ScholarLens Back to search
2001•Coal Geology of ChinaRequires access

Sequence Stratigraphic Features and Coal－accumulating Laws of Permian Basin in Southern China

Gong Shao

Open publisher page 0 citations

Abstract

Permian System of Southern China formed in the epicontinental basin which there are unhomogeneous basal structure. On the Southern China plate, the permian structural frame and sedimentation and coal－accumulation, were controlled by evolution of Tethys sea. Permian system in Southern China may be divided into six Ⅲgrade sequences. On the sequence stratigraphic border in different structural area, there are particular distinguish mark. The sequence strata has different model, primarily showing that lower system territory (LST) has different depositional features and in the different system territory there are different coal－accumulating laws.

About this research paper

What this paper is about

Permian System of Southern China formed in the epicontinental basin which there are unhomogeneous basal structure. On the Southern China plate, the permian structural frame and sedimentation and coal－accumulation, were controlled by evolution of Tethys sea. Permian system in Southern China may be divided into six Ⅲgrade sequences. On the sequence stratigraphic border in different structural area, there are particular distinguish mark. The sequence strata has different model, primarily showing that lower system territory (LST) has different depositional features and in the different system territory there are different coal－accumulating laws.

Why it matters

A significance statement is not available in the OpenAlex record.

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

Permian System of Southern China formed in the epicontinental basin which there are unhomogeneous basal structure. On the Southern China plate, the permian structural frame and sedimentation and coal－accumulation, were controlled by evolution of Tethys sea. Permian system in Southern China may be divided into six Ⅲgrade sequences. On the sequence stratigraphic border in different structural area, there are particular distinguish mark. The sequence strata has different model, primarily showing that lower system territory (LST) has different depositional features and in the different system territory there are different coal－accumulating laws.

Key concepts: Permian, Geology, Paleontology, Sedimentary depositional environment, Sequence (biology), Structural basin, Southern china, Coal

Related papers

Related paper 1Related paper 2Related paper 3
Back to paper searchBrowse research topicsOriginal source
Sequence Stratigraphic Features and Coal－accumulating Laws of Permian Basin in Southern China — Research Paper | ScholarLens