Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China
Through a range of petrological techniques, the petrology, diagenesis, pore characteristics, and controlling factors on the regional variations of reservoir quality of the Chang 7 sandstones were studied. These sandstones, mainly arkoses, lithic arkoses, and feldspathic litharenites, were deposited...
- Autores:
-
Zhu, Haihua
Liu, Guangchen
Zhong, Dakang
Zhang, Tingshan
Lang, Jun
Yao, Jingli
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2018
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/68585
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/68585
http://bdigital.unal.edu.co/69618/
- Palabra clave:
- 55 Ciencias de la tierra / Earth sciences and geology
Diagenesis
tight sandstone
reservoir quality
Ordos Basin
Diagénesis
arenisca apretada
calidad del yacimiento
Cuenca de Ordos
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
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dc.title.spa.fl_str_mv |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China |
title |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China |
spellingShingle |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China 55 Ciencias de la tierra / Earth sciences and geology Diagenesis tight sandstone reservoir quality Ordos Basin Diagénesis arenisca apretada calidad del yacimiento Cuenca de Ordos |
title_short |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China |
title_full |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China |
title_fullStr |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China |
title_full_unstemmed |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China |
title_sort |
Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China |
dc.creator.fl_str_mv |
Zhu, Haihua Liu, Guangchen Zhong, Dakang Zhang, Tingshan Lang, Jun Yao, Jingli |
dc.contributor.author.spa.fl_str_mv |
Zhu, Haihua Liu, Guangchen Zhong, Dakang Zhang, Tingshan Lang, Jun Yao, Jingli |
dc.subject.ddc.spa.fl_str_mv |
55 Ciencias de la tierra / Earth sciences and geology |
topic |
55 Ciencias de la tierra / Earth sciences and geology Diagenesis tight sandstone reservoir quality Ordos Basin Diagénesis arenisca apretada calidad del yacimiento Cuenca de Ordos |
dc.subject.proposal.spa.fl_str_mv |
Diagenesis tight sandstone reservoir quality Ordos Basin Diagénesis arenisca apretada calidad del yacimiento Cuenca de Ordos |
description |
Through a range of petrological techniques, the petrology, diagenesis, pore characteristics, and controlling factors on the regional variations of reservoir quality of the Chang 7 sandstones were studied. These sandstones, mainly arkoses, lithic arkoses, and feldspathic litharenites, were deposited in a delta front and turbidites in semi-deep to deep lacustrine. The detrital constituents were controlled by the provenance and sedimentary condition, which resulted in a spatially variable composition; e.g., high biotite and feldspar contents in the northeast (NE) of the study area, and high contents of rock fragments, especially dolomite, matrix, and quartz in the southwest (SW). Diagenesis includes intense mechanical compaction, cementation, and dissolution of unstable minerals. Diagenetic minerals which were derived internally include quartz, ankerite, ferrous calcite, albite, illite, kaolinite, and chlorite. Thus the original sandstone composition hadfirm control over the development and distribution of cement. Mechanical compaction and late-stage cementations contribute to the porosity loss of sandstones of Chang7 member. The dissolution porosity in major sandstone, slightly higher than primary porosity is principally dependent on the accessibility of acid fluid. The high content of plastic component facilitated the reduction of primary porosity and limited the mineral dissolution. The best reservoir sandstones are found in W, and partly from NE, M districts, with porosity are primary. The relatively high textural maturity of these sandstones reduces the impact of compaction on primary pores, and commonly existed chlorite rims limited the precipitation of pore filling quartz and carbonate cementation in late stage. |
publishDate |
2018 |
dc.date.issued.spa.fl_str_mv |
2018-04-01 |
dc.date.accessioned.spa.fl_str_mv |
2019-07-03T07:12:08Z |
dc.date.available.spa.fl_str_mv |
2019-07-03T07:12:08Z |
dc.type.spa.fl_str_mv |
Artículo de revista |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.content.spa.fl_str_mv |
Text |
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http://purl.org/redcol/resource_type/ART |
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http://purl.org/coar/resource_type/c_6501 |
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publishedVersion |
dc.identifier.issn.spa.fl_str_mv |
ISSN: 2339-3459 |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.unal.edu.co/handle/unal/68585 |
dc.identifier.eprints.spa.fl_str_mv |
http://bdigital.unal.edu.co/69618/ |
identifier_str_mv |
ISSN: 2339-3459 |
url |
https://repositorio.unal.edu.co/handle/unal/68585 http://bdigital.unal.edu.co/69618/ |
dc.language.iso.spa.fl_str_mv |
spa |
language |
spa |
dc.relation.spa.fl_str_mv |
https://revistas.unal.edu.co/index.php/esrj/article/view/72251 |
dc.relation.ispartof.spa.fl_str_mv |
Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research Journal Earth Sciences Research Journal |
dc.relation.references.spa.fl_str_mv |
Zhu, Haihua and Liu, Guangchen and Zhong, Dakang and Zhang, Tingshan and Lang, Jun and Yao, Jingli (2018) Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China. Earth Sciences Research Journal, 22 (2). pp. 129-138. ISSN 2339-3459 |
dc.rights.spa.fl_str_mv |
Derechos reservados - Universidad Nacional de Colombia |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.license.spa.fl_str_mv |
Atribución-NoComercial 4.0 Internacional |
dc.rights.uri.spa.fl_str_mv |
http://creativecommons.org/licenses/by-nc/4.0/ |
dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Atribución-NoComercial 4.0 Internacional Derechos reservados - Universidad Nacional de Colombia http://creativecommons.org/licenses/by-nc/4.0/ http://purl.org/coar/access_right/c_abf2 |
eu_rights_str_mv |
openAccess |
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application/pdf |
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Universidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geociencia |
institution |
Universidad Nacional de Colombia |
bitstream.url.fl_str_mv |
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Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Zhu, Haihua223bfe56-4695-4ada-9b28-cce14801804c300Liu, Guangchen248f406a-132e-49fd-9399-b2565dad3da7300Zhong, Dakang79711e70-3d73-4e12-8a8b-77a2842947ab300Zhang, Tingshan13ec229a-d808-4f1c-b70b-f075e62dd49a300Lang, Jund5851868-4db2-4c9b-ba69-10e7342f00d0300Yao, Jingli12770f9e-7667-4a78-a17c-e2b90fd53ba43002019-07-03T07:12:08Z2019-07-03T07:12:08Z2018-04-01ISSN: 2339-3459https://repositorio.unal.edu.co/handle/unal/68585http://bdigital.unal.edu.co/69618/Through a range of petrological techniques, the petrology, diagenesis, pore characteristics, and controlling factors on the regional variations of reservoir quality of the Chang 7 sandstones were studied. These sandstones, mainly arkoses, lithic arkoses, and feldspathic litharenites, were deposited in a delta front and turbidites in semi-deep to deep lacustrine. The detrital constituents were controlled by the provenance and sedimentary condition, which resulted in a spatially variable composition; e.g., high biotite and feldspar contents in the northeast (NE) of the study area, and high contents of rock fragments, especially dolomite, matrix, and quartz in the southwest (SW). Diagenesis includes intense mechanical compaction, cementation, and dissolution of unstable minerals. Diagenetic minerals which were derived internally include quartz, ankerite, ferrous calcite, albite, illite, kaolinite, and chlorite. Thus the original sandstone composition hadfirm control over the development and distribution of cement. Mechanical compaction and late-stage cementations contribute to the porosity loss of sandstones of Chang7 member. The dissolution porosity in major sandstone, slightly higher than primary porosity is principally dependent on the accessibility of acid fluid. The high content of plastic component facilitated the reduction of primary porosity and limited the mineral dissolution. The best reservoir sandstones are found in W, and partly from NE, M districts, with porosity are primary. The relatively high textural maturity of these sandstones reduces the impact of compaction on primary pores, and commonly existed chlorite rims limited the precipitation of pore filling quartz and carbonate cementation in late stage.A través de una gama de técnicas petrológicas se estudió la petrología, la diagénesis, las características de poro y los factores que controlan las variaciones regionales de la calidad del yacimiento de las areniscas Chang 7. Estas areniscas, principalmente arcosas, arcosas líticas y arenitas líticas feldespáticas, se depositaron en un frente deltáico mientras las turbiditas se depositaron en ambientes lacustres profundos y semi-profundos. Los componentes detríticos dependen de la procedencia y la condición sedimentaria, lo que resultó en una composición variable en el espacio; por ejemplo, altos contenidos de biotita y feldespato en el noreste (NE) del área de estudio, y altos contenidos de fragmentos de roca, especialmente dolomita, matriz y cuarzo en el suroeste (SW). La diagénesis incluye compactación mecánica intensa, cementación y disolución de minerales inestables. Los minerales diagenéticos que se derivaron internamente incluyen cuarzo, ankerita, calcita ferrosa, albita, illita, caolinita y clorita. Por lo tanto, la composición original de arenisca tenía un firme control sobre el desarrollo y la distribución del cemento. La compactación mecánica y las cementaciones de la última etapa contribuyen a la pérdida de porosidad de las areniscas del miembro Chang7. La porosidad de disolución en la piedra arenisca principal, ligeramente más alta que la porosidad primaria, depende principalmente de la accesibilidad del fluido ácido. El alto contenido de componentes plásticos facilitó la reducción de la porosidad primaria y limitó la disolución del mineral. Las mejores areniscas de yacimiento se encuentran en los distritos Occidental, y en parte de los distritos Noroeste y Medio, con niveles primarios de porosidad. La madurez textural relativamente alta de estas areniscas reduce el impacto de la compactación en los poros primarios, y los bordes de clorito comúnmente existentes limitaron la precipitación del cuarzo de llenado de poros y la cementación de carbonato en la etapa tardía.application/pdfspaUniversidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geocienciahttps://revistas.unal.edu.co/index.php/esrj/article/view/72251Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research JournalEarth Sciences Research JournalZhu, Haihua and Liu, Guangchen and Zhong, Dakang and Zhang, Tingshan and Lang, Jun and Yao, Jingli (2018) Diagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, China. Earth Sciences Research Journal, 22 (2). pp. 129-138. ISSN 2339-345955 Ciencias de la tierra / Earth sciences and geologyDiagenesistight sandstonereservoir qualityOrdos BasinDiagénesisarenisca apretadacalidad del yacimientoCuenca de OrdosDiagenetic controls on reservoir quality of tight sandstone: A case study of the Upper Triassic Yanchang formation Chang 7 sandstones, Ordos Basin, ChinaArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTORIGINAL72251-391104-5-PB.pdfapplication/pdf3217772https://repositorio.unal.edu.co/bitstream/unal/68585/1/72251-391104-5-PB.pdfd91f07edd7d9d2a3f1ca827c94c08231MD51THUMBNAIL72251-391104-5-PB.pdf.jpg72251-391104-5-PB.pdf.jpgGenerated Thumbnailimage/jpeg8085https://repositorio.unal.edu.co/bitstream/unal/68585/2/72251-391104-5-PB.pdf.jpg22c02c18b50394f102c38be8a1a9b6b5MD52unal/68585oai:repositorio.unal.edu.co:unal/685852024-05-27 23:09:40.096Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co |