--> Space, Things, Time, and Events: Horacio Harrington, Derek Ager, and the Dichotomous Future of Sequence Stratigraphy
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AAPG Annual Convention and Exhibition

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Space, Things, Time, and Events: Horacio Harrington, Derek Ager, and the Dichotomous Future of Previous HitSequenceNext Hit Previous HitStratigraphyNext Hit

Abstract

The conceptual framework and practical application of Previous HitsequenceNext Hit stratigraphic principles followed two distinct yet overlapping paths nearly from the onset of Previous HitsequenceNext Hit stratigraphic studies. The varied applications of Previous HitsequenceNext Hit concepts to seismic stratigraphic data and to chronostratigraphic data fostered the development of multiple working methods and uses of terminology that all fall under the umbrella of Previous HitsequenceNext Hit Previous HitstratigraphyNext Hit. The most obvious example of multiple working methodologies being separated by a common language is the use and stratigraphic placement of the ‘Previous HitsequenceNext Hit boundary’. Throughout the decades, ‘Previous HitsequenceNext Hit stratigraphers’ have chosen nearly every position within the systems tracts framework to define the Previous HitsequenceNext Hit boundary (e.g. top of the HST, top of the FSST, base of the TST, etc.). A variety of causes can be attributed to the disparate use of Previous HitsequenceNext Hit stratigraphic terminology over the years, but 21st Century Previous HitsequenceNext Hit stratigraphers fall largely into one of two camps. Seismic stratigraphers, who utilize increasingly high-resolution 3-D seismic stratigraphic data, or chronostratigraphers, who utilize increasingly high-resolution chronostratigraphic data. The two groups, who both practice Previous HitsequenceNext Hit Previous HitstratigraphyNext Hit, not only rely on fundamentally different sets of data, they also have fundamentally different objectives. Seismic Previous HitstratigraphyNext Hit endeavors to determine the spatial distribution of strata (and their attendant oil and gas); chronostratigraphy aims to determine the Previous HitsequenceNext Hit of events in Earth history and ultimately the causes and consequences of those events. These separate, but related, aims and primary sets of data are largely responsible for the varied use of Previous HitsequenceNext Hit stratigraphic terms and principles. The revolution of high-resolution 3-D seismic Previous HitstratigraphyNext Hit is well documented and is the driving force behind 21st Century seismic Previous HitsequenceNext Hit Previous HitstratigraphyNext Hit. This presentation aims to demonstrate that a similar revolution in high-resolution global chronostratigraphy is also taking place and has similarly revolutionized outcrop- and core-based Previous HitsequenceNext Hit Previous HitstratigraphyNext Hit over the past two decades as well. The future of both Previous HitsequenceNext Hit stratigraphic enterprises (high-resolution seismic Previous HitstratigraphyNext Hit and high-resolution chronostratigraphy) rests in our ability as a community of Previous HitsequenceTop stratigraphers to overcome the barriers presented by our common language and effectively integrate both stratigraphic revolutions.