2010•Acta Geologica Sinica - English EditionRequires access

Late Carboniferous‐Early Permian Sequence Stratigraphy and Depositional Evolution in the Northeast Ordos Basin, North China

YANG Minghui, Liu Chi-yang, Lan Chao-li, Le Liu, LI Xin, ZHANG Kunshan

Open publisher page 15 citations

Abstract

Abstract: Sequence stratigraphical analysis was applied to the Upper Carboniferous‐Lower Permian sedimentary succession of the northeastern Ordos Basin, north China based on data acquired from ten entire logging curves and eight outcrops. The facies framework of the lithostratigraphical unit, the Taiyuan Formation comprises seven facies in two facies associations, varying from fluvio‐delta to shelf‐barrier islands. The facies are presented within a chronostratigraphical framework, linked by systems tract, which in turn are limited by flooding surfaces and sequence boundaries. Six third‐order depositional sequences are recognised, bounded by six type 2 unconformities. An upwards‐shallowing epicontinental sea sedimentary model is created, which consists of a sandstone, coal seam and carbonate succession.

About this research paper

What this paper is about

Abstract: Sequence stratigraphical analysis was applied to the Upper Carboniferous‐Lower Permian sedimentary succession of the northeastern Ordos Basin, north China based on data acquired from ten entire logging curves and eight outcrops. The facies framework of the lithostratigraphical unit, the Taiyuan Formation comprises seven facies in two facies associations, varying from fluvio‐delta to shelf‐barrier islands. The facies are presented within a chronostratigraphical framework, linked by systems tract, which in turn are limited by flooding surfaces and sequence boundaries. Six third‐order depositional sequences are recognised, bounded by six type 2 unconformities. An upwards‐shallowing epicontinental sea sedimentary model is created, which consists of a sandstone, coal seam and carbonate succession.

Why it matters

OpenAlex reports 15 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

Abstract: Sequence stratigraphical analysis was applied to the Upper Carboniferous‐Lower Permian sedimentary succession of the northeastern Ordos Basin, north China based on data acquired from ten entire logging curves and eight outcrops. The facies framework of the lithostratigraphical unit, the Taiyuan Formation comprises seven facies in two facies associations, varying from fluvio‐delta to shelf‐barrier islands. The facies are presented within a chronostratigraphical framework, linked by systems tract, which in turn are limited by flooding surfaces and sequence boundaries. Six third‐order depositional sequences are recognised, bounded by six type 2 unconformities. An upwards‐shallowing epicontinental sea sedimentary model is created, which consists of a sandstone, coal seam and carbonate succession.

Key concepts: Facies, Geology, Carboniferous, Sedimentary depositional environment, Paleontology, Permian, Outcrop, Unconformity

Related papers

Back to paper searchBrowse research topicsOriginal source
Late Carboniferous‐Early Permian Sequence Stratigraphy and Depositional Evolution in the Northeast Ordos Basin, North China — Research Paper | ScholarLens