Features and Controlling Factors of Epigenic Karstification of the Ordovician Carbonates in Akekule Arch, Tarim Basin
ABSTRACT： Tabei （塔北） uplift is an area with the highest hydrocarbon enrichment in Tarim basin, and large oilfields have been found on Akekule （阿克库勒） arch at the middle section of Tabei uplift, with Ordovician carbonate reservoirs. Storage space of the Ordovician carbonate reservoirs in the Akekule a...
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| Veröffentlicht in: | Journal of earth science (Wuhan, China) China), 2012-08, Vol.23 (4), p.506-515 |
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| creator | 陈强路 赵永强 李国蓉 储呈林 王斌 |
| description | ABSTRACT： Tabei （塔北） uplift is an area with the highest hydrocarbon enrichment in Tarim basin, and large oilfields have been found on Akekule （阿克库勒） arch at the middle section of Tabei uplift, with Ordovician carbonate reservoirs. Storage space of the Ordovician carbonate reservoirs in the Akekule arch are mainly caves, pores and fractures resulted from dissolution and/or karstification. The Ordovician carbonate reservoirs are affected and modified by the diagenetie process in penecontemporaneous, epigenetic and burial periods and the multi-stage karstification related with deep hydrothermal activities, among which the most significant effect is from the meteoric water karstification related to the tectonic uplift from the end of Middle Ordovician to the end of Late Ordovician （end of O2-end of 03） and at the end of Middle Devonian （end of D2）. Varied palacogeologic settings and tectonic features at different geologic periods lead to different fluid flowing patterns, karstification mechanisms and transformation features in different regions, which further influence the reservoir distribution. The paleo-uplifts at different periods, such as end of O2-end of 03 and end of D2, control the dominant development zones of karstification; the paleogeomorphology and faults resulted from tectonic uplift control the flowing depth of the karst fluid; and the lithology controls the position and extent of karst development. |
| doi_str_mv | 10.1007/s12583-012-0271-4 |
| format | Article |
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Storage space of the Ordovician carbonate reservoirs in the Akekule arch are mainly caves, pores and fractures resulted from dissolution and/or karstification. The Ordovician carbonate reservoirs are affected and modified by the diagenetie process in penecontemporaneous, epigenetic and burial periods and the multi-stage karstification related with deep hydrothermal activities, among which the most significant effect is from the meteoric water karstification related to the tectonic uplift from the end of Middle Ordovician to the end of Late Ordovician （end of O2-end of 03） and at the end of Middle Devonian （end of D2）. Varied palacogeologic settings and tectonic features at different geologic periods lead to different fluid flowing patterns, karstification mechanisms and transformation features in different regions, which further influence the reservoir distribution. The paleo-uplifts at different periods, such as end of O2-end of 03 and end of D2, control the dominant development zones of karstification; the paleogeomorphology and faults resulted from tectonic uplift control the flowing depth of the karst fluid; and the lithology controls the position and extent of karst development.</description><identifier>ISSN: 1674-487X</identifier><identifier>EISSN: 1867-111X</identifier><identifier>DOI: 10.1007/s12583-012-0271-4</identifier><language>eng</language><publisher>China University of Geosciences: China University of Geosciences</publisher><subject>Arches ; Basins ; Biogeosciences ; Carbonates ; Caves ; Devonian ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Fluid dynamics ; Fluid flow ; Geochemistry ; Geology ; Geotechnical Engineering & Applied Earth Sciences ; Hydrocarbons ; Karst ; Lithology ; Meteoric water ; Oil and gas fields ; Ordovician ; Reservoirs ; Rocks ; Tectonics ; 地质构造特征 ; 塔里木盆地 ; 奥陶系 ; 岩溶作用 ; 控制因素 ; 流体流动模式 ; 碳酸盐岩储层 ; 阿克库勒凸起</subject><ispartof>Journal of earth science (Wuhan, China), 2012-08, Vol.23 (4), p.506-515</ispartof><rights>China University of Geosciences and Springer-Verlag Berlin Heidelberg 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a398t-20dd51a4ee4da839981af1742fe73c132d6c737fcd381adb9ad178a7a09d878b3</citedby><cites>FETCH-LOGICAL-a398t-20dd51a4ee4da839981af1742fe73c132d6c737fcd381adb9ad178a7a09d878b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/84134A/84134A.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12583-012-0271-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12583-012-0271-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>陈强路 赵永强 李国蓉 储呈林 王斌</creatorcontrib><title>Features and Controlling Factors of Epigenic Karstification of the Ordovician Carbonates in Akekule Arch, Tarim Basin</title><title>Journal of earth science (Wuhan, China)</title><addtitle>J. Earth Sci</addtitle><addtitle>JOURNAL OF EARTH SCIENCE</addtitle><description>ABSTRACT： Tabei （塔北） uplift is an area with the highest hydrocarbon enrichment in Tarim basin, and large oilfields have been found on Akekule （阿克库勒） arch at the middle section of Tabei uplift, with Ordovician carbonate reservoirs. Storage space of the Ordovician carbonate reservoirs in the Akekule arch are mainly caves, pores and fractures resulted from dissolution and/or karstification. The Ordovician carbonate reservoirs are affected and modified by the diagenetie process in penecontemporaneous, epigenetic and burial periods and the multi-stage karstification related with deep hydrothermal activities, among which the most significant effect is from the meteoric water karstification related to the tectonic uplift from the end of Middle Ordovician to the end of Late Ordovician （end of O2-end of 03） and at the end of Middle Devonian （end of D2）. Varied palacogeologic settings and tectonic features at different geologic periods lead to different fluid flowing patterns, karstification mechanisms and transformation features in different regions, which further influence the reservoir distribution. The paleo-uplifts at different periods, such as end of O2-end of 03 and end of D2, control the dominant development zones of karstification; the paleogeomorphology and faults resulted from tectonic uplift control the flowing depth of the karst fluid; and the lithology controls the position and extent of karst development.</description><subject>Arches</subject><subject>Basins</subject><subject>Biogeosciences</subject><subject>Carbonates</subject><subject>Caves</subject><subject>Devonian</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Fluid dynamics</subject><subject>Fluid flow</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydrocarbons</subject><subject>Karst</subject><subject>Lithology</subject><subject>Meteoric water</subject><subject>Oil and gas fields</subject><subject>Ordovician</subject><subject>Reservoirs</subject><subject>Rocks</subject><subject>Tectonics</subject><subject>地质构造特征</subject><subject>塔里木盆地</subject><subject>奥陶系</subject><subject>岩溶作用</subject><subject>控制因素</subject><subject>流体流动模式</subject><subject>碳酸盐岩储层</subject><subject>阿克库勒凸起</subject><issn>1674-487X</issn><issn>1867-111X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kUFLAzEQhRdRUNQf4C3ixYOrmSRtssdarIqCFwVvyzTJttE1qUlW8N-bUhERzGUC8703M7yqOgJ6DpTKiwRspHhNgdWUSajFVrUHaixrAHjeLv-xFLVQ8nm3OkzphZbHmVQg96phZjEP0SaC3pBp8DmGvnd-QWaoc4iJhI5crdzCeqfJHcaUXec0Zhf8upWXljxEEz6cdujJFOM8eMzFz3kyebWvQ2_JJOrlGXnE6N7IJSbnD6qdDvtkD7_rfvU0u3qc3tT3D9e308l9jbxRuWbUmBGgsFYYVLxpFGAHUrDOSq6BMzPWkstOG146Zt6gAalQIm2MkmrO96vTje8qhvfBpty-uaRt36O3YUgtUMUYAOVQ0JM_6EsYoi_bFYpToTijo0LBhtIxpBRt167KURg_C9Sus2g3WbQli3adRSuKhm00qbB-YeNv5_9Fx9-DlsEv3ovuZ5JgDZd8LPkXcXmXJw</recordid><startdate>20120801</startdate><enddate>20120801</enddate><creator>陈强路 赵永强 李国蓉 储呈林 王斌</creator><general>China University of Geosciences</general><general>Springer Nature 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and Controlling Factors of Epigenic Karstification of the Ordovician Carbonates in Akekule Arch, Tarim Basin</title><author>陈强路 赵永强 李国蓉 储呈林 王斌</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a398t-20dd51a4ee4da839981af1742fe73c132d6c737fcd381adb9ad178a7a09d878b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Arches</topic><topic>Basins</topic><topic>Biogeosciences</topic><topic>Carbonates</topic><topic>Caves</topic><topic>Devonian</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Fluid dynamics</topic><topic>Fluid flow</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hydrocarbons</topic><topic>Karst</topic><topic>Lithology</topic><topic>Meteoric water</topic><topic>Oil and gas 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Earth Sci</stitle><addtitle>JOURNAL OF EARTH SCIENCE</addtitle><date>2012-08-01</date><risdate>2012</risdate><volume>23</volume><issue>4</issue><spage>506</spage><epage>515</epage><pages>506-515</pages><issn>1674-487X</issn><eissn>1867-111X</eissn><abstract>ABSTRACT： Tabei （塔北） uplift is an area with the highest hydrocarbon enrichment in Tarim basin, and large oilfields have been found on Akekule （阿克库勒） arch at the middle section of Tabei uplift, with Ordovician carbonate reservoirs. Storage space of the Ordovician carbonate reservoirs in the Akekule arch are mainly caves, pores and fractures resulted from dissolution and/or karstification. The Ordovician carbonate reservoirs are affected and modified by the diagenetie process in penecontemporaneous, epigenetic and burial periods and the multi-stage karstification related with deep hydrothermal activities, among which the most significant effect is from the meteoric water karstification related to the tectonic uplift from the end of Middle Ordovician to the end of Late Ordovician （end of O2-end of 03） and at the end of Middle Devonian （end of D2）. Varied palacogeologic settings and tectonic features at different geologic periods lead to different fluid flowing patterns, karstification mechanisms and transformation features in different regions, which further influence the reservoir distribution. The paleo-uplifts at different periods, such as end of O2-end of 03 and end of D2, control the dominant development zones of karstification; the paleogeomorphology and faults resulted from tectonic uplift control the flowing depth of the karst fluid; and the lithology controls the position and extent of karst development.</abstract><cop>China University of Geosciences</cop><pub>China University of Geosciences</pub><doi>10.1007/s12583-012-0271-4</doi><tpages>10</tpages></addata></record> |
| fulltext | fulltext |
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| ispartof | Journal of earth science (Wuhan, China), 2012-08, Vol.23 (4), p.506-515 |
| issn | 1674-487X 1867-111X |
| language | eng |
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| source | Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings |
| subjects | Arches Basins Biogeosciences Carbonates Caves Devonian Earth and Environmental Science Earth science Earth Sciences Fluid dynamics Fluid flow Geochemistry Geology Geotechnical Engineering & Applied Earth Sciences Hydrocarbons Karst Lithology Meteoric water Oil and gas fields Ordovician Reservoirs Rocks Tectonics 地质构造特征 塔里木盆地 奥陶系 岩溶作用 控制因素 流体流动模式 碳酸盐岩储层 阿克库勒凸起 |
| title | Features and Controlling Factors of Epigenic Karstification of the Ordovician Carbonates in Akekule Arch, Tarim Basin |
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