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Magnetic characteristics and their paleoclimatic significance of Fengzhou loess in the Qinling Mountains of China 被引量:3
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作者 Xiangyi Lei leping yue +1 位作者 Jianqi Wang Li Zhang 《Chinese Science Bulletin》 SCIE EI CAS 1998年第18期1571-1575,共5页
The Fengzhou loess section is very typical in the Qinling Mountains. The section, about 82 m thick and underlain by the Neogene red clay, consists of 33 layers of loess and 33 layers of paleosol. The section covers Br... The Fengzhou loess section is very typical in the Qinling Mountains. The section, about 82 m thick and underlain by the Neogene red clay, consists of 33 layers of loess and 33 layers of paleosol. The section covers Brunhes normal polarity zone and Matuyama reversed polarity zone, and the B/M boundary is located in the middle of L\-8. Matuyama reversed polarity zone records Jaramillo, Olduvai and Reunion normal polarity subchrons. The boundary between Matuyama reversed polarity zone and Gauss normal polarity zone (M/Ga) appears in the lithological boundary between loess and the Neogene red clay. Loess accumulation in Fengzhou started before 2.48 Ma. The magnetic susceptibility curve indicates 33 cold_dry and humid_warm cycles of paleoclimatic variation in the Qinling Mountains during the last 2.48 Ma. The above climatic fluctuation may be well compared with that of the oxygen isotopic records from deep_sea deposits. 展开更多
关键词 QINLING MOUNTAINS PALEOCLIMATIC change magnetic SUSCEPTIBILITY MAGNETOSTRATIGRAPHY of loess.
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