Magnetostratigraphy and rock magnetism of the Neogene Kuitun He section (northwest China): implications for Late Cenozoic uplift of the Tianshan mountains
J Charreau, Y Chen, S Gilder, S Dominguez… - Earth and Planetary …, 2005 - Elsevier
In order to better constrain the tectonic evolution of central Asia under the influence of the
India–Asia collision, we carried out a magnetostratigraphic study at the Kuitun He section,
on the northern flank of the Tianshan range (northwest China). A total of 801 samples were
collected from a 1559-m-thick section, which is composed mainly of fluvio-lacustrine
sandstone and conglomerate. Stepwise thermal and alternating field demagnetization
isolated a linear magnetization component that decays univectorally toward the origin and …
India–Asia collision, we carried out a magnetostratigraphic study at the Kuitun He section,
on the northern flank of the Tianshan range (northwest China). A total of 801 samples were
collected from a 1559-m-thick section, which is composed mainly of fluvio-lacustrine
sandstone and conglomerate. Stepwise thermal and alternating field demagnetization
isolated a linear magnetization component that decays univectorally toward the origin and …
[PDF][PDF] Magnetostratigraphy and rock magnetism of the Neogene Kuitun He section (northwest China): implications for Late Cenozoic uplift of the Tianshan mountains
SS Avouacd, D Sunf, Y Lif, WM Wangg - picture.iczhiku.com
In order to better constrain the tectonic evolution of central Asia under the influence of the
India–Asia collision, we carried out a magnetostratigraphic study at the Kuitun He section,
on the northern flank of the Tianshan range (northwest China). A total of 801 samples were
collected from a 1559-m-thick section, which is composed mainly of fluvio-lacustrine
sandstone and conglomerate. Stepwise thermal and alternating field demagnetization
isolated a linear magnetization component that decays univectorally toward the origin and …
India–Asia collision, we carried out a magnetostratigraphic study at the Kuitun He section,
on the northern flank of the Tianshan range (northwest China). A total of 801 samples were
collected from a 1559-m-thick section, which is composed mainly of fluvio-lacustrine
sandstone and conglomerate. Stepwise thermal and alternating field demagnetization
isolated a linear magnetization component that decays univectorally toward the origin and …
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