Class IV AVA Anomalies in High TOC Shale, a Case Study from Namibia, West Africa

References

1. Altowairqi, Y. Rezaee, R. Evans, Rd B. Urosevic, Th M.
   (2015). Measuring Elastic Properties to determine the influence of TOC on Synthetic Shale Samples. Aseg-Pesa, 1–5.
   [Google Scholar]
2. Avseth, P and Carcione, J.
   (2015). Rock-physics analysis of clay-rich source rocks on the Norwegian Shelf. The Leading Edge. 34 (11), 1340–1348.
   [Google Scholar]
3. Castagna, J. Batzle, M. Eastwood, R.
   . (1985). Relationships between compressional wave in elastic silicate. Geophysics. 50 (4), 571–581.
   [Google Scholar]
4. Loseth, H. Wensaas, L. Gading, M. Duffaut, K. Springer, M.
   . (2011). Can hydrocarbon source rocks be identified on seismic data?. Geology. 39 (12), 1167–1170.
   [Google Scholar]
5. Qin, X. Han, D. Zhao, L.
   (2014). Rock physics modelling of organic-rich shales with different maturity levels. SEG Technical Program Expanded Abstracts 2014. , 2952–2957.
   [Google Scholar]
6. Vernik, L. Landis, C.
   . (1996). Elastic anisotropy of source rocks: Implications for hydrocarbon generation and primary migration. AAPG Bulletin. 80 (4), 531–544.
   [Google Scholar]
7. Yenugu, M. Han, D.
   (2013). Seismic characterization of kerogen maturity : An example from Bakken shale Seismic characterization of kerogen maturity : An example from Bakken shale. SEG Technical Program Expanded Abstracts. 1 (,), 2773–2777.
   [Google Scholar]