Analysis of the four cases of the sequence boundary (SB)-transgressive surf
ace (TS) relation in nature shows that applying transgressive surfaces as s
equence boundaries has the following merits: it improves the methodology of
stratigraphic subdivision; the position of transgressive surface in a sea
level curve is relatively fixed; the transgressive surface is a transformin
g surface of the stratal structure; in platforms or ramps, the transgressiv
e surface is the only choice for determining the sequence boundary; the tra
nsgressive surface is a readily recognized physical surface reflected by se
ismic records in seismostratigraphy. The paper reaches a conclusion that to
delineate a SE in terms of the TS is theoretically and practically better
than to delineate it between highstand and lowstand sediments as has been d
one traditionally.