"GEOECOLOG" Company
Center of Geological and Seismological
Studies
Kyiv, Ukraine
"GEOECOLOG" Company, Center of Geological
and Seismological Studies, offer their services in conducting geological,
hydrogeological and geological-engineering prospecting and geological environment
ecological research. This research is effected with the use of unique opportunities
offered by biological, energetic and information technologies based on
neurotechnical complex that allows to regulate a sensor sensitivity and
capture an adaptive reaction of neuro-muscular human tissues to variations
of amplitude-frequency characteristics of natural electromagnetic field
of the Earth (Patent No 94030887 of July, I, 1993, Ukraine).
The technology provides for:
-
search and surface outline of deposits of hydro-carbonates,
ores of set composition, subsurface water and other natural resources;
-
mapping of karst and other subsurface cavities, landslides
and crack structures, etc.
-
surface geological and prospecting operations on land
and sea from any vehicle (road-, air- or sea-based);
-
in-depth study of the identified objects internal structure
and tracking its single elements in extension;
-
identification and lithological sequence of geological
section and selection of productive horizons (horizons containing any type
of mineral resources, including oil and gas) in it while determining the
depth of deposits;
-
assessment of the relative productive component variation
within the area to be studied (in plane and section) and relative comparison
of its content vs. acknowledged deposits;
-
identification of the subsurface water chemical composition
and relative evaluation of individual components content as well as of
a general mineralization;
-
defining way and direction of the fluid lateral migration
in rocks;
-
outlining anthropogenious zones of subsurface water
contamination with oil products and other substances;
-
identification of leakage from closed pipelines.
Fig.
1, Opportunities Offered by Biological, Energetic and Information Technology
in Studying Lithology and Geographical Section Production Horizons Identification.
H - depth of Deposits (m)
vs. Function electromagnetic wave length;
J - assumptional tensity
of natural electromagentic field in values of coarsening sensor sensitivity
of neuro-muscular tissues:
(a) general or integral;
(b) selective with resonance adjustment for hydrocarbonates;
(c) water;
(d) limestones; (e) clays:
(f) sandstones;
(g) granites:
In Column: 1. limestones;
2. clays 3. producticve hydrocarbonate horizon in sandstones 4. water bearing
sandstones 5. sandstones 6. granites
Unlike its prototype - biological
location - this technology provides physically grounded predictable results
based on laws of a material world. If compared with traditional geophysical
studies, the method is characterized with its efficiency, high resolution
capacity, no limits of measurement in depth and the possibility of natural
resources remote identification, both in surface and section.
The biological, energetic and information technology
using neurotechnical complex when applied in a transport version of research
allows to evaluate potential hydrocarbonate deposits and outline them at
the area ten thousand kilometers within two or three months only.
Fig.
2; Opportunities Offered by Biological, Energetic and Information Technologies
in Hydrogeological Studies.
Assumptional tensity of natural
electromagnetic field in values of neuro-muscular tissue relative coarsening
with resonance adjustment for hydrocarbonates. Graph shows margins
of hydrocarbonate deposits; tensional breaks, and isogyps of oil prone
horison tops.
Using our technology it is
possible for 1-2 days to conduct field studies of the lithological sequence
of geological section at any point of the Earth surface while identifying
in it oil productive and watery horizons up to the depth of 5 to 6 kilometers
mastered with oil industrial drilling. Geological surveys at the area of
several square kilometers resulting in recommendations as to the rational
location and structure of drilled water collectors up to 100 - 200 m. in
depth can be effected for 2-3 weeks whereas similar operations combined
with the detection of watery horizons position up to 20-30 m at individual
piece of land with the area of up to 0. I hectares will take only 1-2 hours.
The cost of survey using biological, energetic and
information technologies constitutes just 2-5% of that of drilling survey
and rational location of wells to be drilled is guaranteed.
This technology has been tested at known deposits
of oil and gas (Crimea, the Karpathian Mountains, Dnieper River left bank
areas, Southern Regions of Ukraine at Black Sea ), at areas of subsurface
water contamination with oil products (Crimea and Dnieper River areas),
during studies of landslides of the Crimean Southern Coast mapping karsts
in Crimea and Karpathian Mountains, searches of local water supply sources
(Crimea, Georgia, Karpathian Mountains). Studies with the use of biological,
energetic and information technologies had been highly estimated by Ukrainian
experts whereas our recommendations as to location of subsurface water
collectors were justified in 95% of cases.
These studies might be very useful for institutions
engaged in exploration and recovery Of Oil, gas and other types of mineral
resources, for companies and individual proprietors of land who need to
have subsurface water collectors industrial companies doing construction
works under adverse engineering and geological conditions, companies designing
and implementing environmental protection projects.
Graph
I; outlining graph;
Graph
II; graphs of probing and position of a corresponding point on profile;
Graph III hydrogeological section.
PLEASE FORWARD YOUR PROPOSAL TO THE FOLLOWING
ADDRESSES:
"GEOECOLOG"
Company
Ivana Maryanenko Lane, 13,
suite 85
Kiev, 21, 252021
UKRAINE
Tel:/ Fax: (380) (44) 293-1297 |
Center of Geological and Seismological
Studies
Gagarina St., 20
Simferopol, 26, 333026
Crimea, Ukraine
Tel: (380) (652) 22-8565 |
This page is maintained by Myroslaw
Smorodsky of BRAMA.
Last modified on March 14, 1997
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