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 ISSN: 1998-4499 
 
 
                  All 
					papers of the journal were peer reviewed by two independent 
					reviewers. Acceptance was granted when both reviewers' 
					recommendations were positive. 
					
                    Main 
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							     Paper 
							Title, Authors, Abstract (Issue 1, Volume 2, 2008)  | 
							
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							Retrieving Slowness 
                            Distribution of a Medium between Two Boreholes from 
                            First Arrival Traveltimes 
							D. Ustundag 
							 
							Abstract: We study a problem of 
                            reconstruction of seismic wave speed distribution 
                            from a set of measured first arrival traveltimes in 
                            presence of strong velocity contrasts, which cause 
                            the problem to be highly non-linear. In this 
                            context, we make an attempt to improve a stable 
                            iterative reconstruction algorithm by incorporating 
                            appropriate a variable regularizing parameter and 
                            also used it for a simple synthetic borehole test 
                            after writing its algorithm in a C++ code. The 
                            simulations results support the effectiveness of the 
                            method. 
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							1-8 | 
						 
						
													
						
						
						
						
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							A Seismotectonic Study for 
                            the Heraklion Basin in Crete (Southern Hellenic Arc, 
                            Greece) 
							E. Kokinou, M. Moisidi, I. Tsanaki, E. Tsakalaki, 
                            E. Tsiskaki, A. Sarris, F. Vallianatos 
							 
							Abstract: In the context of the 
                            present work the spatial distribution of the seismic 
                            activity around Crete Island in the Southern 
                            Hellenic Arc for the period 2003-2007 is studied. 
                            Especially in the period July-October 2007 about 600 
                            events of low and moderate magnitudes have been 
                            indicated. Most of these events are located near 
                            coast and onshore of Crete. Additionally, we studied 
                            the relation of the earthquake epicenters with 
                            specific fault zones for the Heraklion basin. GIS 
                            techniques were used for mapping the distribution of 
                            earthquake epicenters on the various topographic and 
                            geological features of the area. Maps were created 
                            through interpolation algorithms. Spatial tools and 
                            statistical analysis were exploited to examine the 
                            correlation between earthquake loci and faulting 
                            orientations. The distribution of the epicenters 
                            indicates that the near coast and onshore seismicity 
                            is closely associated to the Crete tectonics. 
                            Especially for Heraklion prefecture the epicenter 
                            distribution is related to E-W, NE-SW and NW-SE 
                            striking faults. 
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							9-16 | 
						 
						
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							     Paper 
							Title, Authors, Abstract (Issue 2, Volume 2, 2008)  | 
							
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							Quantitive Assessment of Soil 
                            Degradation in some Areas North Nile Delta, Egypt 
							Kh. M. Darwish, W. A. Abdel Kawy 
							 
							Abstract: Most forms of land 
                            degradation are man-made problems, although there 
                            are some physical environmental factors involved, 
                            but mismanagement and misuse are still considered. 
                            Quantitative assessment of human induced land 
                            degradation and monitoring the changes in land 
                            qualities in Kafr EL-Sheikh Governorate during the 
                            period of 1963 to 2009 are the main objective of 
                            this study. Geometrically corrected 
                            physiographic-soil map was produced for the studied 
                            area. The comparison between the data extracted from 
                            the RISW reports, [1] and the data of this study 
                            were carried out to determine the rate of land 
                            degradation. Aerial photo-interpretation, Landsat 
                            ETM+ image, fieldwork and laboratory analysis data 
                            were used to produce the physiographic-soil map of 
                            Kafr EL-Sheikh Governorate. Land degradation rate, 
                            relative extent, degree, and severity level in the 
                            study area were assessed. The results indicate that 
                            the dominant active land degradation features are; 
                            water logging salinization, alkalinization and 
                            compaction. The main causative factors of human 
                            induced land degradation types in the studied area 
                            are over irrigation, human intervention in natural 
                            drainage, improper time use of heavy machinery and 
                            the absence of conservation measurements. 
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							17-22 | 
						 												
						
						
						
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							Late Cretaceous–Eocene 
                            Reactivations of the Hatta Shear Zone, Northern Oman 
                            Mountains 
							Ali M. A. Abd-Allah, Waheed A. Hashem, Osman 
                            Abdelghany 
							 
							Abstract: The NW-trending Hatta Shear 
                            Zone was formed in the Late Cretaceous during the 
                            emplacement of the Tethyan rocks and oceanic crust 
                            on the eastern margin of the Arabian plate. The 
                            western end of this shear zone is draped over by the 
                            Campanian-Lower Eocene carbonate rocks. These rocks 
                            were thrusted and folded later during the Tertiary 
                            Alpine deformation event. The folds are represented 
                            by two large plunging, asymmetrical NW-oriented 
                            anticlines that are interveined with a middle 
                            box-shape syncline, in addition to, four small NE 
                            and E-W trending folds. The syncline is 
                            characterized by a 3-segmented z-shape, as separated 
                            by the two bends; one of them is occupied by 
                            NE-oriented folds while the other is occupied by E-W 
                            oriented folds. The origin of this syncline may be 
                            controlled by the displacement over NW-trending, 
                            NE-dipping en echelon thrust faults bounding it. The 
                            estimated E-W regional compressive stress that 
                            initially accompanied the Cretaceous rock 
                            emplacement was locally adopted in later stages to 
                            NE-SW orientation. This deformation took place 
                            synchronous to deposition in three stages. It is 
                            commenced during the Campanian-Late Maastrichtian 
                            and renewed in Early Paleocene and in post Early 
                            Eocene times. This NE-SW compression produced El 
                            Rawdah structures, which reflect shortening values 
                            between 14% and 29.4%. The rock mechanical 
                            properties and bed thicknesses controlled the 
                            folding mechanisms. Whereas, buckling developed open 
                            folds in the thick and relatively brittle beds of 
                            the Campanian to Maastrichtian rocks, while flexural 
                            slip folding mechanism produced tight folds in the 
                            thin and ductile beds of the Maastrichtian to Early 
                            Eocene rocks. 
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							23-32 | 
						 			
						
						
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							     Paper 
							Title, Authors, Abstract (Issue 3, Volume 2, 2008)  | 
							
							 Pages  | 
						 
													
						
						
						
						
						
						
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							A Novel Maximum Fuzzy Entropy 
                            Thresholding of Seismic Images 
							Sanjay Kumar Singh 
							 
							Abstract: Image thresholding is very 
                            useful for keeping the significant part of an image 
                            and getting rid of the unimportant part or noise. 
                            This holds true under the assumption that a 
                            reasonable threshold value is chosen. The study of 
                            image thresholding techniques in earthquake 
                            engineering, remote sensing, geology and geophysics 
                            seems to be extremely important for recognition of 
                            certain patterns such as faults, folding, 
                            fracturing, thrusting, closure, salt domes, strong 
                            reflectors, seismic facies, channels, bright spots 
                            etc, and the identification of large zones of common 
                            signal texture which are not detectable so minutely 
                            by other techniques. This paper presents a novel 
                            maximum fuzzy entropy thresholding of seismic 
                            images. The concept of fuzzy probability and fuzzy 
                            partition is introduced first. Then, based on the 
                            conditional probabilities and fuzzy partition, a 
                            2-level optimal thresholding is searched adaptively 
                            through the maximum entropy principle of the seismic 
                            images. 
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							33-37 | 
						 			
						
						
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							The Interaction between Water 
                            Resources and Faults: Case Study of Lar Valley in 
                            Northeast Tehran 
							A. Khorsandi Aghai, T. Miyata, H. Ghoreishi 
							 
							Abstract: This research studies the 
                            interaction between the water resources and faults 
                            with the intention of identifying faults based on 
                            the effects of this inter-relation and their impacts 
                            on water resources. The research was conducted in 
                            the Lar valley located in the northeast of Tehran, 
                            the capital of Iran. The results indicate the 
                            influence of faults on 60% of Lar valley’s rivers as 
                            well as on the quality of Sefidab River. The 
                            location of 57.5% of the springs was also influenced 
                            by the fault’s actions and the change in the height 
                            of wellspring from 2500 to 3800 was attributed to 
                            the fault’s impact. 32.5% of the springs were of 
                            karstic, while 54% were of contact and 46% of 
                            overflow type, originating from the limestone 
                            (karstic), sandstones, siltstones, shale, tuff and 
                            volcanic rocks as well as the quaternary 
                            sedimentations. The water quality of most springs is 
                            thought to be influenced by faults. The results of 
                            this research complement the previous methods and 
                            they can be applied in addition to other procedures 
                            in similar cases to identify faults having an impact 
                            on surface or ground water resources. 
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							38-42 | 
						 		
						
						
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							Soil Study and Interpretation 
                            Procedures in Tourkovounia Hills of Attica, Greece 
							Dimitrios S. Oikonomou, Lambros Ekonomou 
							 
							Abstract: This work is a soil study 
                            which its purpose is to analyze and study the 
                            physicochemical properties of soil in the region of 
                            Tourkovounia hills of Attica, based on the samples 
                            that collected. Fifteen soil samples were collected 
                            from different parts of the analyzed area and 
                            several laboratory tests were carried out on them. 
                            The purpose of this study and laboratory tests is a 
                            deeper understanding of the soil nature and 
                            formation in the region of Tourkovounia hills of 
                            Attica, as well as the possibility of exporting 
                            valuable conclusions for the whole region. 
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							43-46 | 
						 		
						
						
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							Digital Geologic Mapping 
                            Methods: From Field to 3D Model 
							M. De Donatis, S. Susini G. Delmonaco 
							 
							Abstract: Classical geologic mapping 
                            is one of the main techniques used in geology where 
                            pencils, paper base map and field book are the 
                            traditional tools of field geologists. In this 
                            paper, we describe a new method of digital mapping 
                            from field work to buiding three dimensional 
                            geologic maps, including GIS maps and geologic 
                            cross-sections. The project consisted of detailed 
                            geologic mapping of the are of Craco village (Matera 
                            - Italy). The work started in the lab by 
                            implementing themes for defining a cartographic base 
                            (aerial photos, topographic and geologic maps) and 
                            for field work (developing symbols for outcrops, dip 
                            data, boundaries, faults, and landslide types). 
                            Special prompts were created ad hoc for data 
                            collection. All data were located or mapped through 
                            GPS. It was possible to easily store any types of 
                            documents (digital pictures, notes, and sketches), 
                            linked to an object or a geo-referenced point. 
                            Immediate thematic categorization of mapped objects, 
                            correct dimensions and positions allow to collect, 
                            interpret, and interpolate all data directly in the 
                            field. After field, the lab work was carried out 
                            keeping data separate from interpretation thanks to 
                            database opportunities. Finally, the geological map 
                            was interpreted in order to draw geologic sections 
                            and to build three-dimensional geologic model of the 
                            area. 
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							47-52 | 
						 		
						
						
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							Geological Investigation for 
                            Environmental Impact Assessment (EIA): Case Studies 
                            from Some of Mini Hydropower Projects in Sri Lanka 
							Nanda Wipula, Bandara Balasooriya 
							 
							Abstract: The geological investigation 
                            is a very important factor for the environmental 
                            impact assessment (EIA) study for any development 
                            project. The major objectives of this geological 
                            investigation are to identify existing surface and 
                            sub-surface geological conditions of selected 
                            locations for the main structures of the project, to 
                            describe stability condition of soil overburden and 
                            the bed rock, to analyze geological hazard situation 
                            of the area and to recommend appropriate 
                            precautionary measures to mitigate anticipated 
                            environmental impacts due to unfavorable geological 
                            conditions. At present study was focused to conduct 
                            the geological investigations for some of the 
                            mini-hydropower projects in Central Highlands of Sri 
                            Lanka. The mini hydropower project mainly consists 
                            of diversion weir, fore bay tank, penstock line and 
                            a power house. The locations of the above structures 
                            have been selected after the preliminary field and 
                            literature survey. For the purpose of this 
                            geological survey, the evaluation of general aspects 
                            of in-situ ground stability of the proposed location 
                            of the weir site, fore bay tank, penstock line 
                            connecting the fore bay tank, the power house have 
                            been investigated. On an appraisal of the analysis 
                            of data collected in the field and conclusion made 
                            based on the field observations, the proposed 
                            locations to construct the mini hydropower projects 
                            where moderate level of geological hazards and 
                            landslide risk exists can be recommended for the 
                            above projects only with the applications of 
                            location specific guidelines and precautionary 
                            measures for the prevention of future geologic 
                            hazards. It is advised to adhere to some 
                            recommendations for the sound construction and 
                            operation of the proposed mini hydropower projects. 
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							53-58 | 
						 				
						
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							     Paper 
							Title, Authors, Abstract (Issue 4, Volume 2, 2008)  | 
							
							 Pages  | 
						 
													
						
						
						
						
						
						
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							A Study on Light Expended Clay 
                            Aggregate (LECA) in a Geotechnical View and its 
                            Application on Greenhouse and Greenroof Cultivation 
							Siamak Boudaghpour, Shervin Hashemi 
							 
							Abstract: Increasing population in the 
                            world increases the demand of housing and it causes 
                            destroying pasture lands and jungles immethodically. 
                            It also causes soil attrition in every country of 
                            the world. In this way, the demand of making 
                            flowerbeds in the inner and outer parts of the 
                            building increases. But expending method of making 
                            these flowerbeds as they need an environment to keep 
                            the plant and also not to be harmful for the plant 
                            and environment and also they are needed to be light 
                            and economical. According to our studies, LECA has 
                            some specific properties which can be apply as a 
                            suitable material. In this study, first the LECA and 
                            its suitable properties has been introduced in a 
                            geological and geotechnical view. Then the LECA 
                            application on greenhouse cultivation has been 
                            reviewed and a new method of making green roof by 
                            using LECA. 
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							59-63 | 
						 			
						
						
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							The New Prediction of the 
                            Minimum Miscible Pressure by Iranian Fractured 
                            Reservoirs 
							S. Torfi, E. Novieri 
							 
							Abstract: The aim of this study is to 
                            develop a new model to predict the minimum 
                            miscibility pressure (MMP) of Iranian oil 
                            reservoirs. So far, different MMP correlations and 
                            models regarding the kind of injection gas and the 
                            mechanism of miscibility have been proposed, which 
                            are respectively based on mathematical and 
                            thermodynamic calculations. None of these 
                            correlations can be used with enough confidence and 
                            applying them for Iranian reservoirs is more or less 
                            prone to errors. In this article, compositional and 
                            empirical models introduced for predicting MMP 
                            regarding the composition of the injected gas and 
                            the condition in which miscible displacement is done 
                            have been studied. Experimental data from Iranian 
                            oil reservoir b with different injection gases 
                            carried out by slim-tube test have been used to 
                            obtain a new MMP correlation that is suitable to be 
                            applied to Iranian oil reservoir. By applying the 
                            new MMP correlation, one can determine minimum 
                            miscibility pressure of Iranian oil reservoir with 
                            more accuracy and within a shorter period of time. 
                            The predicted MMPs are compared with the 
                            experimental results reported from the above 
                            reservoirs .The sensitivity analysis is done and 
                            consequently their error percentage are determined 
                            and reported. Therefore, a suitable model with less 
                            error and more precision is introduced. It is shown 
                            that the results obtained from the new MMP model are 
                            more accurate when they are compared with other most 
                            common correlations reported in literature. 
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							64-66 | 
						 		
						
						
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							Study of the Causes for a 
                            Landslide Occurring on a National Road 
							Voicu Cristina Otilia, Mirea Monica 
							 
							Abstract: In the beginning of the 
                            report, the authors present several general 
                            considerations regarding the geographic, geological 
                            and climatic placement of the area where the 
                            landslide occurred. Further on, the situation 
                            regarding stability conditions and technical state 
                            of the affected road is described. After the 
                            analysis of the geotechnical and 
                            technical-geological aspects, its causes and 
                            characteristics are established. Following these 
                            aspects, the report presents the recommended and 
                            applied consolidation solution. 
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							67-69 | 
						 		
						
						
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							Microstructural Characteristics 
                            of Saprolite with Different Weathering Degree 
							Hu Ruilin, Li Lihui, Yue Zhongqi, Wang Lichao, Fan 
                            Linfeng 
							 
							Abstract: Microstructural 
                            characteristics of saprolite with different 
                            wheathering degrees is obtained based on SEM images. 
                            A new index—plagioclase solution degree is proposed 
                            to evaluate the weathering degree of saprolite. 
                            Application in three sections of Hong Kong suggests 
                            that the new index is sensitive to saprolite and 
                            that it can identify the degrees of weathering. 
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							70-72 | 
						 			
						 
						
						
 
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