About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

AAPG Special Volumes

Abstract


Pub. Id: A166 (1984)

First Page: 1

Last Page: 6

Book Title: M 36: Interregional Previous HitUnconformitiesNext Hit and Hydrocarbon Accumulation

Article/Chapter: Comparative Anatomy of Cratonic Previous HitUnconformitiesNext Hit

Subject Group: Seismic Stratigraphy, Sequence Stratigraphy

Spec. Pub. Type: Memoir

Pub. Year: 1984

Author(s): L. L. Sloss

Abstract:

Cratonic Previous HitunconformitiesNext Hit represent (1) coincidence of surfaces of sedimentary accumulation with depositional base level, or elevation of depositional surfaces above erosional base level, and (2) renewed deposition covering surfaces of nondeposition or erosion. The chronostratigraphic record of Previous HitunconformitiesNext Hit is best displayed on Wheeler diagrams on which geographic distances are plotted against chronostratigraphic intervals or absolute time. Assessing the lithostratigraphic significance of Previous HitunconformitiesNext Hit requires reconstruction of the pre-unconformity stratigraphy and estimation of the thickness (or volume) of the strata eroded and of their lithologic character.

Interregional cratonic Previous HitunconformitiesNext Hit fall into two major types: (1) those marked by subequal values of nondeposition and erosion, commonly involving 5 to 30 m.y. and the stripping of as much as 1 km (.6 mi) over very broad areas (for example, the sub-Kaskaskia unconformity-Early Devonian to Early Carboniferous); and, (2) Previous HitunconformitiesNext Hit characterized by short-term nondeposition (< 5 m.y.) and extremes of erosional vacuity (for example, the sub-Absaroka surface-Late Carboniferous).

Conventional wisdom suggests that episodes of cratonic nondeposition and erosion should equate with accelerated detrital deposition at continental margins and with perturbations of marine chemistry. Evidence is accumulating to indicate a degree of concomitance between cratonic events and oceanic geochemistry but no complementary pattern is clear in terms of slope/rise depositional rates. Indeed, certain major Previous HitunconformitiesTop identified on continental slopes appear to have equivalents on cratons. These and related questions demand increased communication between land-based and seagoing stratigraphic and tectonic specialists.

Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Watermarked PDF Document: $14
Open PDF Document: $24