Acknowledgements The research work was supported by the National Natural Science Foundation of China (No. 40971115), Scientific Research Foundation of Graduate School of N anjing University (No. 2011CL 11 ), the National Science and Technology Support Program of China (No. 2010BAK67B02), University Doctoral Foundation of China (No. 20090091110036), Open Foundation of the State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS (No. SKLLQG0817), and Major Program of Natural Science Research at University of Anhui Province (No. ZD200908).
Palaeochannels are deposits of unconsolidated sediments or semi-consolidated sedimentary rocks depos- ited in ancient, currently inactive river and stream channel systems. It is distinct from the overbank deposits of ...
Supported by the National High-Tech Research & Development Program of China (863 Program) (Grant No.2008AA06Z206);the Specialized Research Fund for the Doctoral Program of Higher Education (Grant No.20060425004)
The studies on fluvial reservoir architecture are mainly aimed at outcrop and modern deposition,but rarely at the subsurface reservoir,so there are few effective methods to predict the distribution of subsurface reser...
This research was supported by the Natural Science Foundation of Shandong Province of China under contract No.Y2000E03.
The palaeochannel evolution in the study region is divided into four stages by such methods as 14C dating. Sea water intrusion through palaeochannels has been studied as a focal point. Palaeochannels are the main pass...
The palaeochannels in the studied region are divided into four stages by such methods as 14C dating. Marine (saltwater) transgression in the palaeochannels has been studied as a focal point. Palaeochannels are the mai...
Palaeorunoff regimes were reconstructed using the equations relating annual runoff to climatic parameters and palaeoclimatic information acquired mainly by pollen analysis and peat investigation for southem Hebei (114...