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《Earth Science Frontiers》 2002-01
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PELAGIC SEDIMENTARY RECORDS OF THE NINETYEAST RIDGE AND THE LATE CENOZOIC IMPORTANT TECTONO-ENVIRONMENTAL EVENTS

FANG Nian-qiao,DING Xuan,LIU Yong-qin, HU Chao-yong,CHEN Xue-fang,ZHANG Zhen-fang (Institute of Marine Geology and Geophysics, China University of Geosciences,Beijing 100083, China)  
The pelagic sedimentary records from the North of the Ninetyeast Ridge can be regarded as a tele-monitor for understanding the uplift of the Qinghai-Xizang (Tibetan) Plateau. Using the identification of foraminiferal assemblage and analysis of the foraminiferal test and combining the above results with the previous sedimentary, geochemical, paleomagnetic and micropaleontological data, we make an integrated discussion about the ridge records since 9Ma displayed typically by ODP758 site. Some significant signals of variable ocean environment, which response to the phased uplift of the plateau dating from 3.7Ma to 3.2Ma, 0.8Ma to 0.6Ma and 0.17Ma to 0.16Ma, can be obviously recognized in the records. We point out that the intensity of Indian winter monsoon is just a key symptom to mirror the tectonics of the plateau. On the basis of this point, the period marking the most important turn of environment during the Late Cenozoic shown by the ridge records has been found between 3.7Ma and 3.2Ma.
【Fund】: 国家重点基础研究发展规划项目 (G19980 40 80 0 ) ;; 国家自然科学基金资助项目 ( 4 0 170 6 14 )
【CateGory Index】: P736.2
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