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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>Research Article</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 core analysis</article-title></title-group><contrib-group><contrib contrib-type="author"><name name-style="western"><surname>Khassenov</surname><given-names>Askhat G.</given-names></name><email>a.khassenov@kmg.kz</email><uri content-type="orcid">https://orcid.org/0009-0009-7933-4321</uri><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author"><name name-style="western"><surname>Uteyev</surname><given-names>Rakhim N.</given-names></name><bio>&lt;p&gt;PhD&lt;/p&gt;</bio><email>r.uteyev@kmge.kz</email><uri content-type="orcid">https://orcid.org/0000-0003-3461-4118</uri><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author"><name name-style="western"><surname>Imanbayev</surname><given-names>Bakhyt A.</given-names></name><email>b.imanbayev@kmge.kz</email><uri content-type="orcid">https://orcid.org/0009-0004-9736-3453</uri><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author"><name name-style="western"><surname>Bassarbay</surname><given-names>Akbota Ye.</given-names></name><email>a.bassarbay@kmge.kz</email><uri content-type="orcid">https://orcid.org/0009-0003-2887-1481</uri><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author"><name name-style="western"><surname>Alexeyeva</surname><given-names>Yekaterina V.</given-names></name><email>e.alexeyeva@kmge.kz</email><uri content-type="orcid">https://orcid.org/0009-0007-3754-1264</uri><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author"><name name-style="western"><surname>Morozov</surname><given-names>Vitaliy N.</given-names></name><email>vmorozov@advnrg-intl.com</email><uri content-type="orcid">https://orcid.org/0009-0004-3592-0058</uri><xref ref-type="aff" rid="aff-4"/></contrib></contrib-group><aff id="aff-1">KazMunayGas</aff><aff id="aff-2">KMG Engineering</aff><aff id="aff-3">Branch of KMG Engineering «KazNIPImunaigaz»</aff><aff id="aff-4">Advantage Energy International – FZCO</aff><pub-date date-type="epub" iso-8601-date="2026-09-30" publication-format="electronic"><day>30</day><month>09</month><year>2026</year></pub-date><volume>8</volume><issue>3</issue><fpage>8</fpage><lpage>19</lpage><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 © 2026, Khassenov A.G., Uteyev R.N., Imanbayev B.A., Bassarbay A.Y., Alexeyeva Y.V., Morozov V.N.</copyright-statement><copyright-year>2026</copyright-year></permissions><abstract>&lt;p&gt;&lt;strong&gt;Background: &lt;/strong&gt;The geological structure of the Jurassic deposits in the Zhetybay East field is characterized by pronounced facies heterogeneity and complex spatial variability of reservoir properties driven by changes in depositional environments. The insufficient understanding of formation patterns and spatial distribution of facies bodies limits the accuracy of geological modeling and the prediction of productive zones. The study and interpretation of facies settings enable a detailed characterization of depositional environments, hydrodynamic regime parameters, and paleoenvironmental conditions, which form the basis for stratigraphic correlation, paleogeographic reconstructions, and applied geological predictions. In this context, there is a need for detailed sedimentological analysis of core material followed by integration of the obtained results with well log data and seismic survey data in order to improve the reliability of interpretation and refine the geological model of the field.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Aim: &lt;/strong&gt;The aim of this study is to determine the facies environments of the Zhetybay East field based on core analysis results.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Materials and Methods:&lt;/strong&gt; Historical data for each well in the field and laboratory results of core material analysis were used as the main sources of information. Core interpretation was performed using a sedimentological approach, including the analysis of lithological composition, textural and structural features, and diagnostic sedimentary structures. Based on the integrated interpretation of core and well data, facies analysis was carried out with the identification of genetic types of deposits and the reconstruction of their formation conditions.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Results:&lt;/strong&gt; As a result of the sedimentological analysis of core material, a facies interpretation of the Jurassic productive deposits of the Zhetybay East field was performed. Based on the study results, the main depositional environments were identified and a conceptual sedimentological model of the productive interval of the section was developed.&lt;/p&gt;&#13;
&lt;p&gt;&lt;strong&gt;Conclusion: &lt;/strong&gt;The obtained results allow refinement of the geological model and improvement of the prediction of productive horizon distribution. In addition, they contribute to increased reliability of stratigraphic correlation. Overall, the data can be used to substantiate directions for further geological exploration and pilot production studies.&lt;/p&gt;</abstract><kwd-group xml:lang="en"><kwd>facies</kwd><kwd>core</kwd><kwd>interpretation</kwd><kwd>delta plain</kwd><kwd>alluvial plain</kwd><kwd>delta front</kwd></kwd-group><kwd-group xml:lang="kk"><kwd>фация</kwd><kwd>керн</kwd><kwd>интерпретация</kwd><kwd>дельта жазығы</kwd><kwd>аллювиалды жазық</kwd><kwd>дельта фронты</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>фация</kwd><kwd>керн</kwd><kwd>интерпретация</kwd><kwd>дельтовая равнина</kwd><kwd>аллювиальная равнина</kwd><kwd>фронт дельты</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Baraboshkin EY. Prakticheskaya sedimentologiya. Terrigennyye rezervuary: posobiye po rabote s kernom. Tver: GERS Publishing; 2011. 152 p. (In Russ).</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>Pemberton GS, MacEachern JA. The Sequence Stratigraphic Significance of Trace Fossils: Examples from the Cretaceous Foreland Basin of Alberta, Canada. In: Van Wagoner JC, Bertram GT, editors. Sequence Stratigraphy of Foreland Basin Deposits: Outcrop and Subsurface Examples from the Cretaceous of North America. Tulsa: American Association of Petroleum Geologists; 1995. Vol. 64. P:429–475.</mixed-citation></ref><ref id="B3"><label>3.</label><mixed-citation>Allen JRL. Sedimentary Structures: Their Character and Physical Basis. Vol. I. In: Allen JRL, editor. Developments in Sedimentology. 30A. Amsterdam: Elsevier; 1982. 593 p.</mixed-citation></ref><ref id="B4"><label>4.</label><mixed-citation>Allen JRL. Sedimentary Structures: Their Character and Physical Basis. Vol. II. In: Allen JRL, editor. Developments in Sedimentology. 30B. Amsterdam: Elsevier; 1982. 663 p.</mixed-citation></ref><ref id="B5"><label>5.</label><mixed-citation>Buatois LA, Mángano MG. Ichnology: Organism–Substrate Interactions in Space and Time. Cambridge University Press; 2011. 370 p.</mixed-citation></ref><ref id="B6"><label>6.</label><mixed-citation>Li S, Ma YZ, Yu X, Li S. Reservoir potential of deep-water lacustrine delta-front sandstones in the Upper Triassic Yanchang Formation, western Ordos Basin, China. Journal of Petroleum Geology. 2017;40(1):105–118. doi: 10.1111/jpg.12666.</mixed-citation></ref><ref id="B7"><label>7.</label><mixed-citation>Bhattacharya JP. Deltas. In: James NP, Dalrymple RW, editors. Facies Models 4. Geoscience Canada; 2011. P:237–292.</mixed-citation></ref><ref id="B8"><label>8.</label><mixed-citation>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="B9"><label>9.</label><mixed-citation>Robertson Research International Limited. OISC Uzenmunaigas (UMG), Well: GU57-6602. Conventional core analysis report. Report No. AF713. 2002.</mixed-citation></ref><ref id="B10"><label>10.</label><mixed-citation>Alpheus S, Hajek E. The fate of bars in braided rivers. The Sedimentary Record. 2024;22(1). doi: 10.2110/001c.117787.</mixed-citation></ref><ref id="B11"><label>11.</label><mixed-citation>Wheeler DM, Scott AJ, Coringrato VJ, Devine PE. Stratigraphy and depositional history of the Morrow Formation, southeast Colorado and southwest Kansas. In: Sonnenberg SA, Shannon LT, Rader K, et al, editors. Morrow Sandstones of Southeast Colorado and Adjacent Areas: The Rocky Mountain Association of Geologists. Special Paper; 1990. P:3–35.</mixed-citation></ref><ref id="B12"><label>12.</label><mixed-citation>Allen GP, Posamentier HW. Sequence stratigraphy and facies model of an incised valley fill: the Gironde Estuary, France. Journal of Sedimentary Petrology. 1993;63(3):378–391. doi: 10.1306/d4267b09-2b26-11d7-8648000102c1865d.</mixed-citation></ref><ref id="B13"><label>13.</label><mixed-citation>Howell JA, Skorstad A, MacDonald A, et al. Sedimentological parameterization of shallow-marine reservoir. Petroleum Geoscience. 2008;14(1):17–34. doi: 10.1144/1354-079307-787.</mixed-citation></ref></ref-list></back></article>
