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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10069664"> <a href="/gui2/?type=authors&mode=browse&sel=10069664" target="_blank">Hasan, Muhammad Luqman ✉</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10001322"> <a href="/gui2/?type=authors&mode=browse&sel=10001322" target="_blank">M. Tóth, Tivadar</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;33720723" mtid="33720723" target="_blank">Localization of potential migration pathways inside a fractured metamorphic hydrocarbon reservoir using well log evaluation (Mezősas field, Pannonian Basin)</a></div> <div class="pub-info"> <span class="journal-title">GEOENERGY SCIENCE AND ENGINEERING</span> <span class="journal-volume">225</span> <span class="page"> Paper: 211710 , 22 p. </span> <span class="year">(2023)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.geoen.2023.211710" target="_blank" href="https://doi.org/10.1016/j.geoen.2023.211710"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001043034500001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001043034500001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85159761310" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85159761310"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="https://linkinghub.elsevier.com/retrieve/pii/S294989102300297X" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S294989102300297X"> Egyéb URL </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:blue" title="27397" target="_blank" href="http://publicatio.bibl.u-szeged.hu/27397"> SZTE Publicatio </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:33720723 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: National Research, Development and Innovation Office, Hungary [K-138919]
Funding text: Funding This study was supported by the National Research, Development and Innovation Office, Hungary (grant no. K-138919) .</pre>
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Currently, metamorphic rock is a common target for natural gas exploration, and reservoirs are the key factors restricting natural gas exploration and development in metamorphic rocks. The deep metamorphic rock gas reservoir in the central paleo-uplift of the northern Songliao Basin has good exploration and development potential. In this study, we use a combination of qualitative descriptions and quantitative analysis to comprehensively analyze the pore characteristics of the reservoir and explore the factors controlling the pore characteristics of the metamorphic rock reservoir in the central paleo-uplift belt of the Songliao Basin. The metamorphic rock reservoir in the central paleo-uplift belt contains three types of lithologies: chlorite schist, mica schist and mylonite, each with different protoliths and metamorphic histories. The results of high-pressure mercury intrusion and nitrogen adsorption indicate that the pore size distributions of the schist and mylonite differ. Compared with the mylonite, the schist has larger reservoir space, more heterogeneity, smaller pore size, larger specific surface area and larger adsorbed gas storage capacity. This paper also studies the formation process of the reservoir and divides it into four stages. Finally, this article discusses in detail the factors controlling the microscopic pore characteristics of metamorphic rock reservoirs in the central paleo-uplift belt; the metamorphic rock protolith is the most important controlling factor.
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College of Geology and Mining Engineering, Xinjiang University, Urumqi, 830046, China
Shandong Key Laboratory of Depositional Mineralization & Sedimentary Mineral, Shandong University of Science and Technology, Qingdao, Shandong 266590, China
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong 266590, China
Research Institute of Exploration and Development, Xinjiang Oilfield Company, Karamay, 834000, China
Exploration Division of PetroChina Tarim Oilfield Company, Xinjiang, Korla, 841000, China
Cited By :2
Export Date: 18 April 2021
Correspondence Address: Tian, J.; College of Geology and Mining Engineering, China; email: tianxju@yahoo.com
Funding details: 41972176, U1903207
Funding details: XJEDU 2019Y011
Funding details: DMSM20190021
Funding details: PetroChina Company Limited, PetroChina
Funding text 1: The authors gratefully acknowledge the financial support received from the China National Science Fund (Grant Nos. 41972176 and U1903207 ), the Scientific Research Projects in Universities in Xinjiang Autonomous Region (Grant No. XJEDU 2019Y011 ), and the Shandong Key Laboratory of Depositional Mineralization & Sedimentary Mineral Open Fund (Grant No. DMSM20190021 ). We are grateful to the anonymous reviewers for their insightful and constructive comments for improving the manuscript. We also thank the Xinjiang Oil Field, PetroChina, for providing data.
Funding text 2: The authors gratefully acknowledge the financial support received from the China National Science Fund (Grant Nos. 41972176 and U1903207), the Scientific Research Projects in Universities in Xinjiang Autonomous Region (Grant No. XJEDU 2019Y011), and the Shandong Key Laboratory of Depositional Mineralization & Sedimentary Mineral Open Fund (Grant No. DMSM20190021). We are grateful to the anonymous reviewers for their insightful and constructive comments for improving the manuscript. We also thank the Xinjiang Oil Field, PetroChina, for providing data.
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Metamorphic rock reservoirs are special reservoirs that are quite different from traditional sedimentary rock reservoirs and contain rich hydrocarbon reserves. However, their lithofacies characteristics and reservoir properties are relatively underexplored, and the key factor in reservoirs is lithofacies. Based on core samples, thin sections, whole-rock analysis and well-log and seismic data, we evaluated the lithologies, petrological characteristics and reservoir properties of metamorphic rocks and then explored the main factors controlling reservoir formation and metamorphic rock quality in the Aryskum depression, South Turgay Basin, Kazakhstan. In this area, four types of lithofacies are identified: granitic gneiss (high DEN and CN, low GR), leptite (high GR and CN), gabbro (low GR and CN) and granite (high GR and low CN); among these rocks, granitic gneiss is widely distributed. The reservoir spaces of metamorphic rocks are divided into fractures and pores produced via metamorphism and structural movements. Fractures can be subdivided into structural fractures (SFs), dissolution fractures (DFs), cleavage microfissures (CMfs) and microfissures (Mfs), and pores include dissolved intergranular pores (DInterPs), dissolved intragranular pores (DIntrPs) and vugs (Vgs). Numerous SFs and DFs provide the main reservoir spaces for hydrocarbons. The reservoir quality of metamorphic rocks is primarily controlled by faults, fractures, lithofacies, minerals, dissolution and paleogeomorphology. Lithofacies and minerals are the internal factors that control dissolution and fragmentation, while paleogeomorphology and faults are the external factors that control fracture development. Leptite and granitic gneiss are high-quality reservoir lithofacies, and high paleogeomorphology areas and fault zones are the optimal locations for fractures and pores. Reservoir spaces undergo a series of repeated changes from formation to development, filling and reformation, and a comprehensive reservoir evolution model is proposed to illustrate the distribution of high-quality reservoirs. This study has scientific significance for investigating the reservoir-forming mechanisms of metamorphic rocks and practical applications for exploring and developing oil and gas fields in areas with metamorphic rocks.
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<span class="author-name" >Huan Zhipeng
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<span class="author-name" >Feng Shuo
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;31453490" target="_blank">Lithofacies characteristics and their controlling effects on reservoirs in buried hills of metamorphic rocks: A case study of late Paleozoic units in the Aryskum depression, South Turgay Basin, Kazakhstan</a></div> <div> <span class="journal-title">JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: College of Geology and Mining Engineering, Xinjiang University, Urumqi, 830046, China
Shandong Key Laboratory of Depositional Mineralization & Sedimentary Mineral, Shandong University of Science and Technology, Qingdao, Shandong 266590, China
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong...</pre>
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Localisation of ductile and brittle shear zones along the Szentlőrinc-1 well in the Mecsekalja Zone using quartz microstructural and well-log data
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10038186"> <a href="/gui2/?type=authors&mode=browse&sel=10038186" target="_blank">Skultéti, Á</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10001322"> <a href="/gui2/?type=authors&mode=browse&sel=10001322" target="_blank">M, Tóth T</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;2949640" mtid="2949640" target="_blank">Localisation of ductile and brittle shear zones along the Szentlőrinc-1 well in the Mecsekalja Zone using quartz microstructural and well-log data</a></div> <div class="pub-info"> <span class="journal-title">ACTA GEODAETICA ET GEOPHYSICA</span> <span class="journal-volume">51</span> : <span class="journal-issue">2</span> <span class="page"> pp. 295-314. , 20 p. </span> <span class="year">(2016)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_PAY" title=" Fizetős "> <a style="color:blue" title="10.1007/s40328-015-0127-3" target="_blank" href="https://doi.org/10.1007/s40328-015-0127-3"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000375597500011" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000375597500011"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="84971265214" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-84971265214"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="http://link.springer.com/article/10.1007/s40328-015-0127-3" target="_blank" href="http://link.springer.com/article/10.1007/s40328-015-0127-3"> Teljes dokumentum </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:blue" title="11496" target="_blank" href="http://publicatio.bibl.u-szeged.hu/11496"> SZTE Publicatio </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:2949640 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 2</span> | Független: 1 | Függő: 1 | Nem jelölt: 0 | WoS jelölt: 1 | Scopus jelölt: 2 | WoS/Scopus jelölt: 2 | DOI jelölt: 2 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png">
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<div class="autype autype0"> <span class="author-name" mtid="10038186"><a
href="/gui2/?type=authors&mode=browse&sel=10038186" target="_blank">Skultéti Á
(<span class="authorship-author-name">Skultéti Ágnes</span>
<span class="authorAux-mtmt"> Geológia</span>)
</a>
</span>
<span class="author-affil"><span title="Szegedi Tudományegyetem">SZTE</span>/<span title="Természettudományi és Informatikai Kar">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Ásványtani, Geokémiai és Kőzettani Tanszék</span>
;
<span class="author-name" mtid="10001322"><a
href="/gui2/?type=authors&mode=browse&sel=10001322" target="_blank">M Tóth T
(<span class="authorship-author-name">M. Tóth Tivadar</span>
<span class="authorAux-mtmt"> Kőzettan</span>)
</a>
</span>
<span class="author-affil"><span title="Szegedi Tudományegyetem">SZTE</span>/<span title="Természettudományi és Informatikai Kar">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Ásványtani, Geokémiai és Kőzettani Tanszék</span>
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</div>
<div class="title"><a href="/gui2/?mode=browse¶ms=publication;2949640" target="_blank">Localisation of ductile and brittle shear zones along the Szentlőrinc-1 well in the Mecsekalja Zone using quartz microstructural and well-log data</a></div> <div> <span class="journal-title">ACTA GEODAETICA ET GEOPHYSICA</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/2213-5812">2213-5812</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/2213-5820">2213-5820</a>)</span>:
<span class="journal-volume">51</span> <span class="journal-issue">2</span>
<span class="page">
pp 295-314
</span> <span class="year">(2016)</span>
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<div class="pub-footer">
<span class="language" xmlns="http://www.w3.org/1999/html">Nyelv:
Angol
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<span class="identifiers">
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<a style="color:blue" title="10.1007/s40328-015-0127-3" target="_blank" href="https://doi.org/10.1007/s40328-015-0127-3">
DOI
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<a style="color:blue" title="000375597500011" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000375597500011">
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Scopus
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<a style="color:black" title="http://link.springer.com/article/10.1007/s40328-015-0127-3" target="_blank" href="http://link.springer.com/article/10.1007/s40328-015-0127-3">
Teljes dokumentum
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</span>
<span class="id identifier oa_GREEN" title=" Green
">
<a style="color:blue" title="11496" target="_blank" href="http://publicatio.bibl.u-szeged.hu/11496">
SZTE Publicatio
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<div class="publication-citation" style="margin-left: 0.5cm;">
<span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 2</span>
| Független: 1
| Függő: 1
| Nem jelölt: 0
| WoS jelölt: 1
| Scopus jelölt: 2
| WoS/Scopus jelölt: 2
| DOI jelölt: 2
</div>
<div class="publication-citation">
<a target="_blank" href="/api/publication?cond=citations.related;eq;2949640&sort=publishedYear,desc&sort=title">
Idézett közlemények száma: 18
</a>
</div>
<div class="mtid"><span class="long-pub-mtid">Közlemény: 2949640</span>
| <span class="status-data status-VALIDATED"> Egyeztetett
</span>
<span class="oldId">Régi azonosító: 2949640</span> |
Forrás Idéző
| <span class="type-subtype">Folyóiratcikk
( Szakcikk
)
</span>
| <span class="pub-category">Tudományos</span>
| <span class="publication-sourceOfData">kézi felvitel</span>
</div>
<div class="lastModified">Utolsó módosítás: 2020.04.16. 11:27 Nemec Évi (MTMT Központi 3, admin)
</div>
<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :2
Export Date: 12 February 2021
Correspondence Address: Skultéti, Á.; Department of Mineralogy Geochemistry and Petrology, Hungary; email: skulteti.agi@gmail.com
Cited By :2
Export Date: 18 April 2021
Correspondence Address: Skultéti, Á.; Department of Mineralogy Geochemistry and Petrology,...</pre>
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