• Provide an understanding of the practical concepts and procedures for recognizing and interpreting the stratigraphic nature of microfossils in the Mesozoic and Cenezoic.
• Study the Value of High-resolution biostratigraphy is demonstrated with microfossils, their abundance and marker species in genetic sequences, types of reservoirs, group rocks into series of time correlatable chronostratigraphic genetic intervals, and establish sound correlations,
• Improve ability to observe and understand the cyclic nature of sediments in your wells.
• Apply High resolution biostratigraphy with abundance and marker species are used to identify, correlate and age date MFS on logs and seismic.
• Correlate wells using cyclic packages of sediments, log signatures patterns, in between age datable mapping horizons, Maximum Flooding Surfaces. 
• Dissect Extreme value of Maximum Flooding Surfaces, their Condensed Sections are emphasized throughout the course; Identified on well-logs, seismic profiles, as time lines and age datable mapping horizons to construct various, maps with reservoir trends for prospect generation during highstand and lowstand of relative sea level.
• Comprehend Maximum Flooding Surface (MFS) on well-logs correlated to age datable continuous reflectors on seismic is necessary to construct accurate time structure and seismic facies maps and to ensure reservoir facies are properly correlated regionally.
• Identify types of potential reservoir sands, their position and location from shelf slope break and their associated systems tract, parallel or perpendicular to strike, above and below Salt, as basin floor fans, channel and overbank sands, sheet or prograding sands to IVF sands to improve your ability to locate reservoirs, structural traps, stratigraphic traps, identify source rocks and migration pathways to reduce risk and cost
• Analyze Maximum Flooding Surface and their deposition Facies the MFS condensed section are shown as Source Rocks, Seals, and mapping Horizons.
• Understand Global Cycle Chart, is used to subdivide wells into third order depositional, highstand, transgressive and lowstands systems tracts including prograding complex, , slope fan  and basin floor fan complex and to recognized major and minor occurrences of source rocks and seals for reservoirs.
• The cyclic patterns and MFS are seen in diagrams below: (Dashed line, MFS. at top of TST (green).

A MUST ATTEND for geologists, geophysicists, engineers and managers who are setting forth to improve their application and understanding of advanced biostratigraphy and therefore reducing risk and cost in exploration and development in the petroleum industry.