Magnetostratigraphy of the lower Cretaceous strata in Tlayúa Quarry, Tepexi de Rodriguez, State of Puebla, Mexico
A stratigraphic sequence of magnetic polarity reversals consisting of nine magnetozones is recognized in Early Cretaceous sedimentary strata in the Tlayúa Quarry of Tepexi de Rodriguez, state of Puebla. Combined with biostratigraphic age assignments using ammonites that apparently belonging to the A...
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| Veröffentlicht in: | Earth, planets, and space planets, and space, 2006-01, Vol.58 (10), p.1295-1302 |
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| creator | Benammi, Mouloud Alvarado-Ortega, Jesus Urrutia-Fucugauchi, Jaime |
| description | A stratigraphic sequence of magnetic polarity reversals consisting of nine magnetozones is recognized in Early Cretaceous sedimentary strata in the Tlayúa Quarry of Tepexi de Rodriguez, state of Puebla. Combined with biostratigraphic age assignments using ammonites that apparently belonging to the Albian, the geomagnetic polarity sequence can be correlated with the middle part of chron C34n (C34n.1n-C34n.2n chrons, with an age of 100–105 Myr), the Cretaceous long normal interval. The magnetic properties and characteristic remanence of magnetization are dominated by soft and hard coercivity magnetic minerals. Rock-magnetic properties and a positive reversal test suggest that remanence is primary. The section displays both reverse and normal polarities with mean directions:
D
=344.9°,
I
=32.4°,
k
=21, a95=4.2° and
D
=149.4°,
I
=−36.6°,
k
=17, a95=8.7°, respectively. Comparison with the North American apparent polar wander path indicates tectonic stability of the region since the Cretaceous. |
| doi_str_mv | 10.1186/BF03352624 |
| format | Article |
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D
=344.9°,
I
=32.4°,
k
=21, a95=4.2° and
D
=149.4°,
I
=−36.6°,
k
=17, a95=8.7°, respectively. Comparison with the North American apparent polar wander path indicates tectonic stability of the region since the Cretaceous.</description><identifier>ISSN: 1880-5981</identifier><identifier>ISSN: 1343-8832</identifier><identifier>EISSN: 1880-5981</identifier><identifier>DOI: 10.1186/BF03352624</identifier><language>eng</language><publisher>Springer / Terra Scientific Publishing Company</publisher><subject>Earth Sciences ; Paleontology ; Sciences of the Universe</subject><ispartof>Earth, planets, and space, 2006-01, Vol.58 (10), p.1295-1302</ispartof><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a477t-963a3c876deac22f828501400ab27a67b3af61d532a6fd75efd74b6ed4b56a323</citedby><cites>FETCH-LOGICAL-a477t-963a3c876deac22f828501400ab27a67b3af61d532a6fd75efd74b6ed4b56a323</cites><orcidid>0000-0003-4707-7518</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,777,781,882,27905,27906</link.rule.ids><backlink>$$Uhttps://hal.science/hal-00436247$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Benammi, Mouloud</creatorcontrib><creatorcontrib>Alvarado-Ortega, Jesus</creatorcontrib><creatorcontrib>Urrutia-Fucugauchi, Jaime</creatorcontrib><title>Magnetostratigraphy of the lower Cretaceous strata in Tlayúa Quarry, Tepexi de Rodriguez, State of Puebla, Mexico</title><title>Earth, planets, and space</title><description>A stratigraphic sequence of magnetic polarity reversals consisting of nine magnetozones is recognized in Early Cretaceous sedimentary strata in the Tlayúa Quarry of Tepexi de Rodriguez, state of Puebla. Combined with biostratigraphic age assignments using ammonites that apparently belonging to the Albian, the geomagnetic polarity sequence can be correlated with the middle part of chron C34n (C34n.1n-C34n.2n chrons, with an age of 100–105 Myr), the Cretaceous long normal interval. The magnetic properties and characteristic remanence of magnetization are dominated by soft and hard coercivity magnetic minerals. Rock-magnetic properties and a positive reversal test suggest that remanence is primary. The section displays both reverse and normal polarities with mean directions:
D
=344.9°,
I
=32.4°,
k
=21, a95=4.2° and
D
=149.4°,
I
=−36.6°,
k
=17, a95=8.7°, respectively. Comparison with the North American apparent polar wander path indicates tectonic stability of the region since the Cretaceous.</description><subject>Earth Sciences</subject><subject>Paleontology</subject><subject>Sciences of the Universe</subject><issn>1880-5981</issn><issn>1343-8832</issn><issn>1880-5981</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNpNkc9OwzAMhyMEEmNw4QlyQgKtkDRt2h1hYgxpE__GOXJbdyvqlpKkQHk0rrwYLUPAxbasT59k_wg55OyU81ieXYyZEKEv_WCL9HgcMy8cxnz737xL9qx9YkywQIoeMTNYrNFp6wy4YmGgWjZU59QtkZb6FQ0dGXSQoq4t_YaAFms6L6H5_AB6V4MxzYDOscK3gmZI73VmikWN7wP64MBhJ7utMSlhQGctk-p9spNDafHgp_fJ4_hyPpp405ur69H51IMgipw3lAJEGkcyQ0h9P4_9OGQ8YAwSPwIZJQJyybNQ-CDzLAqxLUEiMQuSUILwRZ8cb7xLKFVlihWYRmko1OR8qrodY4FoPxW98JY92rCV0c81WqdWhU2xLGHdXa4EY4xzzlrwZAOmRltrMP81c6a6CNRfBOILodZ5Jg</recordid><startdate>20060101</startdate><enddate>20060101</enddate><creator>Benammi, Mouloud</creator><creator>Alvarado-Ortega, Jesus</creator><creator>Urrutia-Fucugauchi, Jaime</creator><general>Springer / Terra Scientific Publishing Company</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SM</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0003-4707-7518</orcidid></search><sort><creationdate>20060101</creationdate><title>Magnetostratigraphy of the lower Cretaceous strata in Tlayúa Quarry, Tepexi de Rodriguez, State of Puebla, Mexico</title><author>Benammi, Mouloud ; Alvarado-Ortega, Jesus ; Urrutia-Fucugauchi, Jaime</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a477t-963a3c876deac22f828501400ab27a67b3af61d532a6fd75efd74b6ed4b56a323</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Earth Sciences</topic><topic>Paleontology</topic><topic>Sciences of the Universe</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Benammi, Mouloud</creatorcontrib><creatorcontrib>Alvarado-Ortega, Jesus</creatorcontrib><creatorcontrib>Urrutia-Fucugauchi, Jaime</creatorcontrib><collection>CrossRef</collection><collection>Earthquake Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Earth, planets, and space</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Benammi, Mouloud</au><au>Alvarado-Ortega, Jesus</au><au>Urrutia-Fucugauchi, Jaime</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Magnetostratigraphy of the lower Cretaceous strata in Tlayúa Quarry, Tepexi de Rodriguez, State of Puebla, Mexico</atitle><jtitle>Earth, planets, and space</jtitle><date>2006-01-01</date><risdate>2006</risdate><volume>58</volume><issue>10</issue><spage>1295</spage><epage>1302</epage><pages>1295-1302</pages><issn>1880-5981</issn><issn>1343-8832</issn><eissn>1880-5981</eissn><abstract>A stratigraphic sequence of magnetic polarity reversals consisting of nine magnetozones is recognized in Early Cretaceous sedimentary strata in the Tlayúa Quarry of Tepexi de Rodriguez, state of Puebla. Combined with biostratigraphic age assignments using ammonites that apparently belonging to the Albian, the geomagnetic polarity sequence can be correlated with the middle part of chron C34n (C34n.1n-C34n.2n chrons, with an age of 100–105 Myr), the Cretaceous long normal interval. The magnetic properties and characteristic remanence of magnetization are dominated by soft and hard coercivity magnetic minerals. Rock-magnetic properties and a positive reversal test suggest that remanence is primary. The section displays both reverse and normal polarities with mean directions:
D
=344.9°,
I
=32.4°,
k
=21, a95=4.2° and
D
=149.4°,
I
=−36.6°,
k
=17, a95=8.7°, respectively. Comparison with the North American apparent polar wander path indicates tectonic stability of the region since the Cretaceous.</abstract><pub>Springer / Terra Scientific Publishing Company</pub><doi>10.1186/BF03352624</doi><tpages>8</tpages><orcidid>https://orcid.org/0000-0003-4707-7518</orcidid><oa>free_for_read</oa></addata></record> |
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| source | J-STAGE Free; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Springer Nature OA Free Journals; Springer Nature - Complete Springer Journals; Alma/SFX Local Collection |
| subjects | Earth Sciences Paleontology Sciences of the Universe |
| title | Magnetostratigraphy of the lower Cretaceous strata in Tlayúa Quarry, Tepexi de Rodriguez, State of Puebla, Mexico |
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