Research on Tectono-Thermal Evolution Modeling Method for Superimposed Basin with the Jianghan Basin as an Example
Tectono‐thermal evolution modeling based on geodynamic methods is an important method for studying sedimentary basin's thermal history. We restored superimposed basin's complex and long‐time evolution by using balanced cross‐section method, and inverted for its paleo‐heatflow by using mult...
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| Veröffentlicht in: | Chinese journal of geophysics 2010-01, Vol.53 (1), p.92-102 |
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| container_title | Chinese journal of geophysics |
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| creator | ZHAO, Chang‐Yu SONG, Hai‐Bin QIAN, Rong‐Yi SONG, Yang HUANG, Xing‐Hui CHEN, Lin TIAN, Li‐Hua |
| description | Tectono‐thermal evolution modeling based on geodynamic methods is an important method for studying sedimentary basin's thermal history. We restored superimposed basin's complex and long‐time evolution by using balanced cross‐section method, and inverted for its paleo‐heatflow by using multiple‐stage finite extensional and compressional strain rate method, with Yisui profile in the Jianghan Basin as an example. Finally, we calculated the paleo‐temperature of superimposed basin. Thus, we established a workflow of multiple‐stage extensional and compressional modeling, in which tectonic restoration, paleo‐heatflow inversion, lithosphere temperature reconstruction, and sedimentary basin temperature inversion are combined, and sedimentary basin's thermal evolution is coupled with that of the lithosphere. |
| doi_str_mv | 10.1002/cjg2.1476 |
| format | Article |
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We restored superimposed basin's complex and long‐time evolution by using balanced cross‐section method, and inverted for its paleo‐heatflow by using multiple‐stage finite extensional and compressional strain rate method, with Yisui profile in the Jianghan Basin as an example. Finally, we calculated the paleo‐temperature of superimposed basin. 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Geophys</addtitle><description>Tectono‐thermal evolution modeling based on geodynamic methods is an important method for studying sedimentary basin's thermal history. We restored superimposed basin's complex and long‐time evolution by using balanced cross‐section method, and inverted for its paleo‐heatflow by using multiple‐stage finite extensional and compressional strain rate method, with Yisui profile in the Jianghan Basin as an example. Finally, we calculated the paleo‐temperature of superimposed basin. Thus, we established a workflow of multiple‐stage extensional and compressional modeling, in which tectonic restoration, paleo‐heatflow inversion, lithosphere temperature reconstruction, and sedimentary basin temperature inversion are combined, and sedimentary basin's thermal evolution is coupled with that of the lithosphere.</description><subject>Paleo-heatflow</subject><subject>Paleo-temperature</subject><subject>Strain rate</subject><subject>Superimposed basin</subject><subject>Tectono-thermal evolution</subject><issn>0898-9591</issn><issn>2326-0440</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNp1kFFPwjAUhRujiYg--A_66sOg7bZue1SCKAE0ipj40ty1HRuOdWmHwL93BOKbT-fk3u_c3ByEbinpUUJYX66WrEeDiJ-hDvMZ90gQkHPUIXESe0mY0Et05dyqRRNCgg6yb9ppsDLHpsJzLRtTGW-ea7uGEg9_TLlpinYzNUqXRbXEU93kRuHMWPy-qbUt1rVxWuEHcEWFt0WT4ybXeFxAtcyhOs3B4dYPd7CuS32NLjIonb45aRd9PA7ngydv8jJ6HtxPPKBRyD2IwVeUpklMgUcxbTWUQapSriSklCnlS8LAZ1EgtVREZglnJJUygpjrLPW76O54V1rjnNWZqNt3we4FJeJQljiUJQ5ltWz_yG6LUu__B8VgPGKnhHdMFK7Ru78E2G_BIz8Kxeds1LrJV7xYvIqZ_wu4mXyf</recordid><startdate>201001</startdate><enddate>201001</enddate><creator>ZHAO, Chang‐Yu</creator><creator>SONG, Hai‐Bin</creator><creator>QIAN, Rong‐Yi</creator><creator>SONG, Yang</creator><creator>HUANG, Xing‐Hui</creator><creator>CHEN, Lin</creator><creator>TIAN, Li‐Hua</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>201001</creationdate><title>Research on Tectono-Thermal Evolution Modeling Method for Superimposed Basin with the Jianghan Basin as an Example</title><author>ZHAO, Chang‐Yu ; SONG, Hai‐Bin ; QIAN, Rong‐Yi ; SONG, Yang ; HUANG, Xing‐Hui ; CHEN, Lin ; TIAN, Li‐Hua</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a1756-a8a3d11b981a67819815c4bdb6dcab12dd3c02a3274cecd0cf9620bcc7a86efb3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Paleo-heatflow</topic><topic>Paleo-temperature</topic><topic>Strain rate</topic><topic>Superimposed basin</topic><topic>Tectono-thermal evolution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>ZHAO, Chang‐Yu</creatorcontrib><creatorcontrib>SONG, Hai‐Bin</creatorcontrib><creatorcontrib>QIAN, Rong‐Yi</creatorcontrib><creatorcontrib>SONG, Yang</creatorcontrib><creatorcontrib>HUANG, Xing‐Hui</creatorcontrib><creatorcontrib>CHEN, Lin</creatorcontrib><creatorcontrib>TIAN, Li‐Hua</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><jtitle>Chinese journal of geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>ZHAO, Chang‐Yu</au><au>SONG, Hai‐Bin</au><au>QIAN, Rong‐Yi</au><au>SONG, Yang</au><au>HUANG, Xing‐Hui</au><au>CHEN, Lin</au><au>TIAN, Li‐Hua</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Research on Tectono-Thermal Evolution Modeling Method for Superimposed Basin with the Jianghan Basin as an Example</atitle><jtitle>Chinese journal of geophysics</jtitle><addtitle>Chinese J. Geophys</addtitle><date>2010-01</date><risdate>2010</risdate><volume>53</volume><issue>1</issue><spage>92</spage><epage>102</epage><pages>92-102</pages><issn>0898-9591</issn><eissn>2326-0440</eissn><abstract>Tectono‐thermal evolution modeling based on geodynamic methods is an important method for studying sedimentary basin's thermal history. We restored superimposed basin's complex and long‐time evolution by using balanced cross‐section method, and inverted for its paleo‐heatflow by using multiple‐stage finite extensional and compressional strain rate method, with Yisui profile in the Jianghan Basin as an example. Finally, we calculated the paleo‐temperature of superimposed basin. Thus, we established a workflow of multiple‐stage extensional and compressional modeling, in which tectonic restoration, paleo‐heatflow inversion, lithosphere temperature reconstruction, and sedimentary basin temperature inversion are combined, and sedimentary basin's thermal evolution is coupled with that of the lithosphere.</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1002/cjg2.1476</doi><tpages>11</tpages></addata></record> |
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| ispartof | Chinese journal of geophysics, 2010-01, Vol.53 (1), p.92-102 |
| issn | 0898-9591 2326-0440 |
| language | eng |
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| source | Alma/SFX Local Collection |
| subjects | Paleo-heatflow Paleo-temperature Strain rate Superimposed basin Tectono-thermal evolution |
| title | Research on Tectono-Thermal Evolution Modeling Method for Superimposed Basin with the Jianghan Basin as an Example |
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