1994•Chinese Science BulletinRequires access

Evolution of Authigenic Glauconite in Early Diagenesis

陈丽蓉

Open publisher page 0 citations

Abstract

According to the data of the mineral assemblages, the sediment layers with authigenic glauconite were found in the X_1 core collected from the northeast of the Beibu Gulf. Pliocene sediment layer containing a lot of foraminifera shows a shallow sea facies. Its thickness is larger than 30 m and is located at the depth below 59 m of the core.

About this research paper

What this paper is about

According to the data of the mineral assemblages, the sediment layers with authigenic glauconite were found in the X_1 core collected from the northeast of the Beibu Gulf. Pliocene sediment layer containing a lot of foraminifera shows a shallow sea facies. Its thickness is larger than 30 m and is located at the depth below 59 m of the core.

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

According to the data of the mineral assemblages, the sediment layers with authigenic glauconite were found in the X_1 core collected from the northeast of the Beibu Gulf. Pliocene sediment layer containing a lot of foraminifera shows a shallow sea facies. Its thickness is larger than 30 m and is located at the depth below 59 m of the core.

Key concepts: Authigenic, Glauconite, Diagenesis, Geology, Foraminifera, Facies, Geochemistry, Sediment

Related papers

Back to paper searchBrowse research topicsOriginal source
Evolution of Authigenic Glauconite in Early Diagenesis — Research Paper | ScholarLens