2001•Unpublished venueRequires access

The Sedimentary Characteristics of the Tempestites in Zhenlongchang Formation, Zhaertaishan Group in Guyang Area,Inner Mongolia

Pan Yongsheng

Abstract

Based on the theory of the sequence stratigraphy, the characteristics of the m-grade cycle sequence and the sequence of the sedimentary facies in the Zhenlongchang Formation, Zhaertaishan Groupe in Guyang area, the sedimentary characteristics of the tempestites in the Zhenlongchang formation were expounded. The cause and tectornic meaning of the tempestites also be discussed in the paper.

About this research paper

What this paper is about

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

Key concepts: Facies, Sequence (biology), Sedimentary rock, Group (periodic table), Paleontology, Inner mongolia, Geology, Sequence stratigraphy