Qüxü batholith, located on the Eurasia side nearby the Yarlung Zangbo suture zone, is a complex composed of gabbro, diorite, quartz-monzodiorite, granodiorite and granite. The ages of the main part of the ba...Qüxü batholith, located on the Eurasia side nearby the Yarlung Zangbo suture zone, is a complex composed of gabbro, diorite, quartz-monzodiorite, granodiorite and granite. The ages of the main part of the batholith are from 40 to 50 Ma, corresponding to the final stage of the northward subduction of the Tethys ocean floor and the beginning展开更多
Based on the data of organic carbon stable isotope ratios and magnet ic susceptibility, climate evolution in the past 5 kaB.P. in Poyang Lake plain (in Jiangxi Province) has been reconstructed. The results of the re...Based on the data of organic carbon stable isotope ratios and magnet ic susceptibility, climate evolution in the past 5 kaB.P. in Poyang Lake plain (in Jiangxi Province) has been reconstructed. The results of the research indicate that the climate evolution can be divided into nine stages in the past 5 kaB.P.. Comparisons of different regional environmental records suggest that the intens ity and the temporal spatial changes of monsoon in China mainly controlled the climate evolution.展开更多
基金Project supported by the National Post-Doctor Science Foundation of China and the National Natural Science Foundation of China
文摘Qüxü batholith, located on the Eurasia side nearby the Yarlung Zangbo suture zone, is a complex composed of gabbro, diorite, quartz-monzodiorite, granodiorite and granite. The ages of the main part of the batholith are from 40 to 50 Ma, corresponding to the final stage of the northward subduction of the Tethys ocean floor and the beginning
文摘Based on the data of organic carbon stable isotope ratios and magnet ic susceptibility, climate evolution in the past 5 kaB.P. in Poyang Lake plain (in Jiangxi Province) has been reconstructed. The results of the research indicate that the climate evolution can be divided into nine stages in the past 5 kaB.P.. Comparisons of different regional environmental records suggest that the intens ity and the temporal spatial changes of monsoon in China mainly controlled the climate evolution.
