In: Wagner W., Szekely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7,2010, IAPRS, Vol. XXXVIII, Part 7B 
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result, we have the initial quantitative information for search 
features, which the possible, can be controlling of the pools. 
Another group of methods is allowing the assessing of 
connection of the searches of features, which was selected, with 
the objects of prognosis for the complex estimate of prognosis 
of territory. 
These exploration methods include the traditional methods 
and methods developed by authors or with their participation. 
Methods, which were developed by authors in this article, are 
submitted. 
2.2. Methods of structural of research 
For the study of anticline structures of sedimentary cover is 
used the method of selection of anomalous values of the height 
field of modem relief. Relief is created from the Shuttle satellite 
data. For most regions the anticlines in modem relief are 
revealed as raising. Authenticity of the selected anticline fields 
are estimating by comparing seismic research data and 
materials of structural interpretation. 
We use the structural interpretation results of multispectral 
space images as the initial information for studying breaks, 
knots of cross breakings and circular structures. We used the 
structural interpretation results of multispectral space images as 
the initial information for studying breaks, knots of cross 
breakings and circular structures. The structural interpretation 
of multispectral images is conducted by sight by known 
methods of interpretations (Kats and et. 1988, Aerospace 
research, 1988, Barret, Kurtis, 1979, Kravtsova and Dr., 1985, 
Kronberg, 1988, Multispectral remote sensing, 2006, et.). 
Parallel comparative analysis of interpretation of multispectral 
images and topographical maps is performed for control and 
delete the man-made lineaments. It is very important to fulfill 
the works for territory that have the high loading man-made. If 
the multispectral images did not show of the lineaments or 
they are expressed badly, interpretation is conducted on the 
topographical maps. The 3D relief model will be interpreted. 
As a result of interpretation, the maps are created for breaks, 
circular and plicate structures and scheme of breakings and 
blocks structures for the studied territory. All information is 
present in a vector form. It allows the constructed maps to be 
juxtaposed with other different geologic-geophysical data and 
prepared in GIS. It is very important for further use. 
2.3. Method of study of crack permeability of rocks 
The special attention is given to studying breaks of rock 
permeability. It is one of important search features. Traditional 
methods studies of permeability of breaks are use of study for 
rock exposure, in the production excavation and of core 
drilling. These methods are expensive and labor intensive and 
limited the opportunities of study of breaks permeability of 
rocks. 
We developed method of rock permeability study for poorly 
naked territory and large areas. Method is based on lineaments 
study. Lineaments are characterized by different sizes of break 
in the earth's surface such as large faults, raised strips, fracture 
zones, fold structures and etc. Lineaments are characterized by 
different sizes of break in the earth's surface such as large 
faults, raised strips, fracture zones, fold structures and etc. 
Due to inherent evolution of rock structure, a new relief is 
reorganized and the ancient relief is saved. Naturally, 
lineaments can give generalize and integrate schemes of breaks 
of the earth's crust. As a result of joint action of several 
exogenous processes, the numerous lineaments for any territory 
may be detailed. Lineaments have diversity of orientation and 
extent. In the process of structural interpretation of 
multispectral images for the study of crack permeability of rocks 
all lineaments are selecting. Their quantity does not depend on 
size, orientation or landscape of indicators. Our method differs 
from the structural interpretation method with the purpose of 
studying faults and folds. The number of selected lineaments are 
considerably more that the quantity of faults and breaks, which are 
selected by other methods of research (Mesheryakov, 1965, 
Golbrayh and et., 1968, Chebanenko, 1977, Tyapkin, 1998, 
Palienko and et. 2005, Multispectral remote sensing, 2006, and 
other). 
Furthermore we must to know such the parameter of 
permeability of zone of exploration as fissire opening. It is 
impossible to do on the remotely-sensed data. We assume that 
within the limits of every lineament system all fissures are 
characterized by nearest values of opening. The common quantity 
of fissures of every system can be evaluate for cracked rock 
permeability (i.e., rock crack permeability can be quantitative 
value estimated in every point of territory as the quantity or total 
length of lineaments of every system, attributed to unit of area). 
The results of studying rock break permeability are represented 
in a quantitative form. It is very important and allows 
mathematical methods to be used for processing and analysis. The 
results of special research showed that the accumulation of 
hydrocarbons did not have maximal or minimal permeability 
values. These values are conformed to intermediate (optimum) of 
permeability. The quantitative analysis methods determine 
optimum interval values for these features. They can be 
incorporated with other search features, and first of all, with the 
geophysical research data. It is necessary and important for 
reliable evaluate of potential of territory. 
For the decision of tasks of prognosis to present the lineament 
maps in a quantitative form are necessary. The methods of 
lineament analysis include: 
1) . Analysis of orientation regularity and selection of borders of 
the lineaments. 
2) . Select of indexes for quantitative description of the lineaments 
field. 
3) Analysis and interpretation of geological maps for graph 
tightness and total length of lineaments for every system. 
The characteristic features of this analysis method are: 
1) The attention is focused for localization of the borders of the 
lineament systems. The modal values of every system are second- 
rate. This analysis provides of the orienting the maximums and 
minimums on the graphs of azimuth distribution of extending 
lineaments. 
2) For the selection of the systems of lineaments are using the 
graphs of dispensation of their distribution azimuths. The graphs 
are constructed with differing sites of initial points. 
3) The interval width is specially selected for lineament groupings. 
This value is used to construct and analyze graphs of azimuth 
distribution of extended lineaments. Easily is showed that the 
quantity of the lineament systems, which is possible select on the 
analyzed graphs, relies on the interval width of grouping which is 
used to construct these graphs. 
The analyses of regularity of orientation of lineaments are 
conducted in two stages. The first stage is calculated azimuth 
trends of all selected lineaments within the limits of separate 
blocks or local areas with the relatively homogeneous measured 
geological structure. The significant distribution values for 
azimuths of extended lineaments from normal distribution are 
determined. Meaningful distinctions testify to existence of the 
separate lineaments systems. For reliability, the nonparametric 
statistical criteria of Pirson (y 2 ) are used to estimate separate 
maximums and minimums. 
The second stage is selecting of the general lineaments systems 
for explored territory only. The data are used on separate blocks to 
construct azimuth distribution of modal values of local maximums