Late Cenozoic magnetostratigraphy (11 – 0 Ma) of the Dongshanding and Wangjiashan sections in the Longzhong Basin, western China
dc.contributor.author | Mac Niocaill, Conall | en_US |
dc.contributor.author | Wang, Jianli | en_US |
dc.contributor.author | Zhong, Wei | en_US |
dc.contributor.author | Li, Ji-Jun | en_US |
dc.contributor.author | Fang, Xiao-Min | en_US |
dc.contributor.author | Van der Voo, Rob | en_US |
dc.contributor.author | Zhu, Jun-Jie | en_US |
dc.contributor.author | Cao, Ji-Xiu | en_US |
dc.contributor.author | Chen, Huai-Lu | en_US |
dc.contributor.author | Wang, Jian-Ming | en_US |
dc.contributor.author | Zhang, Yie-Chun | en_US |
dc.date.accessioned | 2006-09-11T14:01:44Z | |
dc.date.available | 2006-09-11T14:01:44Z | |
dc.date.issued | 1997-03 | en_US |
dc.identifier.citation | Li, Ji-Jun; Fang, Xiao-Min; Van der Voo, Rob; Zhu, Jun-Jie; Mac Niocaill, Conall; Cao, Ji-Xiu; Zhong, Wei; Chen, Huai-Lu; Wang, Jianli; Wang, Jian-Ming; Zhang, Yie-Chun; (1997). "Late Cenozoic magnetostratigraphy (11 – 0 Ma) of the Dongshanding and Wangjiashan sections in the Longzhong Basin, western China." Geologie en Mijnbouw 76 (1-2): 121-134. <http://hdl.handle.net/2027.42/43922> | en_US |
dc.identifier.issn | 0016-7746 | en_US |
dc.identifier.issn | 1573-9708 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/43922 | |
dc.description.abstract | A paleomagnetic study of the 510-m-thick Wangjiashan section of Late Miocene and Pliocene terrestrial sediments reveals a fairly complete reversal record with ages from 11 to 1.8 Ma. The magnetostratigraphy of the Dongshanding section, located nearby, reveals a partially overlapping reversal record with ages from 2.2 to 0 Ma, and facilitates correlation of the Wangjiashan section with the global polarity time scale. A new stratigraphic division of the Wangjiashan section replaces the name Linxia formation by five new formation names, based on lithologic variation and mammalian fossil finds. The new formations and their magnetostratigraphically determined ages are: Dongshan Formation (c. 1.75–2.6 Ma), Jishi Fm. (c. 2.6–3.6 Ma), Hewangjia Fm. (4.5–6.0 Ma), Liushu Fm. (6.0–7.6 Ma), and Dongxiang Fm. (7.6–c. 12 Ma). The Neogene stratigraphy and fossil mammals suggest that the nearby part of the Tibetan Plateau experienced a persistent denudation during the Late Miocene and Early Pliocene, but that it was uplifted more rapidly at about 3.6 Ma. | en_US |
dc.format.extent | 387773 bytes | |
dc.format.extent | 3115 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Kluwer Academic Publishers; Springer Science+Business Media | en_US |
dc.subject.other | Geosciences | en_US |
dc.subject.other | Structural Geology | en_US |
dc.subject.other | Reversals | en_US |
dc.subject.other | Pliocene | en_US |
dc.subject.other | Miocene | en_US |
dc.title | Late Cenozoic magnetostratigraphy (11 – 0 Ma) of the Dongshanding and Wangjiashan sections in the Longzhong Basin, western China | en_US |
dc.type | Article | en_US |
dc.subject.hlbsecondlevel | Materials Science and Engineering | en_US |
dc.subject.hlbsecondlevel | Civil and Environmental Engineering | en_US |
dc.subject.hlbtoplevel | Engineering | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China; Department of Geological Sciences, the University of Michigan, Ann Arbor, MI, 48109-1063, U.S.A | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, the University of Michigan, Ann Arbor, MI, 48109-1063, U.S.A | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, the University of Michigan, Ann Arbor, MI, 48109-1063, U.S.A | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationother | Department of Geography, Lanzhou University, Lanzhou, Gansu, 730 000, China | en_US |
dc.contributor.affiliationumcampus | Ann Arbor | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/43922/1/11288_2004_Article_147540.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1023/A:1003153717799 | en_US |
dc.identifier.source | Geologie en Mijnbouw | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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