Inclination shallowing in Eocene Linzizong sedimentary rocks from   Southern Tibet: correction, possible causes and implications for   reconstructing the India-Asia collision

doi:10.1093/gji/ggt188

CORC > 北京大学 > 地球与空间科学学院

	Inclination shallowing in Eocene Linzizong sedimentary rocks from Southern Tibet: correction, possible causes and implications for reconstructing the India-Asia collision
	Huang, Wentao ; Dupont-Nivet, Guillaume ; Lippert, Peter C. ; van Hinsbergen, Douwe J. J. ; Hallot, Erwan
刊名	geophysical journal international
	2013
关键词	Magnetic fabrics and anisotropy Palaeomagnetism applied to tectonics Rock and mineral magnetism Continental tectonics: compressional Asia AXIAL DIPOLE HYPOTHESIS MAUCH CHUNK FORMATION CLAY-RICH SEDIMENT MAGNETIC-ANISOTROPY PALEOMAGNETIC INCLINATIONS RED BEDS VOLCANIC-ROCKS LHASA BLOCK TECTONIC EVOLUTION REMANENCE ANISOTROPY
DOI	10.1093/gji/ggt188
英文摘要	A systematic bias towards low palaeomagnetic inclination recorded in clastic sediments, that is, inclination shallowing, has been recognized and studied for decades. Identification, understanding and correction of this inclination shallowing are critical for palaeogeographic reconstructions, particularly those used in climate models and to date collisional events in convergent orogenic systems, such as those surrounding the Neotethys. Here we report palaeomagnetic inclinations from the sedimentary Eocene upper Linzizong Group of Southern Tibet that are similar to 20 degrees lower than conformable underlying volcanic units. At face value, the palaeomagnetic results from these sedimentary rocks suggest the southern margin of Asia was located similar to 10 degrees N, which is inconsistent with recent reviews of the palaeolatitude of Southern Tibet. We apply two different correction methods to estimate the magnitude of inclination shallowing independently from the volcanics. The mean inclination is corrected from 20.5 degrees to 40.0 degrees within 95 per cent confidence limits between 33.1 degrees and 49.5 degrees by the elongation/inclination (E/I) correction method; an anisotropy-based inclination correction method steepens the mean inclination to 41.3 +/- 3.3 degrees after a curve fitting- determined particle anisotropy of 1.39 is applied. These corrected inclinations are statistically indistinguishable from the well-determined 40.3 +/- 4.5 boolean OR mean inclination of the underlying volcanic rocks that provides an independent check on the validity of these correction methods. Our results show that inclination shallowing in sedimentary rocks can be corrected. Careful inspection of stratigraphic variations of rock magnetic properties and remanence anisotropy suggests shallowing was caused mainly by a combination of syn- and post-depositional processes such as particle imbrication and sedimentary compaction that vary in importance throughout the section. Palaeolatitudes calculated from palaeomagnetic directions from Eocene sedimentary rocks of the upper Linzizong Group that have corrected for inclination shallowing are consistent with palaeolatitude history of the Lhasa terrane, and suggest that the India-Asia collision began at similar to 20 degrees N by 45-55 Ma.; Geochemistry & Geophysics; SCI(E); EI; 10; ARTICLE; 3; 1390-1411; 194
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/311070]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	Huang, Wentao,Dupont-Nivet, Guillaume,Lippert, Peter C.,et al. Inclination shallowing in Eocene Linzizong sedimentary rocks from Southern Tibet: correction, possible causes and implications for reconstructing the India-Asia collision[J]. geophysical journal international,2013.
APA	Huang, Wentao,Dupont-Nivet, Guillaume,Lippert, Peter C.,van Hinsbergen, Douwe J. J.,&Hallot, Erwan.(2013).Inclination shallowing in Eocene Linzizong sedimentary rocks from Southern Tibet: correction, possible causes and implications for reconstructing the India-Asia collision.geophysical journal international.
MLA	Huang, Wentao,et al."Inclination shallowing in Eocene Linzizong sedimentary rocks from Southern Tibet: correction, possible causes and implications for reconstructing the India-Asia collision".geophysical journal international (2013).