Types of presentation
Oral Presentation
Presentation time for ORAL presentation is 10 minutes + 5 min for questions from the audience.
You shall make your presentation in a timely manner. Kindly note that the time is usually followed the the conference Chairman.
All presentations have to be made in English
Speakers are kindly asked to use the available in the Conference hall Laptop. Only if they have special reasons they may use their own laptops (in that case they have to inform the technical assistant before the session).
Only PowerPoint presentations on a CD-ROM/DVD or a USB Memory stick will be accepted.
Types of presentation
Oral Presentation
Presentation time for ORAL presentation is 10 minutes + 5 min for questions from the audience.
You shall make your presentation in a timely manner. Kindly note that the time is usually followed the the conference Chairman.
All presentations have to be made in English
Speakers are kindly asked to use the available in the Conference hall Laptop. Only if they have special reasons they may use their own laptops (in that case they have to inform the technical assistant before the session).
Only PowerPoint presentations on a CD-ROM/DVD or a USB Memory stick will be accepted.
Types of presentation
Oral Presentation
Presentation time for ORAL presentation is 10 minutes + 5 min for questions from the audience.
You shall make your presentation in a timely manner. Kindly note that the time is usually followed the the conference Chairman.
All presentations have to be made in English
Speakers are kindly asked to use the available in the Conference hall Laptop. Only if they have special reasons they may use their own laptops (in that case they have to inform the technical assistant before the session).
Only PowerPoint presentations on a CD-ROM/DVD or a USB Memory stick will be accepted.
Types of presentation
Oral Presentation
Presentation time for ORAL presentation is 10 minutes + 5 min for questions from the audience.
You shall make your presentation in a timely manner. Kindly note that the time is usually followed the the conference Chairman.
All presentations have to be made in English
Speakers are kindly asked to use the available in the Conference hall Laptop. Only if they have special reasons they may use their own laptops (in that case they have to inform the technical assistant before the session).
Only PowerPoint presentations on a CD-ROM/DVD or a USB Memory stick will be accepted.
Publication ethics
Authors
The Author declares that the manuscript is original and in its present form has not been published elsewhere in any form, that it has not been submitted to any journal/proceedings and that it will not be submitted to any other journal/proceedings, if it is accepted for publication in the GEOLINKS Conference Proceedings.
The Author is responsible for the research they have been done and for the results described in the paper.
The Author warrants that the article doesn't infringe upon any copyright, contains no libelous or otherwise unlawful statements, and does not otherwise infringe on the rights of others.
The Author transfers the copyright for this publication/article to the GEOLINKS Conferences.
The Author licenses to the Publisher the right to distribute the Article as a part of GEOLINKS Conference proceedings.
Submission Guidelines
Abstract Submission
An abstract between 300 to 500 words, clearly summarising the arguments, should be submitted before deadline.
The preferred length of paper (including footnotes) is 5,000 words (maximum limit). In general, please confine your paper between 10-12 pages, everything included.
It is author's responsibility to ensure that all references and citations are correct, and that the contribution does not contain any material that infringes copyright, or is defamatory, obscene or otherwise unlawful or litigious. Please check GEOLINKS Tips.
Copyright in the article will remain jointly with the owner of the copyright and the Publisher. By submitting an article to the conference, the owner of the copyright grants the publisher with a license to publish the article. The author warrants that he is the owner of all rights of copyright in the article. Where the author subsequently publishes the article, the author is requested to acknowledge the article appeared in the conference proceedings.
The Author(s) will indemnify and defend the Publisher against any claim, demand or recovery against the Publisher by reason of any violation of any proprietary right or copyright, or because of any libellous or scandalous matter contained in the Manuscript.
The Publisher will have the right to edit the work for the original edition and for any revision, provided that the meaning of the text is not materially altered.
Submission Guidelines
Abstract Submission
An abstract between 300 to 500 words, clearly summarising the arguments, should be submitted before deadline.
The preferred length of paper (including footnotes) is 5,000 words (maximum limit). In general, please confine your paper between 10-12 pages, everything included.
It is author's responsibility to ensure that all references and citations are correct, and that the contribution does not contain any material that infringes copyright, or is defamatory, obscene or otherwise unlawful or litigious. Please check GEOLINKS Tips.
Copyright in the article will remain jointly with the owner of the copyright and the Publisher. By submitting an article to the conference, the owner of the copyright grants the publisher with a license to publish the article. The author warrants that he is the owner of all rights of copyright in the article. Where the author subsequently publishes the article, the author is requested to acknowledge the article appeared in the conference proceedings.
The Author(s) will indemnify and defend the Publisher against any claim, demand or recovery against the Publisher by reason of any violation of any proprietary right or copyright, or because of any libellous or scandalous matter contained in the Manuscript.
The Publisher will have the right to edit the work for the original edition and for any revision, provided that the meaning of the text is not materially altered.
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Types of presentation
Proceedings 2020
All GEOLINKS 2020 participants get an online access to the full conference proceedings.
You can find the full digital books, including all accepted and published double blind peer-reviewed papers.

GEOLINKS Proceedings
Book 1 Volume 2
Air Pollution and Climate Change
Biotechnologies
Environmental Geology
Soil Science
Water Resources
GEOLINKS Proceedings
Book 2 Volume 2
Ecology and Environmental Studies
Environmental Economics
Green Buildings Technology and Materials
Green Design and Sustainable Architecture
GEOLINKS International Conference 2020, Book 1
ENVIRONMENTAL GEOLOGY
GEOLOGICAL AND GEOPHYSICAL STUDY FOR ELABORATION OF GEOTHERMAL MODEL IN ORADEA-BAILE FELIX AREA
Dr. Laurențiu Asimopolos, Dr. Natalia-Silvia Asimopolos
ABSTRACT
Thermal methods consist of measuring thermal gradient and satellite data, which can be used to determine the Earth's surface temperature and thermal inertia of surficial materials, of thermal infrared radiation emitted at the Earth's surface.
Thermal gradient measuring, with a knowledge of the thermal conductivity provides a measure of heat flow. Conditions that may increase or decrease and heat flow are influenced by hydrologic, topographic factors and anomalous thermal conductivity.
Also, oxidation of sulphide bodies in-place or on waste deposits, if sufficiently rapid, can generate thermal anomalies, which can provide a measure of the amount of metal being released to the environment.
The geothermal gradient on the territory of Romania, the increase of the temperature with the depth, has an average value of 2.5°-3°C/100m, which corresponds to a temperature of 100° C at 3000 m deep. There are many areas where the value of the geothermal gradient differs considerably from this average.
For example, in areas where the rock plate suffered rapid dips and the basin was filled with sediment "very young "from a geological point of view, the geothermal gradient may be less than 1° C/100m. On the other hand, in other geothermal areas the gradient exceeds much this average.
These areas are true underground thermal reservoirs of potentially high geothermal energy which under certain favourable conditions can be exploited to serve heating installations and domestic hot water systems.
The geothermal prospecting for the entire territory of Romania, carried out by temperature measurements allowed the development of geothermal maps, highlighting the temperature distribution at different depths.
Geophysical data obtained through various methods and geophysical modelling provide generalized and non-unique solutions to the geometry of underground geological relations as well as to the physical characteristics of different formations.
The non-uniqueness of these models (solutions to the direct problem) arises from the impossibility of knowing the boundary conditions between different strata, which together with the propagation equations of the different fields (depending on the geophysical method used for the investigation of the basement) form the systems that offer the solutions of the model.
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The Oradea geothermal reservoir is located in the Triassic limestones and dolomites at depths of 2,200-3,200 m, on an area of about 75 km2 , and it is exploited by 14 wells with a total maximum flow rate of 140 l/s geothermal water with well head temperatures of 70-105°C. There are no dissolved gases, the mineralisation is 0.9-1.2 g/l, the water being of calcium-sulphate-bicarbonate type.
The Oradea Triassic aquifer is hydrodynamically connected to the Felix Spa Cretaceous aquifer, and together are part of the active natural flow of water. The water is about 20,000 years old and the recharge area is in the northern edge of the Padurea Craiului Mountains and the Borod Basin.
KEYWORDS
geological and geophysical model, geothermal water, thermal conductivity, flow rate