2008Zhongguo dizhiRequires access

Paleogene sequence stratigraphic framework and model in the Huanghua depression

Miao Shun-de

Open publisher page 2 citations

Abstract

Sequence stratigraphy has developed for over 40 years,but it was applied to continental basins in China only ten years ago.The integrated sequence stratigraphic framework for the entire stratigraphic succession has not been established in many basins such as the Huanghua depression.Based on previous research,proceeding from the principle of sequence division and through studies of the characteristics and identification indicators of different orders of sequences and system tract boundaries,the paper proposes a scheme of sequence division in the Huangliua depression and divides the Paleogene strata into 1 first-order sequence,3 second-order sequences and 11 third-order sequences.Based on studies of typical sections,the authors propose that the abrupt change of the depositional slopes,resulting from the structural slope break zone or flexure slope break zone,has an important effect on the accommodation and sedimentation in the basin and that the structural slope break zone and flexure slope break zone control the development of the sequences and lowstand sand bodies.Two models for the relation between slope break zones and sequences have been constructed,and it is pointed out that the areas below the slope break zones are favorable zones for the deposition of lowstand sand bodies.

About this research paper

What this paper is about

Sequence stratigraphy has developed for over 40 years,but it was applied to continental basins in China only ten years ago.The integrated sequence stratigraphic framework for the entire stratigraphic succession has not been established in many basins such as the Huanghua depression.Based on previous research,proceeding from the principle of sequence division and through studies of the characteristics and identification indicators of different orders of sequences and system tract boundaries,the paper proposes a scheme of sequence division in the Huangliua depression and divides the Paleogene strata into 1 first-order sequence,3 second-order sequences and 11 third-order sequences.Based on studies of typical sections,the authors propose that the abrupt change of the depositional slopes,resulting from the structural slope break zone or flexure slope break zone,has an important effect on the accommodation and sedimentation in the basin and that the structural slope break zone and flexure slope break zone control the development of the sequences and lowstand sand bodies.Two models for the relation between slope break zones and sequences have been constructed,and it is pointed out that the areas below the slope break zones are favorable zones for the deposition of lowstand sand bodies.

Why it matters

OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Sequence stratigraphy has developed for over 40 years,but it was applied to continental basins in China only ten years ago.The integrated sequence stratigraphic framework for the entire stratigraphic succession has not been established in many basins such as the Huanghua depression.Based on previous research,proceeding from the principle of sequence division and through studies of the characteristics and identification indicators of different orders of sequences and system tract boundaries,the paper proposes a scheme of sequence division in the Huangliua depression and divides the Paleogene strata into 1 first-order sequence,3 second-order sequences and 11 third-order sequences.Based on studies of typical sections,the authors propose that the abrupt change of the depositional slopes,resulting from the structural slope break zone or flexure slope break zone,has an important effect on the accommodation and sedimentation in the basin and that the structural slope break zone and flexure slope break zone control the development of the sequences and lowstand sand bodies.Two models for the relation between slope break zones and sequences have been constructed,and it is pointed out that the areas below the slope break zones are favorable zones for the deposition of lowstand sand bodies.

Key concepts: Geology, Paleogene, Sequence stratigraphy, Paleontology, Sequence (biology), Sedimentary depositional environment, Structural basin, Geomorphology

Related papers

Back to paper searchBrowse research topicsOriginal source
Paleogene sequence stratigraphic framework and model in the Huanghua depression — Research Paper | ScholarLens