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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-3206</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Геоморфология и народное хозяйство</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Geomorphology and economy</subject></subj-group></article-categories><title-group><article-title>О возможности обнаружения коренных алмазоносных пород в Ленинградской области</article-title><trans-title-group xml:lang="en"><trans-title>On the possibility to find diamond-bearing solid rocks in the Leningrad region</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Ладнер</surname><given-names>Г. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Ladner</surname><given-names>G. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Егоров</surname><given-names>И. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Egorov</surname><given-names>I. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>ВНИИКАМ, г. С.-Петербург</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1995</year></pub-date><pub-date pub-type="epub"><day>10</day><month>03</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>47</fpage><lpage>56</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ладнер Г.А., Егоров И.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Ладнер Г.А., Егоров И.В.</copyright-holder><copyright-holder xml:lang="en">Ladner G.A., Egorov I.V.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://geomorphology.igras.ru/jour/article/view/3206">https://geomorphology.igras.ru/jour/article/view/3206</self-uri><abstract><p>Structural-geomorphological works carried out with view to forecast mineral deposits suggest the Lembolov morphostructure (Karelian Isthmus) to be promising for search for diamonds in solid rocks. The morphostructure is located within an area complicated in geological structure, at a node of deep-seated faults which delimit earthorust blocks different in characteristics. The Lembolov morphostructure was formed as an elevation during the post-Cambrian time (probably in the Lower Paleozoic) , when molten magma penetrated the earthcrust. The present appearance of the morphostructure is due to denudation and glacial deposition processes.</p></abstract><trans-abstract xml:lang="en"><p>Structural-geomorphological works carried out with view to forecast mineral deposits suggest the Lembolov morphostructure (Karelian Isthmus) to be promising for search for diamonds in solid rocks. The morphostructure is located within an area complicated in geological structure, at a node of deep-seated faults which delimit earthorust blocks different in characteristics. The Lembolov morphostructure was formed as an elevation during the post-Cambrian time (probably in the Lower Paleozoic) , when molten magma penetrated the earthcrust. The present appearance of the morphostructure is due to denudation and glacial deposition processes.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
