Loess is the most important aeolian deposit of the Quaternary and plays an important role in explorations of the evolution of paleoclimate and paleoenvironment. In recent years, historians of science have been working on how loess research originated, developed, and was promoted in Europe in the early 19th century. The Chinese community has a clear history of the loess research from the late 20th century. However, it remains unclear when and how modern loess studies were communicated between western and eastern academic societies and who contributed to the development and dissemination of modem loess knowledge, especially from the western to the eastern societies. Based on books, essays, memoirs, travel notes, published letters, and other t...
Liu Tungsheng featured on the list of twelve notable loess investigators prepared for the great Loes...
In this paper characteristics of loess are discussed from a pedological perspective. A new model of ...
Loess formation generally involves the four main stages of production, deflation, transportation, an...
Loess is the most important aeolian deposit of the Quaternary and plays an important role in explora...
Loessification is a process by which a body of non-loess ground is transformed into a body of loess ...
Loess is well developed at the middle latitude of the Eurasian continent. I occupies nearly 400,000 ...
Loess-soil sequences are among the best terrestrial records of paleoenvironments. Those in northern ...
Leonard Horner (1785-1864) made substantial contributions to the study of loess. He made field trips...
The loess-paleosol sequences of the Danube basin contain the longest and most complete terrestrial r...
Charles Lyell (1797–1875) was an important loess pioneer. His major contribution was to distribute i...
Loess was first identified in England as early as the mid-19th century, although these deposits were...
Well-preserved loess deposits are found on the foothills of mountains along the middle reaches of th...
Loess is an eolian (windblown) sediment that is an important archive of Quaternary climate changes. ...
Leonard Horner (1785–1864) was a pioneer in the study of loess. His 1836 paper on the geology of Bon...
The two critical books, launching the study and appreciation of loess, were ‘Charakteristik der Fels...
Liu Tungsheng featured on the list of twelve notable loess investigators prepared for the great Loes...
In this paper characteristics of loess are discussed from a pedological perspective. A new model of ...
Loess formation generally involves the four main stages of production, deflation, transportation, an...
Loess is the most important aeolian deposit of the Quaternary and plays an important role in explora...
Loessification is a process by which a body of non-loess ground is transformed into a body of loess ...
Loess is well developed at the middle latitude of the Eurasian continent. I occupies nearly 400,000 ...
Loess-soil sequences are among the best terrestrial records of paleoenvironments. Those in northern ...
Leonard Horner (1785-1864) made substantial contributions to the study of loess. He made field trips...
The loess-paleosol sequences of the Danube basin contain the longest and most complete terrestrial r...
Charles Lyell (1797–1875) was an important loess pioneer. His major contribution was to distribute i...
Loess was first identified in England as early as the mid-19th century, although these deposits were...
Well-preserved loess deposits are found on the foothills of mountains along the middle reaches of th...
Loess is an eolian (windblown) sediment that is an important archive of Quaternary climate changes. ...
Leonard Horner (1785–1864) was a pioneer in the study of loess. His 1836 paper on the geology of Bon...
The two critical books, launching the study and appreciation of loess, were ‘Charakteristik der Fels...
Liu Tungsheng featured on the list of twelve notable loess investigators prepared for the great Loes...
In this paper characteristics of loess are discussed from a pedological perspective. A new model of ...
Loess formation generally involves the four main stages of production, deflation, transportation, an...