Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/8127| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Lucifora, S.; Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.authorall | Cifelli, F.; Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.authorall | Mattei, M.; Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.authorall | Sagnotti, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
| dc.contributor.authorall | Cosentino, D.; Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.authorall | Roberts, A. P.; Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia | en |
| dc.date.accessioned | 2012-10-10T12:21:50Z | en |
| dc.date.available | 2012-10-10T12:21:50Z | en |
| dc.date.issued | 2012-10-05 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/8127 | en |
| dc.description.abstract | We present paleomagnetic, rock magnetic and scanning electron microscope data from three upper Messinian stratigraphic sections from the Adana Basin (southern Turkey). The collected samples are from fine-grained units, which were deposited during the Messinian Salinity Crisis (within subchron C3r). Paleomagnetic results reveal an inconsistent polarity record, related to a mixture of magnetite and greigite that hinders determination of a reliable magnetostratigraphy. Three classes of samples are recognized on the basis of paleomagnetic results. The first is characterized by a single magnetization component, with normal polarity, that is stable up to 530–580 C and is carried by magnetite. The second is characterized by a single magnetization component, with reversed polarity, that is stable up to 330–420 C. This magnetization is due to greigite, which developed after formation of slumps and before tectonic tilting of the studied successions. The third is characterized by reversed polarity, which is stable up to 530–580 C. We interpret this component as a primary magnetization carried by fine-grained and magnetically stable detrital magnetite. Results indicate that in the Adana Basin the assumption that a primary magnetization is carried by magnetite, and a magnetic overprint carried by greigite, does not hold because a late magnetic overprint has also been found for magnetite-bearing samples. Our data illustrate the complexity of magnetostratigraphic reconstructions in successions characterized by variable mixtures of magnetic minerals with different magnetic stability that formed at different stages. We demonstrate the need to perform detailed magnetic mineralogy analyses when conducting magnetostratigraphic studies of clay-rich sediments from marine or lacustrine environments. | en |
| dc.language.iso | English | en |
| dc.publisher.name | American Geophysical Union | en |
| dc.relation.ispartof | Geochemistry, Geophysics, Geosystems | en |
| dc.relation.ispartofseries | 10 / 13 (2012) | en |
| dc.subject | Messinian | en |
| dc.subject | remagnetization | en |
| dc.subject | reversals | en |
| dc.subject | rock and mineral magnetism | en |
| dc.subject | southern Turkey | en |
| dc.title | Inconsistent magnetic polarities in magnetite-and greigite-bearing sediments: Understanding complex magnetizations in the late Messinian in the Adana Basin (southern Turkey) | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | Q10002 | en |
| dc.subject.INGV | 04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetism | en |
| dc.subject.INGV | 04. Solid Earth::04.05. Geomagnetism::04.05.07. Rock magnetism | en |
| dc.identifier.doi | 10.1029/2012GC004248 | en |
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Liu (2008), Identifying reversible and irreversible magnetization changes in prototype patterned media using first- and second-order reversal curves, J. Appl. Phys., 103, 07C518, doi:10.1063/1.2837888. | en |
| dc.description.obiettivoSpecifico | 2.2. Laboratorio di paleomagnetismo | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | restricted | en |
| dc.relation.issn | ISSN: 1525-2027 | en |
| dc.relation.eissn | 1525-2027 | en |
| dc.contributor.author | Lucifora, S. | en |
| dc.contributor.author | Cifelli, F. | en |
| dc.contributor.author | Mattei, M. | en |
| dc.contributor.author | Sagnotti, L. | en |
| dc.contributor.author | Cosentino, D. | en |
| dc.contributor.author | Roberts, A. P. | en |
| dc.contributor.department | Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.department | Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.department | Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
| dc.contributor.department | Dipartimento di Scienze Geologiche, Università Roma Tre, Largo San Leonardo Murialdo 1, IT-00146 Rome, Italy | en |
| dc.contributor.department | Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Roma Tre University | - |
| crisitem.author.dept | Università degli studi di Roma TRE | - |
| crisitem.author.dept | Università degli studi di Roma TRE | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
| crisitem.author.dept | Dipartimento di Scienze Geologiche, Universita` 'Roma Tre', Rome, Italy | - |
| crisitem.author.dept | National Oceanography Centre, University of Southampton, European Way, Southampton SO14 3ZH, UK | - |
| crisitem.author.orcid | 0000-0003-3944-201X | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
Files in This Item:
| File | Description | Size | Format | Existing users please Login |
|---|---|---|---|---|
| Lucifora et al 2012 G3 Vol 13 No 10.pdf | 2.4 MB | Adobe PDF |
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