相关期刊:《Science China Earth Sciences》《Journal of Ocean University of China》《Science China Chemistry》《World Journal of Gastrointestinal Pharmacology and Therapeutics》更多>>
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...
the National Natural Science Foundation of China (Grant Nos. 49625609 and 49421007).
As the Okinawa Trough is a back-arc basin in early spreading, modern submarine hydrothermal activity and minerallization have many characteristics which have aroused wide attention. Up to now, three well-known hydro-t...
a joint Chinese-French study funded by the National Natural Science Foundation of China (Grant Nos. 49776292 and 49736210).
Planktonic foraminiferal δ18O record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely t...
THERE are four submarine hydrothermal activity areas in the Middle Okinawa Trough. They are Izena hole(127°05’E, 27°16’N), Iheya Deep (126°58’E, 27°33’N). Natsushima 84-1 Mound (127°08.6’E, 27°34.4’N), Wes...
Based on the analyses of foraminifer and accelerator mass spectrometer radiocarbon dating in DGKS9603 core from mid-Okinawa Trough close to bottom, oscillation curve, which expressed the relation between the surface w...
Core 255 from the southern Okinawa Trough was selected to monitor the shift of the Kuroshio axis over the last 20 000 years. During the last glacial maximum the Kuroshio axis had ever shifted outside the Okinawa Troug...
THE application of phytolith study in geology in the world has experienced a history of over 30 years. The earliest application of phytolith study to marine geology was made by Smithson when he made a study on the sub...
THE hydrothermal activity area investigated is located at the middle of the trough (126°50′—127°30′E; 27°20′—27°50′N). Some surface sediment samples and core samples were collected, with other samples from n...