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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">gtcrust</journal-id><journal-title-group><journal-title xml:lang="ru">Геодинамика и тектонофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Geodynamics &amp; Tectonophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2078-502X</issn><publisher><publisher-name>Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.5800/GT-2024-15-2-0754</article-id><article-id custom-type="edn" pub-id-type="custom">GJZCIS</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1824</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>ТЕКТОНОФИЗИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>TECTONOPHYSICS</subject></subj-group></article-categories><title-group><article-title>О ВОЗМОЖНОМ МЕХАНИЗМЕ ОБРАЗОВАНИЯ ОТКРЫТОЙ ТРЕЩИНОВАТОСТИ В ОСАДОЧНЫХ БАССЕЙНАХ</article-title><trans-title-group xml:lang="en"><trans-title>ON THE POSSIBLE FORMATION MECHANISM OF THE OPEN FRACTURING IN SEDIMENTARY BASINS</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>Ребецкий</surname><given-names>Ю. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Rebetsky</surname><given-names>Yu. L.</given-names></name></name-alternatives><bio xml:lang="ru"><p>123242, Москва, ул. Большая Грузинская, 10, стр. 1</p></bio><bio xml:lang="en"><p>10-1 Bolshaya Gruzinskaya St, Moscow 123242</p></bio><email xlink:type="simple">reb@ifz.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт физики Земли им. О.Ю. Шмидта РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Schmidt Institute of Physics of the Earth, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>20</day><month>04</month><year>2024</year></pub-date><volume>15</volume><issue>2</issue><fpage>754</fpage><lpage>754</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ребецкий Ю.Л., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Ребецкий Ю.Л.</copyright-holder><copyright-holder xml:lang="en">Rebetsky Y.L.</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://www.gt-crust.ru/jour/article/view/1824">https://www.gt-crust.ru/jour/article/view/1824</self-uri><abstract><p>В работе показано, что формирование ортогональных систем открытых макротрещин (отрывы) осадочных бассейнов может происходить на стадии диагенеза за время в первые сотни лет для небольшого диапазона глубин шельфа (до 100 м) в процессе осадконакопления. В этот период идет вязкое изотропное уплотнение осадков и медленное отжатие излишков воды, определяющее уменьшение упругого коэффициента Пуассона от значений, близких к 0.5, до значений 0.3–0.2. Из-за этого в осадках, напряженное состояние которых практически полностью определяется только силой тяжести вышележащих пород, происходит снижение на 50 % и более уровня напряжений горизонтального сжатия от начального литостатического уровня давления. С другой стороны, в случае достижения предела псевдопластического течения в породе происходит вертикальное уплотнение, со­провождающееся ростом горизонтального сжатия. Эти два конкурирующих процесса вместе с фактором флюидного давления в трещинах и порах определяют возможность формирования хрупких трещин отрыва. Показано, что в породах, имеющих низкий уровень предела текучести (глины), уплотнение на стадии псевдопластического течения приводит к повышению уровня напряжений горизонтального сжатия, из-за чего хрупкое разрушение в них на стадии диагенеза становится невозможным. В породах, обладающих высоким уровнем сдвиговой прочности (песчаник, известняк), хрупкое разрушение из-за превышения давления воды в субвертикальных микротрещинах начинается раньше, чем достижение предела текучести.</p></abstract><trans-abstract xml:lang="en"><p>The paper shows that the formation of orthogonal systems of open macrofractures (cleavages) of sedimentary basins can occur at the stage of diagenesis during the first hundreds of years for a small range of shelf depths (up to 100 m) during sedimentation. During this period, sediments are compacted and the excess water is slowly squeezed out, which determines the decrease in the Poisson’s ratio from values close to 0.5 to values 0.3–0.2. Because of this, in sediments, the stress state of which is almost completely determined only by the gravity of the overlying rocks, is reduced by 50 % or more of the horizontal compression stress level from the initial lithostatic pressure level. On the other hand, if the limit of pseudoplastic flow is reached in the rock, vertical compaction occurs, accompanied by an increase in horizontal compression. These two competing processes together with the factor of fluid pressure in fractures and pores determine the possibility of brittle fracture formation. It is shown that for rocks with a low level of yield strength (clay), compaction leads to an increase in the level of horizontal compression stresses, which makes brittle fracture in such rocks at the stage of diagenesis impossible. In rocks with a high level of strength (sandstone, limestone), brittle fracture due to excess water pressure in the sub­vertical microcracks starts earlier than the shear yield limit is reached.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>напряжения</kwd><kwd>коэффициент Пуассона</kwd><kwd>трещины</kwd><kwd>отрывы</kwd><kwd>текучесть</kwd><kwd>осадки</kwd><kwd>диагенез</kwd></kwd-group><kwd-group xml:lang="en"><kwd>stresses</kwd><kwd>Poisson’s ratio</kwd><kwd>fractures</kwd><kwd>cleavage</kwd><kwd>fluidity</kwd><kwd>sediments</kwd><kwd>diagenesis</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках госзадания ИФЗ РАН.</funding-statement><funding-statement xml:lang="en">The study was done as part of the state assignment of the IPE RAS.</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Aydin A., 2014. 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