(hH^`OJQJo(hH^`OJQJ^Jo(hHoP^P`OJQJo(hHh^`OJQJo(hHh^`OJQJ^Jo(hHohp^p`OJQJo(hHh@ ^@ `OJQJo(hHh^`OJQJ^Jo(hHoh^`OJQJo(hHh^`OJQJo(hHh^`OJQJ^Jo(hHohP^P`OJQJo(hH ^`CJaJo(.^`OJPJQJ^Jo(-pL^p`L.@ ^@ `.^`.L^`L.^`.^`.PL^P`L.i@K*>`A&rr7d~}|\>-\J_>_S#1&:Z w>> FHY:D                 T}/        ,8                  L|Jq WHb*(&5Id                  6Q                           | ,,8       e{'& Y;}2>,QGAe{',QGwY& Y;YGu,QGYX+,^9:9F#py&^ gN1H?4BVUE e-  Vb W  x E 6Fa5?v BZp}V\nw3 M?s6v+Z1F^IUv-*DGE+_. 6,!#>#+e# #$s$B%%&V'r' u'eS(@;*(+ ,5,l0I80~X0"1n1[22B23}v3,6Wr78e8Np8$9}9)e:g:;B<2=>9>H@MS@d@FAJBepC0EF; GfGZIbJ4$L2MXMS^MOoO]a]Xi]O6`Ta'bOeb}ebe$4fs=f\f>gRgh"hTghGNiXk}lJm\n$noQo`p p1pvDpBqUq{rwir4 s4psst?*tW3txt-udu~v'vN6vb]wxx@yGjy ky?zyzQ|,~a~ZFQfmL~yVd bJW>"&ZDs%>lw +k=RH; 5DcuPRzxPd[[k6B8| 1 ]7yi~w0}> #*N/b#hN5uk_^o{ iY+v]BtzN~Nk7Dr/Pp.{ smslG9?JczT,\/V#I. sLbVpbu#OjacG#UZLcX>\Fw ^w@(?0@p !u':GqwMd-UnK%.5@0Zp(+@-czUu3050@ PPP P! # $%&(+,00 @0@$L@*X@.`@2h@6p@@x@@Unknown G.Cx Times New Roman5Symbol3. *Cx Arial7.@Calibri5. .[`)TahomaC.,{ @Calibri Light?= *Cx Courier New;WingdingsG=  jMS Mincho-3 fgA$BCambria Math#1h*U*UĆ1)W1)W!400 3qHX $PF2! xx SGEM2008paper templateSGEM Organizing Team Matej Vargat                     Oh+'0$4 HT t    SGEM2008paper templateSGEM Organizing Team$http://www.sgem.org sgem@sgem.orgNormal Matej Varga2Microsoft Office Word@@@@1)՜.+,D՜.+,\ hp  ,International Scientific Conference SGEMW0  SGEM2008 Title 8@ _PID_HLINKSAx$? https://earthexplorer.usgs.gov/x$< https://earthexplorer.usgs.gov/ "mailto:mvarga@geof.hrRNhttp://www.sgem.org/  !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvwxyz{|}~      !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvwxyz{|}~      !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvwxyz{|}~    $%(Root Entry F-'@Data HV1TablecfWordDocument ;SummaryInformation( DocumentSummaryInformation8MsoDataStore0P-p-11Q3CKOW0PBDZUZ==20P-p-Item  PropertiesUCompObj r   F Microsoft Word 97-2003 Document MSWordDocWord.Document.89q