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<records>

  <record>
    <language>eng</language>
          <publisher>Oriental Scientific Publishing Company</publisher>
        <journalTitle>Biosciences Biotechnology Research Asia</journalTitle>
          <issn>0973-1245</issn>
            <publicationDate>2016-06-13</publicationDate>
    
        <volume>11</volume>
        <issue>Spl.Edn.2</issue>

 
    <startPage></startPage>
    <endPage></endPage>

	    <publisherRecordId>12080</publisherRecordId>
    <documentType>article</documentType>
    <title language="eng">The Way of Structural Interpretation of Potential Fields Under Condition of a Priori Geological Information Minimum</title>

    <authors>
	 


      <author>
       <name>Igor B. Movchan</name>

 
		
	<affiliationId>1</affiliationId>
      </author>
    

	 


      <author>
       <name>Alexandra A. Yakovleva</name>


		
	<affiliationId>1</affiliationId>

      </author>
    

	

	


	


	
    </authors>
    
	    <affiliationsList>
	    
		
		<affiliationName affiliationId="1">National Mineral Resource University (University of Mines) Russia, 199106, St.-Petersburg, Vasil’evsky island, 21st line, 2, Russia</affiliationName>
    

		
		
		
		
		
	  </affiliationsList>






    <abstract language="eng">The aim of paper is in development of interpretation of potential and
quasipotential fields which in geophysics traditionally includes the qualitative and
quantitative approaches. To the first interpretation they relate the transformations of
structure of measured signal: filtration and zoning. At the stage of qualitative
interpretation the processed field is considered in the area of absence of sources of its
anomalies and these fields keep the analyticity. The quantitative interpretation is in
various recalculations of field in the depth, i.e. in the area of existence of anomalous
geological sources in the small vicinity of which the gravitational, magnetic and electric
potentials approach infinity. Under such transformations the geometrical and physical
parameters of heterogeneities of geological half-space are reconstructed by the methods of
solution of ill-posed problems. The last ones has some peculiarities: on one hand, it takes
time with regard to the qualitative interpretation and, on the other hand, it rouses
censure within geologists because of the necessity of simplification of reconstructed
heterogeneities in geological media. The solution of ill-posed problem always has
multivalued character: one anomaly corresponds to a wide class of models of geological
heterogeneities with significant difference in geometry, elements of bedding, average
physical properties. This difficulty is overcame by the set of independent methods of
analytical continuation, one of which gives the structural image of geological cross section
which is comparable to the seismic cross section.</abstract>

    <fullTextUrl format="html">https://www.biotech-asia.org/vol11_nospl_edn2/the-way-of-structural-interpretation-of-potential-fields-under-condition-of-a-priori-geological-information-minimum/</fullTextUrl>



      <keywords language="eng">
        <keyword>Inverse problem; models; interactive fit; structural image; potential signal</keyword>
      </keywords>

  </record>
</records>