Peter R. Vail1,
Gerald R. Baum1
(1) Rice University, Houston, TX
Abstract: Historical development of the coastal onlap chart and eustatic sea level cycles
In the 1950’s, Larry Sloss
proposed major tectonic-stratigraphic sequences used for regional correlations.
During the late 1950’s, local onlap charts, mostly Paleozoic and Mesozoic, were
compiled from the regional studies performed at Exxon’s affiliates. In the
early 1960’s, as seismic
acquisition and processing techniques became more
sophisticated, these onlap cycles could be readily recognized and dated
paleontologically, especially in the Cenozoic. Additionally, the
seismic
patterns and geometries observed could be related to stratal surfaces seen in
geological data. This work was released in 1977, AAPG Memoir 26, laying the
foundation for
seismic
stratigraphy.
The late 1970’s-early 1980’s
witnessed several seminal changes in research direction. A series of applied
seismic
projects began to reveal repetitive patterns of deposition, including
incised-valleys feeding lowstand wedges and the enigmatic detached fans. The
latter were quite different from previously recognized turbidite deposits.
Simultaneously, outcrop studies in Alabama more accurately defined and dated
sequence
boundaries
and flooding events. In addition, a two-component system
used rates of sea level change and subsidence to provide a graphic solution to
sea level. For the first time, qualitative sea level changes were
differentiated from coastal onlap, and flooding events (condensed sections)
became as significant as unconformities. In an iterative process between
seismic
, wireline logs, cores and outcrops, the technology of
sequence
stratigraphy evolved and was published formally in 1988.
The controversy of eustasy still
remains, particularly for the Mesozoic. Oxygen isotope records, a proxy for
climate and/or sea level change, suggest eustasy is the primary mechanism in
creating sequence
boundaries
.
AAPG Search and Discovery Article #90914©2000 AAPG Annual Convention, New Orleans, Louisiana