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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
Page
Paper
Title, Authors, Abstract (Issue 1, Volume 2, 2008) |
Pages |
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 |
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 |
Paper
Title, Authors, Abstract (Issue 2, Volume 2, 2008) |
Pages |
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 |
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 |
Paper
Title, Authors, Abstract (Issue 3, Volume 2, 2008) |
Pages |
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 |
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 |
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 |
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 |
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 |
Paper
Title, Authors, Abstract (Issue 4, Volume 2, 2008) |
Pages |
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 |
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 |
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 |
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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