Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系德阶界线层型,山西德冀家沟剖面记录了12个正极性段11个负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建段的理由，介绍了名称来源、层型剖面、地层的延伸，讨论了地质时代。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系保德阶界线,山西保德冀家沟剖面记录12极性段与11负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐建段的理由，介绍名称来、剖面、地的延伸与对比，讨论地质时代。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系德阶界线层型,西德冀家沟剖面记录了12个正极性段与11个负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建段的理由，介绍了名称来源、层型剖面、地层的延伸与，论了地质时代。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系保德阶界线层型,山西保德冀家沟剖面记录了12个正极性段与11个负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建段的理由，介绍了名称来源、层型剖面、地层的延伸与对比，讨论了地质时代。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系德界线层型,山西德冀家沟剖面记录了12个正极性段与11个负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建段的理由，介绍了名称来源、层型剖面、地层的延伸与对比，讨论了地质。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系保德线层型,山西保德冀家沟剖面记录了12个正极性段与11个负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建段的理由，介绍了名称来源、层型剖面、地层的延伸与对比，讨论了地。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系保德阶界线型,山西保德冀家沟剖面记录了12个正极性段与11个负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建段的理由，介绍了名称来源、型剖面、地的延伸与对比，讨论了地质时代。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系保德阶界线层型,山西保德冀家沟剖面记录了12个正与11个负。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建，介绍了名称来源、层型剖面、地层延伸与对比，讨论了地质时代。

Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.

古地磁测量表明,中国新近系保德阶界线层,山西保德冀家沟剖面记录了12个正极性段与11个负极性段。

This paper indicates the reasons of establish member and introduces its origin and stratotype section, as well as its extend and correlation.At last, its geological age is discussed.

文中阐了建段的理由，介绍了名称来、层剖面、地层的延伸与对比，讨论了地质时代。