Supported by the program for the Ministry of Education of China;National Natural Science Foundation of China (Grant Nos. B07039, 40673020 and 40521001);the SinoPec project (Grant No. G0800-06-ZS-319)
Mo isotopes along with Nd isotopes and other geochemical characteristics of the Phanerozoic clastic sediments from the northern margin of the Yangtze block were analyzed by MC-ICP-MS and some other techniques, spannin...
Supported by National Natural Science Foundation of China (Grant No.40471139);National Basic Research Program of China (Grant No.2004CB720206);the Special Fund of Scientific Research for Doctoral Subjects of Chinese Universities (Grant No. 20070574005);the RGC Grant of the HKSAR (HKU7243/04H)
The paleoenvironment indicated by the geochronology,major oxides——SiO2,Al2O3 and TOFE(Fe2O3 + FeO),and CIA(Chemical Index of Alteration) value of the red earth and brown-yellow silt primarily characterized by the Li...
Supported by the National Natural Science Foundation of China(Grant No.90411015);the National Science and Technology Support Project(Grant No.2006BAK21B02);the University Doctoral Foundation(Grant No.20050284011);the Foundation of Important Basic Research at Nanjing University(Grant No.0209005206);the Open Foundation of the State Key Laboratory of Loess and Qua-ternary Geology from the Institute of Earth Environment,CAS(Grant No.SKLLQG0503);the Physical Geography of"985"Items and the Test Foundation of Modern Analyses Center of Nanjing University(Grant No.0209001309)
Based on the detailed analyses,multi-proxies such as AMS 14 C dating,grain size,component and morphology of heavy minerals,micromorphology of zircon,magnetic susceptibility,Rb/Sr and Hg content are used to research th...
Supported by 2003 Liu Tungsheng National Top Science and Technology Awards
The anisotropy of magnetic susceptibility (AMS) is a rapid and precise tool for determining paleowind directions. During the past several decades, AMS has been used for determining paleowind directions of Chinese loes...
Various methods for precise orbit determination (POD) of low earth orbiters (LEO) are briefly intro-duced in this paper. Based on the software named SHORD-Ⅲ developed by our institute,sin-gle-difference (SD) and zero...
supported by the Key Project of the National Natural Science Foun-dation of China(Grant No.90411015);the National Natural Science Foundation of China(Grant No.40271103);Open Foundation of the State Key Laboratory of Loess and Quaternary Geology from the Insti-tute of Earth Environment,CAS(Grant No.SKLLQG0503);Physical Geography of“985”Item and Foundation of Modern Analyses Center of Nanjing University.
Based on the principle that the present is the key to the past , detailed analyses, such as AMS 14C dating, grain size, component and morphology of heavy minerals, micro-morphology of zircon, Rb/Sr, magnetic susceptib...
the Special Coordination Funds for Promoting Science and Technology of the Science and Technology Agency of Japan and by the National Natural Science Foundation of China (Grant Nos. 49732060 and 49894170).
Based on pollen records in B-3GC gravity core, environmental change since 9500 aBP of Okinawa Trough and its adjacent islands was derived. The result showed that the most time during this period was in a warm temperat...
This work was supported by the National Key Basic Research Development Planning (Grant No. 1999043502) ; the National Natural Science Foundation of China (Grant No. 49671009).
For past decades there have been many studies on the climate features during the last interglacial and glacial periods. A comparison between the loess record of western China with that of monsoon areas shows some regi...
Core NS-93-5 was taken from the mild slope terrace of the southern South China Sea (SCS), which has preserved the steadiness depositional record of the normal marine environment since late Quaternary. Sedimentary sequ...
MOST of the preexisting paleomagnetic studies on the Tarim Basin were conducted within its northern ànd northwestern margins with the exception that few people have paid their attention to starting paleomagnetism stu...