1976Journal of the Japan Society of Engineering GeologyOpen access

The Characteristic Altered Biotite in the Weathered Tottori Granite and Their Significances to Applied Geology

Kiyoshi Miura

Open full text 1 citations

Abstract

The characteristic altered biotites are observed in the weathered granite at eastern part of Tottori prefecture, Japan, From the mineral assemblage, they are classified into following types:(1) Kaolinite+interstratified Chlorite-Vermiculite(2) Kaolinite+Vermiculite + interstratified Chlorite-Vermiculite(3) Kaolinite+Chlorite+Vermiculite+ interstratified Chlorite-Vermiculite.The hydroxy-aluminium interlayer may form in the all of discrete vermiculite and interstratified vermiculite.They are different from the mineral assemblages of weathered biotite.Judging from the mode of occurrence, they were formed from the altered chloritic biotite under the weathering condition.They gives a evidence of hydrothermal alteration before weathering of the parent rock.

Open-access reader

About this research paper

What this paper is about

The characteristic altered biotites are observed in the weathered granite at eastern part of Tottori prefecture, Japan, From the mineral assemblage, they are classified into following types:(1) Kaolinite+interstratified Chlorite-Vermiculite(2) Kaolinite+Vermiculite + interstratified Chlorite-Vermiculite(3) Kaolinite+Chlorite+Vermiculite+ interstratified Chlorite-Vermiculite.The hydroxy-aluminium interlayer may form in the all of discrete vermiculite and interstratified vermiculite.They are different from the mineral assemblages of weathered biotite.Judging from the mode of occurrence, they were formed from the altered chloritic biotite under the weathering condition.They gives a evidence of hydrothermal alteration before weathering of the parent rock.

Why it matters

OpenAlex reports 1 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

The characteristic altered biotites are observed in the weathered granite at eastern part of Tottori prefecture, Japan, From the mineral assemblage, they are classified into following types:(1) Kaolinite+interstratified Chlorite-Vermiculite(2) Kaolinite+Vermiculite + interstratified Chlorite-Vermiculite(3) Kaolinite+Chlorite+Vermiculite+ interstratified Chlorite-Vermiculite.The hydroxy-aluminium interlayer may form in the all of discrete vermiculite and interstratified vermiculite.They are different from the mineral assemblages of weathered biotite.Judging from the mode of occurrence, they were formed from the altered chloritic biotite under the weathering condition.They gives a evidence of hydrothermal alteration before weathering of the parent rock.

Key concepts: Vermiculite, Biotite, Chlorite, Kaolinite, Weathering, Geology, Geochemistry, Mineral

Related papers

Back to paper searchBrowse research topicsOriginal source
The Characteristic Altered Biotite in the Weathered Tottori Granite and Their Significances to Applied Geology — Research Paper | ScholarLens