SEQUENCE STRATIGRAPHY - TRANSGRESSION, REGRESSION AND SYSTEM TRACTS
SEQUENCE STRATIGRAPHY
TRANSGRESSION
Shoreline shift landward
Retrogradational pattern- fining upward
Feature name - Estuaries
Sea level rise
Deepening upward (Deep facies found at the top whereas shallow facies found at the bottom)
Transgressive system tract found - due to rapid increase in sea level
REGRESSION
Shoreline shifts seaward
either due to sedimentation - Normal regression
due to sea level fall - Forced regression
Regression is of two types
1) NORMAL REGRESSION
Shoreline shift seaward due to sedimentation
Low stand system tract, High stand system tract

2) FORCED REGRESSION
Shoreline shift seaward due to rapid fall in sea level
Falling stage system tract - rapid decrease in sea level
Coarsening upward - Progradational pattern

SYSTEM TRACTS
1) FSST - Rapid fall in sea level : Forced regression
2) LST - Sea level just start rising (initial stage when sea level start rises)
3) TST - rapid rise in sea level : Transgression (retrogradation pattern)
4) HST - Last stages of rise in sea level (progradation pattern)
BOUNDARIES
- Maximum flooding surface : TST and HST
- Sequence boundary : FSST and HST
- Maximum flooding surface is present between Transgressive system tract and High stand system tract
- The mfs often mark the bounding surface between coarsening and/or fining upward cycles
OVERALL FIGURE

RELATION OF STRATA
Upper boundary :
Erosional truncation
Toplap : Progradation
Concordance
Lower boundary
Onlap : Transgression
Downlap : Forced regression
Concordance
ONLAP:
Termination of low angle strata against a steep stratigraphic surface
Indicates Transgression
Inclined or horizontal strata terminate against a surface of greater inclination
DOWNLAP:
Termination of steep inclined strata against a low lying surface
Indicates forced regression
Onlap and downlap indicates non-depositional hiatuses
TOPLAP:
Upper boundary of depositional sequence
Termination of inclined strata against a low lying surface
Indicates progradation
OFFLAP:
a surface where stratigraphic terminations downstep basinward during forced regression.
I didn't understand in case of forced regression sea level is rapidly falling then how come its a retrogradational??
ReplyDeleteIts coarsening upward so progradational??
You are right, actually its a typing error. Thank you for your rectification.
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