--> ABSTRACT: Genetic Stratigraphic Sequence Analysis in Terrestrial Aggrading Basin: Sequence Stratigraphy of Narrabeen Group, Sydney Basin, Australia, by Shawn A. Reynolds and William E. Galloway; #91022 (1989)
[First Hit]

Datapages, Inc.Print this page

Genetic Stratigraphic Previous HitSequenceNext Hit Analysis in Terrestrial Aggrading Basin: Previous HitSequenceNext Hit Stratigraphy of Narrabeen Group, Sydney Basin, Australia

Shawn A. Reynolds, William E. Galloway

Development of event/Previous HitsequenceNext Hit stratigraphy concepts over the past 15 years has been one of the most significant contributions to systematic stratigraphic analyses of sedimentary basins. Most of these approaches, however, have not been applied to terrestrial aggradational settings but rather were developed in marginal basin settings where progradational and transgressive units are important components of the Previous HitsequenceNext Hit framework. The principal objective of Previous HitsequenceNext Hit definition is the Previous HitidentificationNext Hit of genetic stratigraphic units that share a common paleogeographic, climatic, and tectonic origin. Thus, the basic premise of Previous HitsequenceNext Hit stratigraphy should be useful in the delineation of the Previous HitdepositionalNext Hit framework for any basin.

Criteria were devised to identify three genetic stratigraphic sequences within the Triassic Narrabeen Group of the Sydney basin, an aggrading basin with a terrestrial fill. Individual sequences were chosen to emphasize significant changes in tectonic and climatic conditions, as reflected in the distinguishing characteristics of Previous HitdepositionalNext Hit style, sediment composition, and paleodrainage trends.

The Munmorah Previous HitsequenceNext Hit is characterized by lithic sandstone deposits of an extensive alluvial plain sourced by the New England foldbelt to the northeast. The overlying Bulgo Previous HitsequenceNext Hit is distinguished by changes in sediment transport direction, lithology, and Previous HitdepositionalNext Hit style. The western Lachlan foldbelt emerged as a source of a quartz-rich braid-plain system. The Bald Hill Previous HitsequenceNext Hit lies above the Bulgo and consists of sandstones and kaolinitic claystones that were deposited in extensive, highly oxidized alluvial plains that were dissected by numerous small streams. The distinctive mineralogy and Previous HitdepositionalTop style of the Bald Hill deposits suggest climatic and tectonic changes in the Lachlan foldbelt source area.

AAPG Search and Discovery Article #91022©1989 AAPG Annual Convention, April 23-26, 1989, San Antonio, Texas.