气候变化领域集成服务门户(CCPortal): Corrected late triassic latitudes for continents adjacent to the North Atlantic

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DOI	10.1126/science.1105826
	Corrected late triassic latitudes for continents adjacent to the North Atlantic
	Kent D.V.; Tauxe L.
发表日期	2005
ISSN	0036-8075
起始页码	240
结束页码	244
卷号	307 期号:5707
英文摘要	We use a method based on a statistical geomagnetic field model to recognize and correct for inclination error in sedimentary rocks from early Mesozoic rift basins in North America, Greenland, and Europe. The congruence of the corrected sedimentary results and independent data from igneous rocks on a regional scale indicates that a geocentric axial dipole field operated in the Late Triassic. The corrected paleolatitudes indicate a faster poleward drift of ∼0.6 degrees per million years for this part of Pangea and suggest that the equatorial humid belt in the Late Triassic was about as wide as it is today.
英文关键词	Igneous rocks; Sedimentary rocks; Statistical methods; Geomagnetic fields; Latitudes; North Atlantic; Regional scale; Geomagnetism; geomagnetic field; sedimentary rock; Triassic; article; Europe; geography; Greenland; latitude; magnetic field; North America; paleontology; priority journal; rock; Triassic
语种	英语
来源期刊	Science
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/244259
作者单位	Department of Geological Sciences, Rutgers University, Piscataway, NJ 08854, United States; Lamont-Doherty Earth Observ. C., Palisades, NY 10964, United States; Scripps Institution of Oceanography, San Diego, CA 92093, United States
推荐引用方式 GB/T 7714	Kent D.V.,Tauxe L.. Corrected late triassic latitudes for continents adjacent to the North Atlantic[J],2005,307(5707).
APA	Kent D.V.,&Tauxe L..(2005).Corrected late triassic latitudes for continents adjacent to the North Atlantic.Science,307(5707).
MLA	Kent D.V.,et al."Corrected late triassic latitudes for continents adjacent to the North Atlantic".Science 307.5707(2005).