Shiming Wan
Datos Biográficos
| ID | 6370977 |
|---|---|
| NOMBRE | Shiming Wan |
| NOMBRES | Shiming |
| APELLIDO | Wan |
| FIRMA | WAN S |
| AFILIACIONES | Chinese Academy of Sciences |
| ORCID | 0000-0001-9335-2248 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 4 |
| TOTAL DE CITAS | 0 |
| TOTAL COMO AUTOR | 4 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 2011 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2024 |
| ÍNDICE H | 0 |
Wind-driven sediment exchange between the Indian marginal seas over the last 18 000 years
The Indian Coastal Current is the only channel for material exchange between the two largest marginal seas in the northern Indian Ocean: the Bay of Bengal and the Arabian Sea. However, its past history is poorly known, limiting accurate predictions of its future changes. Here, we present a new clay mineral record from south of India supported by interpretations of model simulations to trace its variability over the last 18 000 years. Decreased sm…
Deep-sea carbonate preservation in the western Philippine Sea over the past 1Ma
Sediment provenance and paleoenvironmental change in the middle Okinawa Trough during the last 18.5 ky
Sensitive grain-size records of Holocene East Asian summer monsoon in sediments of northern South China Sea slope
Changes in paleoenvironments over the last 17,500 yr have been documented by a high-resolution clay mineralogy and grain–size records of Core KNG5 from the northern slope of the South China Sea. Our results indicate that clay minerals are mainly from the Pearl River from 17,500 to 12,500 cal yr BP, and the South China Sea modern current system began to form since 12,500 cal yr BP, as a result, Taiwan turns to be the major contributor of clay mine…
Sin obras prominentes en esta página.
Sensitive grain-size records of Holocene East Asian summer monsoon in sediments of northern South China Sea slope
Changes in paleoenvironments over the last 17,500 yr have been documented by a high-resolution clay mineralogy and grain–size records of Core KNG5 from the northern slope of the South China Sea. Our results indicate that clay minerals are mainly from the Pearl River from 17,500 to 12,500 cal yr BP, and the South China Sea modern current system began to form since 12,500 cal yr BP, as a result, Taiwan turns to be the major contributor of clay mine…
Sediment provenance and paleoenvironmental change in the middle Okinawa Trough during the last 18.5 ky
Deep-sea carbonate preservation in the western Philippine Sea over the past 1Ma
Wind-driven sediment exchange between the Indian marginal seas over the last 18 000 years
The Indian Coastal Current is the only channel for material exchange between the two largest marginal seas in the northern Indian Ocean: the Bay of Bengal and the Arabian Sea. However, its past history is poorly known, limiting accurate predictions of its future changes. Here, we present a new clay mineral record from south of India supported by interpretations of model simulations to trace its variability over the last 18 000 years. Decreased sm…
Geology and Paleoclimatology Research (4 obras) · Geochemistry (3 obras) · Geological formations and processes (3 obras) · Geology (3 obras) · Holocene (3 obras) · Oceanography (3 obras) · Climatology (2 obras) · Geomorphology (2 obras) · Methane Hydrates and Related Phenomena (2 obras) · Bay (1 obras)