Add to ORKGLoess-soil sequences are among the best terrestrial records of paleoenvironments. Those in northern China provide a 22 million-year (Ma) geological history of the Asian deserts (dust sources), winter monsoon (dust carrier) and summer monsoon (moisture carrier) winds, and the regional vegetation. Loess geochemistry represents one of the most dynamic research fields in loess-based Paleoclimatology. Some of the most frequent approaches are reviewed here with emphasis to the loess deposits in China
The Quaternary wind-blown Chinese loess-paleosol sequence, which developed as a product of the inten...
The Quaternary wind-blown Chinese loess-paleosol sequence, which developed as a product of the inten...
Loess is the most important aeolian deposit of the Quaternary and plays an important role in explora...
Loess deposits in the Eastern Qinling Mountains (central China) provide a detailed archive for recon...
This paper aims to characterize seasonal variations in the potential sources of loess deposited on t...
Loess is well developed at the middle latitude of the Eurasian continent. I occupies nearly 400,000 ...
Whether during past climate stages or into a progressively warming world, changes in precipitation c...
The Chinese Loess Plateau in north central China contains one of the most valuable Cenozoic climate ...
ABSTRACT. Loess deposition within the Loess Plateau of China records the history of environmental ch...
The magnetic susceptibility of loess and paleosols in central China represents a proxy climate index...
Loess is widely distributed over Asia and North America and constitutes one of the most important su...
Recent chronological studies have revealed significant site-specific variations in loess sedimentati...
Loess deposition within the Loess Plateau of China records the history of environmental change over ...
The aeolian loess blanketing the Chinese Loess Plateau (CLP) is sensitive to climate change in monso...
Eolian deposit (loess) in the Chinese Loess Plateau is an excellent record of paleo-climate change s...
The Quaternary wind-blown Chinese loess-paleosol sequence, which developed as a product of the inten...
The Quaternary wind-blown Chinese loess-paleosol sequence, which developed as a product of the inten...
Loess is the most important aeolian deposit of the Quaternary and plays an important role in explora...
Loess deposits in the Eastern Qinling Mountains (central China) provide a detailed archive for recon...
This paper aims to characterize seasonal variations in the potential sources of loess deposited on t...
Loess is well developed at the middle latitude of the Eurasian continent. I occupies nearly 400,000 ...
Whether during past climate stages or into a progressively warming world, changes in precipitation c...
The Chinese Loess Plateau in north central China contains one of the most valuable Cenozoic climate ...
ABSTRACT. Loess deposition within the Loess Plateau of China records the history of environmental ch...
The magnetic susceptibility of loess and paleosols in central China represents a proxy climate index...
Loess is widely distributed over Asia and North America and constitutes one of the most important su...
Recent chronological studies have revealed significant site-specific variations in loess sedimentati...
Loess deposition within the Loess Plateau of China records the history of environmental change over ...
The aeolian loess blanketing the Chinese Loess Plateau (CLP) is sensitive to climate change in monso...
Eolian deposit (loess) in the Chinese Loess Plateau is an excellent record of paleo-climate change s...
The Quaternary wind-blown Chinese loess-paleosol sequence, which developed as a product of the inten...
The Quaternary wind-blown Chinese loess-paleosol sequence, which developed as a product of the inten...
Loess is the most important aeolian deposit of the Quaternary and plays an important role in explora...