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<article 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" article-type="research-article" dtd-version="1.1d1" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher">Kazakhstan journal for oil &amp; gas industry</journal-id><journal-title-group><journal-title>Kazakhstan journal for oil &amp; gas industry</journal-title></journal-title-group><issn publication-format="print">2707-4226</issn><issn publication-format="electronic">2957-806X</issn><publisher><publisher-name>KMG Engineering</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">108953</article-id><article-id pub-id-type="doi">10.54859/kjogi108953</article-id><article-categories><subj-group subj-group-type="heading"><subject></subject></subj-group></article-categories><title-group><article-title>Conceptual model for the formation of jurassic deposits of the Zhetybay East field based on sedimentological analysis of core data</article-title></title-group><contrib-group><contrib contrib-type="author"><name name-style="western"><surname>Bassarbay</surname><given-names>Akbota</given-names></name><email>A.Bassarbay@kmge.kz</email><uri content-type="orcid">https://orcid.org/0009-0003-2887-1481</uri></contrib><contrib contrib-type="author"><name name-style="western"><surname>Morozov</surname><given-names>Vitalii Nikolaevich</given-names></name><email>vmorozov@advnrg-ntl.com</email><uri content-type="orcid">https://orcid.org/0009-0004-3592-0058</uri></contrib><contrib contrib-type="author"><name name-style="western"><surname>Alexeyeva</surname><given-names>Yekaterina Vasilevna</given-names></name><email>e.alexeyeva@kmge.kz</email><uri content-type="orcid">https://orcid.org/0009-0007-3754-1264</uri></contrib></contrib-group><volume>8</volume><issue>3</issue><history><pub-date date-type="received" iso-8601-date="2026-02-16"><day>16</day><month>02</month><year>2026</year></pub-date><pub-date date-type="accepted" iso-8601-date="2026-06-17"><day>17</day><month>06</month><year>2026</year></pub-date></history><permissions><copyright-statement>Copyright © , Bassarbay A., Morozov V.N., Alexeyeva Y.V.</copyright-statement></permissions><abstract>&lt;p&gt;&lt;strong&gt;A&lt;/strong&gt;&lt;strong&gt;BSTRACT&lt;/strong&gt;&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Background&lt;/strong&gt;&lt;strong&gt;.&lt;/strong&gt; The present study is aimed at integrating core and to refine the lithological framework, identify the main facies environments, and develop a conceptual sedimentological model, which is important for predicting the distribution of productive zones.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Aim&lt;/strong&gt;&lt;strong&gt;. &lt;/strong&gt;Determination of the facies environments of the Zhetybay East field based on core studies. The study and interpretation of facies environments allow for a detailed characterization of the geological conditions of sedimentation, the parameters of the hydrodynamic regime, and the features of the paleoenvironment, which serve as a basis for stratigraphic correlation, paleogeographic reconstructions, and applied geological predictions.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Materials and methods&lt;/strong&gt;&lt;strong&gt;. &lt;/strong&gt;The primary sources of information include historical data for each well in the field, results of laboratory studies (both standard and specialized) of core samples from three wells.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Results&lt;/strong&gt;&lt;strong&gt;. &lt;/strong&gt;As a result of a comprehensive analysis of core materials, a facies interpretation of the Jurassic productive deposits of the Zhetybay East field was performed. The study identified the main facies environments of sedimentation and resulted in the development of a conceptual model of the field.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Conclusion&lt;/strong&gt;&lt;strong&gt;.&lt;/strong&gt; A facies interpretation of the Jurassic deposits of the Zhetybay East field was carried out based on core analysis. The results obtained allow for refinement of the geological model and prediction of the distribution of productive horizons.&lt;/p&gt;</abstract><kwd-group xml:lang="en"><kwd>deposits, facies, core, interpretation.</kwd></kwd-group><kwd-group xml:lang="kk"><kwd>кен орны, фация, керн, интерпретация.</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>месторождения, фация, керн, интерпретация.</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>1.	 Baraboshkin EY. Practical sedimentology. Terrigenous reservoirs. Core workshop manual. Tver: GERS Publishing; 2011. 152 p.</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>2. Pemberton SG, MacEachern JA. The sequence stratigraphic significance of trace fossils in examples from the Cretaceous of Alberta. In: Van Wagoner JC, Bertram GT, editors. Sequence stratigraphy of foreland basin deposits: outcrop and subsurface examples from the Cretaceous of North America. Tulsa (OK): American Association of Petroleum Geologists; 1995. p. 429–475.</mixed-citation></ref><ref id="B3"><label>3.</label><mixed-citation>3. Allen JRL. Sedimentary structures: their character and physical basis. Vol. 1. Amsterdam: Elsevier Scientific Publishing Company; 1982. 593 p.</mixed-citation></ref><ref id="B4"><label>4.</label><mixed-citation>4. Allen JRL. Sedimentary structures: their character and physical basis. Vol. 2. Amsterdam: Elsevier Scientific Publishing Company; 1982. 663 p.</mixed-citation></ref><ref id="B5"><label>5.</label><mixed-citation>5. Buatois LA, Mángano MG. Ichnology: organism–substrate interactions in space and time. Cambridge: Cambridge University Press; 2011.</mixed-citation></ref><ref id="B6"><label>6.</label><mixed-citation>6. Walker RG, James NP. Facies models: response to sea level change. St. John’s: Geological Association of Canada; 1992. 454 p.</mixed-citation></ref><ref id="B7"><label>7.</label><mixed-citation>7. Bhattacharya JP. Deltas. In: James NP, Dalrymple RW, editors. Facies models 4. St. John’s: Geological Association of Canada; 2012. p. 237–292.</mixed-citation></ref></ref-list></back></article>
