Sequence Stratigraphy Basics Course

Free Course
 “Well Logging Introduction”
• Initiative training service, training your team and apply courses in your real case study with all support you need to solve complex problem with after courses service, self-training course give you video lectures with specialists in your field:
1. Well Logging Simple and Easy
• Well Logging Simple An...
2. Introduction to Well Logging
• Introduction to Well L...
3. Gamma Ray Tool | Gamma-ray logging
• Well Logging | Gamma R...
4. Gamma Ray Log
• Well Logging | Gamma R...
5. Gamma-Ray & Neutron Porosity Log
• Well Logging Gamma-Ra...
6. Spontaneous potential & Gamma-Ray Logs
• Well Logging | Spontan...
100% Free Basic introductory course on Seismic Method:
Seismic Survey
• Seismic Survey
Seismic Imaging | Seismic method | Geophysics
• Seismic Imaging | Seis...
Basic principles of the seismic method | Seismic Principles
• Basic principles of th...
Marine Seismic Surveys | Offshore Seismic Surveying
• Marine Seismic Surveys...
Seismic Survey Methods
• Seismic Survey Methods
Seismic Air Guns Operation
• Seismic Air Guns Opera...
Seismic Vibrator | Seismic Survey Vibratory Buggy
• Seismic Vibrator | Sei...
Exploring with Seismic Vibration
• Exploring with Seismic...
sequence stratigraphy,stratigraphy,sequence stratigraphy basics,sequence stratigraphy lecture,what is sequence stratigraphy,parasequence in sequence stratigraphy,applications of sequence stratigraphy,principles of sequence stratigraphy,sequence stratigraphy systems tracts,environmental sequence stratigraphy,introduction to sequence stratigraphy,sequence boundary,seismic stratigraphy,principles of stratigraphy,applications of stratigraphy,sequence

[@masoz91]

None of the definitions are correct in the first slide. Transgression and regression describe the position of the shoreline. Highstand and lowstand are not necassrily caused by eustatic sea level, they are defined by relative sea level (accomodation+sediment supply).

[@wwlittle]

Very nicely presented, both visually and orally; however, there are significant misconceptions, particularly with respect to vocabulary. You are mixing terms that relate to base level rise and fall, shoreline transgression and regression, and deposition progradation and retrogradation. These are related but do not have a one-to-one correlation and are important to distinguish. There is inconsistency in distinguishing between the relative influence of accommodation and sediment supply vs. simple base-level fluctuation. The figure used for the FSST in proximal sections should be an erosional surface, not an incised valley fill. Again, a nice presentation, but the content needs some work.