S C Porter
Biographic Data
| ID | 5471850 |
|---|---|
| NAME | S C Porter |
| GIVEN NAMES | S C |
| FAMILY NAME | Porter |
| SIGNATURE | PORTER S C |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 10 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1990 |
| LATEST PUBLICATION YEAR | 1992 |
| H-INDEX | 1 |
Chronology of the Baxie Loess Profile and the History of Monsoon Climates in China Between 17,000 and 6000 Years BP
The valley of the Baxie River, situated in the western region of the Loess Plateau in central China, contains a loess profile 15 m thick, which can be considered representative of loess-paleosol sequences formed over the last 17 ka. Both thermoluminescence (TL) determinations on fine-grained sediment (4–11 μm) and 14 C determinations on various organic fractions of paleosols from the profile have provided an extremely useful chronological framewo…
The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China
Report on Inqua-finances
Chronology of the Baxie Loess Profile and the History of Monsoon Climates in China Between 17,000 and 6000 Years BP
The valley of the Baxie River, situated in the western region of the Loess Plateau in central China, contains a loess profile 15 m thick, which can be considered representative of loess-paleosol sequences formed over the last 17 ka. Both thermoluminescence (TL) determinations on fine-grained sediment (4–11 μm) and 14 C determinations on various organic fractions of paleosols from the profile have provided an extremely useful chronological framewo…
The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China
Report on Inqua-finances
Chronology of the Baxie Loess Profile and the History of Monsoon Climates in China Between 17,000 and 6000 Years BP
The valley of the Baxie River, situated in the western region of the Loess Plateau in central China, contains a loess profile 15 m thick, which can be considered representative of loess-paleosol sequences formed over the last 17 ka. Both thermoluminescence (TL) determinations on fine-grained sediment (4–11 μm) and 14 C determinations on various organic fractions of paleosols from the profile have provided an extremely useful chronological framewo…
Geography (3 works) · Geology (3 works) · Climatology (2 works) · East Asian Monsoon (2 works) · Geology and Paleoclimatology Research (2 works) · Loess (2 works) · Monsoon (2 works) · Paleontology (2 works) · Paleosol (2 works) · Physical geography (2 works)