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Terrestrial Heat Flow in the Qagan Sag, Inner Mongolia
The Qagan sag has the largest oil and gas exploration potential in the Inggen‐Ejin Qi basin, Inner Mongolia. The terrestrial heat flow research is still blank in the Qagan sag and rest of the Inggen‐Ejin Qi basin, which seriously restricts the oil and gas resource assessment in the basin. In this wo...
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Published in: | Chinese journal of geophysics 2013-09, Vol.56 (5), p.559-571 |
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container_title | Chinese journal of geophysics |
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creator | Yin-Hui, ZUO Nan-Sheng, QIU Yi-Xun, DENG Song, RAO Shen-Mou, XU Jian-Guo, LI |
description | The Qagan sag has the largest oil and gas exploration potential in the Inggen‐Ejin Qi basin, Inner Mongolia. The terrestrial heat flow research is still blank in the Qagan sag and rest of the Inggen‐Ejin Qi basin, which seriously restricts the oil and gas resource assessment in the basin. In this work, 107 rock thermal conductivity data of 19 wells were measured and in‐situ corrected, and the rock thermal conductivities of each stratum were obtained by the union average formula. Based on the 9 wells' temperatures, combined with the above rock thermal conductivity data, the geothermal gradients and terrestrial heat flow were calculated. The results show the Qagan sag has the characteristics of the medium temperature field between tectonically stable and active regions, with an average thermal gradient of 33.6 °C/km and an average terrestrial heat flow value of 74.5 mW/m2. This work provides the geothermal data for oil and gas resource assessment of the Qagan sag and other sags of the Inggen‐Ejin Qi basin. |
doi_str_mv | 10.1002/cjg2.20053 |
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The terrestrial heat flow research is still blank in the Qagan sag and rest of the Inggen‐Ejin Qi basin, which seriously restricts the oil and gas resource assessment in the basin. In this work, 107 rock thermal conductivity data of 19 wells were measured and in‐situ corrected, and the rock thermal conductivities of each stratum were obtained by the union average formula. Based on the 9 wells' temperatures, combined with the above rock thermal conductivity data, the geothermal gradients and terrestrial heat flow were calculated. The results show the Qagan sag has the characteristics of the medium temperature field between tectonically stable and active regions, with an average thermal gradient of 33.6 °C/km and an average terrestrial heat flow value of 74.5 mW/m2. 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The terrestrial heat flow research is still blank in the Qagan sag and rest of the Inggen‐Ejin Qi basin, which seriously restricts the oil and gas resource assessment in the basin. In this work, 107 rock thermal conductivity data of 19 wells were measured and in‐situ corrected, and the rock thermal conductivities of each stratum were obtained by the union average formula. Based on the 9 wells' temperatures, combined with the above rock thermal conductivity data, the geothermal gradients and terrestrial heat flow were calculated. The results show the Qagan sag has the characteristics of the medium temperature field between tectonically stable and active regions, with an average thermal gradient of 33.6 °C/km and an average terrestrial heat flow value of 74.5 mW/m2. This work provides the geothermal data for oil and gas resource assessment of the Qagan sag and other sags of the Inggen‐Ejin Qi basin.</description><subject>Assessments</subject><subject>Basins</subject><subject>Heat transfer</subject><subject>Heat transmission</subject><subject>Inggen-Ejin Qi basin</subject><subject>Natural gas</subject><subject>Qagan sag</subject><subject>Rock</subject><subject>Rock thermal conductivity</subject><subject>Sag</subject><subject>Terrestrial heat flow</subject><subject>Thermal conductivity</subject><subject>Thermal gradient</subject><issn>0898-9591</issn><issn>2326-0440</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqN0MtKAzEUBuAgCtbLxicYcCPi6Mk9WUqxF6l3RXchM6Z16nRGkynVtzd11IULcREC4fvDOT9COxgOMQA5yqcTckgAOF1BHUKJSIExWEUdUFqlmmu8jjZCmEarAVgHiVvnvQuNL2yZDJxtkl5ZL5KiSponl1zZia2SGzs5SIZV5XxyVleTuizsFlob2zK47a97E931Tm67g3R00R92j0dpTjjQlAlK9KPOaZ4rKbUimGKQEhOW6Sw-xWMVcfljpqnEGVXYxXmV40oxmXFHN9Fe---Lr1_ncU4zK0LuytJWrp4HgyVjEqgS4h8UEy5BCh7p7i86ree-iotEBYJIqoFFtd-q3NcheDc2L76YWf9uMJhl22bZtvlsO2Lc4kVRuvc_pOme9sl3Jm0zRWjc20_G-mcjJJXc3J_3zfVD74zfjIS5pB8QiIuy</recordid><startdate>201309</startdate><enddate>201309</enddate><creator>Yin-Hui, ZUO</creator><creator>Nan-Sheng, QIU</creator><creator>Yi-Xun, DENG</creator><creator>Song, RAO</creator><creator>Shen-Mou, XU</creator><creator>Jian-Guo, LI</creator><general>Blackwell Publishing Ltd</general><general>Wiley Subscription Services, Inc</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>7TB</scope><scope>FR3</scope></search><sort><creationdate>201309</creationdate><title>Terrestrial Heat Flow in the Qagan Sag, Inner Mongolia</title><author>Yin-Hui, ZUO ; Nan-Sheng, QIU ; Yi-Xun, DENG ; Song, RAO ; Shen-Mou, XU ; Jian-Guo, LI</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2503-46329d9c3cc877982131077124b9bc87bc8a82ecdb9371b381e0448e58847b5e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Assessments</topic><topic>Basins</topic><topic>Heat transfer</topic><topic>Heat transmission</topic><topic>Inggen-Ejin Qi basin</topic><topic>Natural gas</topic><topic>Qagan sag</topic><topic>Rock</topic><topic>Rock thermal conductivity</topic><topic>Sag</topic><topic>Terrestrial heat flow</topic><topic>Thermal conductivity</topic><topic>Thermal gradient</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yin-Hui, ZUO</creatorcontrib><creatorcontrib>Nan-Sheng, QIU</creatorcontrib><creatorcontrib>Yi-Xun, DENG</creatorcontrib><creatorcontrib>Song, RAO</creatorcontrib><creatorcontrib>Shen-Mou, XU</creatorcontrib><creatorcontrib>Jian-Guo, LI</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Engineering Research Database</collection><jtitle>Chinese journal of geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yin-Hui, ZUO</au><au>Nan-Sheng, QIU</au><au>Yi-Xun, DENG</au><au>Song, RAO</au><au>Shen-Mou, XU</au><au>Jian-Guo, LI</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Terrestrial Heat Flow in the Qagan Sag, Inner Mongolia</atitle><jtitle>Chinese journal of geophysics</jtitle><addtitle>Chinese Journal of Geophysics</addtitle><date>2013-09</date><risdate>2013</risdate><volume>56</volume><issue>5</issue><spage>559</spage><epage>571</epage><pages>559-571</pages><issn>0898-9591</issn><eissn>2326-0440</eissn><abstract>The Qagan sag has the largest oil and gas exploration potential in the Inggen‐Ejin Qi basin, Inner Mongolia. The terrestrial heat flow research is still blank in the Qagan sag and rest of the Inggen‐Ejin Qi basin, which seriously restricts the oil and gas resource assessment in the basin. In this work, 107 rock thermal conductivity data of 19 wells were measured and in‐situ corrected, and the rock thermal conductivities of each stratum were obtained by the union average formula. Based on the 9 wells' temperatures, combined with the above rock thermal conductivity data, the geothermal gradients and terrestrial heat flow were calculated. The results show the Qagan sag has the characteristics of the medium temperature field between tectonically stable and active regions, with an average thermal gradient of 33.6 °C/km and an average terrestrial heat flow value of 74.5 mW/m2. 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subjects | Assessments Basins Heat transfer Heat transmission Inggen-Ejin Qi basin Natural gas Qagan sag Rock Rock thermal conductivity Sag Terrestrial heat flow Thermal conductivity Thermal gradient |
title | Terrestrial Heat Flow in the Qagan Sag, Inner Mongolia |
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