17 results on '"Xu, Taoyu"'
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2. Seismic reflection characteristics and controlling factors of shallow gas in the alongshore mud clinoform of the East China Sea
3. Holocene sedimentary evolution and hypoxia development in the subaqueous Yangtze (Changjiang) Delta, China
4. Formation of the Yangtze Shoal in response to the post-glacial transgression of the paleo-Yangtze (Changjiang) estuary, China
5. Stratigraphic framework and evolution of the mid–late Quaternary (since marine isotope stage 8) deposits on the outer shelf of the East China Sea
6. The fluid mud flow deposits represent mud caps of Holocene hybrid event beds from the widest and gentlest shelf
7. Heavy-mineral-based provenance and environment analysis of a Pliocene series marking a prominent transgression in the south Yellow Sea
8. Late Quaternary sedimentary evolution of the outer shelf of the East China Sea
9. Formation processes and evolution of Holocene sediments in the Yangtze offshore area: A review and new interpretation on the response to sea-level rise and deltaic progradation
10. Exploring Spatiotemporal Paleoenvironmental and Paleoceanographic Changes on the Continental Shelf Using Authigenic Greigite: A Case Study From the East China Sea
11. Sequence stratigraphy of the subaqueous Changjiang (Yangtze River) delta since the Last Glacial Maximum
12. Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene
13. Authigenic Iron Sulfides Indicate Sea‐Level Change on the Continental Shelf: An Illustration From the East China Sea
14. Carbon isotope and rare earth element composition of Late Quaternary sediment gravity flow deposits on the mid shelf of East China Sea: Implications for provenance and origin of hybrid event beds
15. Sedimentary architecture of the Bohai Sea China over the last 1 Ma and implications for sea-level changes
16. Hainan mantle plume produced late Cenozoic basaltic rocks in Thailand, Southeast Asia
17. THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka
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