Automated Author ProfileRidley Thomas, W N
Ridley Thomas, W N
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 38.6 (sum of 27 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
High-resolution boomer profiles from Tai O Bay, Hong Kong SAR, were ground-truthed using ten discontinuously sampled boreholes penetrating bedrock with a maximum length of 82.1 m. The relationship between depth below seabed and seismic profiles was established through the measurement of two borehole compressional-wave velocity profiles. In departure from previous interpretations, nine Quaternary seismic units were identified, which can be divided into eight systems tracts formed by cycles of fourth-order sea-level fluctuations dating back at least to marine isotope stage (MIS) 7 (ca. 190-245 ka). These consist of two lowstand systems tracts, two transgressive systems tracts, and four highstand systems tracts. Secondary unconformities within the highstand deposits are interpreted to document fifth-order sea-level fluctuations. Lowstand deposits are less common because, as soon as the sea level drops by a few metres, Tai O Bay becomes sub-aerially exposed, leading to widespread non-deposition or erosion. At the same time, extensive fluvial erosion and channel incision take place. Filling of the fluvial channels occurs during rising sea level. Lowstand sediments (if present) are generally landslide deposits laid down on a basal alluvial plain. Uncorrected accelerator mass spectrometry (AMS) radiocarbon dates of mollusc shells show that the depositional environment was marine since 6.2 ka, becoming gradually more brackish as a result of progradation of the Pearl River delta. The computed average sedimentation rate for the period 6.2-4.1 ka is 4.4 m/1,000 year, and approximately 1 m/1,000 year since 4.1 ka.
Authors
- Bahr, André ;
- Wong, H K ;
- Yim, Wyss W-S ;
- Huang, G ;
- Lüdmann, Thomas ;
- Chan, L S ;
- Ridley Thomas, W N
No description available
Authors
- Ridley Thomas, W N ;
- Yeats, Robert S ;
- Hart, Stanley R
No description available
Authors
- Ridley Thomas, W N ;
- Yeats, Robert S ;
- Hart, Stanley R
No description available
Authors
- Ridley Thomas, W N ;
- Yeats, Robert S ;
- Hart, Stanley R
No description available
Authors
- Ridley Thomas, W N ;
- Yeats, Robert S ;
- Hart, Stanley R
No description available
Authors
- Ridley Thomas, W N ;
- Talwani, Manik ;
- Udintsev, Gleb B
No description available
Authors
- Ridley Thomas, W N ;
- Talwani, Manik ;
- Udintsev, Gleb B
No description available
Authors
- Ridley Thomas, W N ;
- Talwani, Manik ;
- Udintsev, Gleb B
No description available
Authors
- Ridley Thomas, W N ;
- Talwani, Manik ;
- Udintsev, Gleb B