Initial analysis of the Jurassic “Nordegg Member”, Fernie Formation: using paleomagnetism to date source rock thermal maturation
Paleomagnetic analysis demonstrates that the mean inclination, and therefore the age of the magnetization, in the organic-rich shales of the “Nordegg Member” of the Jurassic Fernie Formation correlates with thermal maturity indices. In the immature wells, the magnetization is probably Early to Middl...
Gespeichert in:
| Veröffentlicht in: | Physics and chemistry of the earth. Parts A/B/C 2002-01, Vol.27 (25), p.1161-1168 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1168 |
|---|---|
| container_issue | 25 |
| container_start_page | 1161 |
| container_title | Physics and chemistry of the earth. Parts A/B/C |
| container_volume | 27 |
| creator | Cioppa, M.T Symons, D.T.A Flore, M |
| description | Paleomagnetic analysis demonstrates that the mean inclination, and therefore the age of the magnetization, in the organic-rich shales of the “Nordegg Member” of the Jurassic Fernie Formation correlates with thermal maturity indices. In the immature wells, the magnetization is probably Early to Middle Jurassic (
I=60°±5°), in the mature wells, Late Jurassic (
I=70°±3°) and in the overmature wells, Late Cretaceous (
I=77°+7/−5°). The change in inclination with time, which reflects varying ages of magnetization, also allows the possibility that the inclination can be used as a proxy for the maturity level in the “Nordegg Member” and thereby aid in petroleum exploration. |
| doi_str_mv | 10.1016/S1474-7065(02)00105-5 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_21870671</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S1474706502001055</els_id><sourcerecordid>18928292</sourcerecordid><originalsourceid>FETCH-LOGICAL-a392t-b8aeefd6ccd59699511ed94537c5faff7ce35c17cdec3256271d0cb2f7538fd3</originalsourceid><addsrcrecordid>eNqFkctOxCAUhhujiddHMGFlNLEKtJTWjTETx0u8LHRPGDiMaFtGoCbuXPgY-nI-iYyja1ecxff9J5w_y7YJPiCYVId3pORlznHFdjHdw5hglrOlbI3UvMgZaYrlNP8hq9l6CI8J4qQs17L3i95GK1ske9m-BhuQMyg-ALocvAzBKvT19nHjvIbpFF1DNwH_9fa5j8bgewto7Hwno3X9ERqC7adoJltwnZz2EG3oUHRIywgouMErQN6pp3l6klqUxLRjLm9mK0a2AbZ-343sfnx6PzrPr27PLkYnV7ksGhrzSS0BjK6U0qypmoYRAropWcEVM9IYrqBginClQRWUVZQTjdWEGs6K2uhiI9tZxM68ex4gRNHZoKBtZQ9uCIKmg-GKk39BUje0pg1NIFuAyrsQPBgx87aT_lUQLObdiJ9uxPzwAlPx041gyTteeJB--2LBi6As9Aq09aCi0M7-k_ANdX-bIw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>18928292</pqid></control><display><type>article</type><title>Initial analysis of the Jurassic “Nordegg Member”, Fernie Formation: using paleomagnetism to date source rock thermal maturation</title><source>Elsevier ScienceDirect Journals</source><creator>Cioppa, M.T ; Symons, D.T.A ; Flore, M</creator><creatorcontrib>Cioppa, M.T ; Symons, D.T.A ; Flore, M</creatorcontrib><description>Paleomagnetic analysis demonstrates that the mean inclination, and therefore the age of the magnetization, in the organic-rich shales of the “Nordegg Member” of the Jurassic Fernie Formation correlates with thermal maturity indices. In the immature wells, the magnetization is probably Early to Middle Jurassic (
I=60°±5°), in the mature wells, Late Jurassic (
I=70°±3°) and in the overmature wells, Late Cretaceous (
I=77°+7/−5°). The change in inclination with time, which reflects varying ages of magnetization, also allows the possibility that the inclination can be used as a proxy for the maturity level in the “Nordegg Member” and thereby aid in petroleum exploration.</description><identifier>ISSN: 1474-7065</identifier><identifier>EISSN: 1873-5193</identifier><identifier>DOI: 10.1016/S1474-7065(02)00105-5</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Marine ; Organic maturation ; Paleomagnetism ; Remagnetization ; Thermal maturation indices</subject><ispartof>Physics and chemistry of the earth. Parts A/B/C, 2002-01, Vol.27 (25), p.1161-1168</ispartof><rights>2002 Elsevier Science Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a392t-b8aeefd6ccd59699511ed94537c5faff7ce35c17cdec3256271d0cb2f7538fd3</citedby><cites>FETCH-LOGICAL-a392t-b8aeefd6ccd59699511ed94537c5faff7ce35c17cdec3256271d0cb2f7538fd3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S1474706502001055$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65534</link.rule.ids></links><search><creatorcontrib>Cioppa, M.T</creatorcontrib><creatorcontrib>Symons, D.T.A</creatorcontrib><creatorcontrib>Flore, M</creatorcontrib><title>Initial analysis of the Jurassic “Nordegg Member”, Fernie Formation: using paleomagnetism to date source rock thermal maturation</title><title>Physics and chemistry of the earth. Parts A/B/C</title><description>Paleomagnetic analysis demonstrates that the mean inclination, and therefore the age of the magnetization, in the organic-rich shales of the “Nordegg Member” of the Jurassic Fernie Formation correlates with thermal maturity indices. In the immature wells, the magnetization is probably Early to Middle Jurassic (
I=60°±5°), in the mature wells, Late Jurassic (
I=70°±3°) and in the overmature wells, Late Cretaceous (
I=77°+7/−5°). The change in inclination with time, which reflects varying ages of magnetization, also allows the possibility that the inclination can be used as a proxy for the maturity level in the “Nordegg Member” and thereby aid in petroleum exploration.</description><subject>Marine</subject><subject>Organic maturation</subject><subject>Paleomagnetism</subject><subject>Remagnetization</subject><subject>Thermal maturation indices</subject><issn>1474-7065</issn><issn>1873-5193</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNqFkctOxCAUhhujiddHMGFlNLEKtJTWjTETx0u8LHRPGDiMaFtGoCbuXPgY-nI-iYyja1ecxff9J5w_y7YJPiCYVId3pORlznHFdjHdw5hglrOlbI3UvMgZaYrlNP8hq9l6CI8J4qQs17L3i95GK1ske9m-BhuQMyg-ALocvAzBKvT19nHjvIbpFF1DNwH_9fa5j8bgewto7Hwno3X9ERqC7adoJltwnZz2EG3oUHRIywgouMErQN6pp3l6klqUxLRjLm9mK0a2AbZ-343sfnx6PzrPr27PLkYnV7ksGhrzSS0BjK6U0qypmoYRAropWcEVM9IYrqBginClQRWUVZQTjdWEGs6K2uhiI9tZxM68ex4gRNHZoKBtZQ9uCIKmg-GKk39BUje0pg1NIFuAyrsQPBgx87aT_lUQLObdiJ9uxPzwAlPx041gyTteeJB--2LBi6As9Aq09aCi0M7-k_ANdX-bIw</recordid><startdate>20020101</startdate><enddate>20020101</enddate><creator>Cioppa, M.T</creator><creator>Symons, D.T.A</creator><creator>Flore, M</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20020101</creationdate><title>Initial analysis of the Jurassic “Nordegg Member”, Fernie Formation: using paleomagnetism to date source rock thermal maturation</title><author>Cioppa, M.T ; Symons, D.T.A ; Flore, M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a392t-b8aeefd6ccd59699511ed94537c5faff7ce35c17cdec3256271d0cb2f7538fd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Marine</topic><topic>Organic maturation</topic><topic>Paleomagnetism</topic><topic>Remagnetization</topic><topic>Thermal maturation indices</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cioppa, M.T</creatorcontrib><creatorcontrib>Symons, D.T.A</creatorcontrib><creatorcontrib>Flore, M</creatorcontrib><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Physics and chemistry of the earth. Parts A/B/C</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cioppa, M.T</au><au>Symons, D.T.A</au><au>Flore, M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Initial analysis of the Jurassic “Nordegg Member”, Fernie Formation: using paleomagnetism to date source rock thermal maturation</atitle><jtitle>Physics and chemistry of the earth. Parts A/B/C</jtitle><date>2002-01-01</date><risdate>2002</risdate><volume>27</volume><issue>25</issue><spage>1161</spage><epage>1168</epage><pages>1161-1168</pages><issn>1474-7065</issn><eissn>1873-5193</eissn><abstract>Paleomagnetic analysis demonstrates that the mean inclination, and therefore the age of the magnetization, in the organic-rich shales of the “Nordegg Member” of the Jurassic Fernie Formation correlates with thermal maturity indices. In the immature wells, the magnetization is probably Early to Middle Jurassic (
I=60°±5°), in the mature wells, Late Jurassic (
I=70°±3°) and in the overmature wells, Late Cretaceous (
I=77°+7/−5°). The change in inclination with time, which reflects varying ages of magnetization, also allows the possibility that the inclination can be used as a proxy for the maturity level in the “Nordegg Member” and thereby aid in petroleum exploration.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/S1474-7065(02)00105-5</doi><tpages>8</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1474-7065 |
| ispartof | Physics and chemistry of the earth. Parts A/B/C, 2002-01, Vol.27 (25), p.1161-1168 |
| issn | 1474-7065 1873-5193 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_21870671 |
| source | Elsevier ScienceDirect Journals |
| subjects | Marine Organic maturation Paleomagnetism Remagnetization Thermal maturation indices |
| title | Initial analysis of the Jurassic “Nordegg Member”, Fernie Formation: using paleomagnetism to date source rock thermal maturation |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-21T19%3A25%3A56IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Initial%20analysis%20of%20the%20Jurassic%20%E2%80%9CNordegg%20Member%E2%80%9D,%20Fernie%20Formation:%20using%20paleomagnetism%20to%20date%20source%20rock%20thermal%20maturation&rft.jtitle=Physics%20and%20chemistry%20of%20the%20earth.%20Parts%20A/B/C&rft.au=Cioppa,%20M.T&rft.date=2002-01-01&rft.volume=27&rft.issue=25&rft.spage=1161&rft.epage=1168&rft.pages=1161-1168&rft.issn=1474-7065&rft.eissn=1873-5193&rft_id=info:doi/10.1016/S1474-7065(02)00105-5&rft_dat=%3Cproquest_cross%3E18928292%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=18928292&rft_id=info:pmid/&rft_els_id=S1474706502001055&rfr_iscdi=true |