Luo Chengde. A PRELIMINARY STUDY ON QUATERNARY GLACIAL LANDFORMS IN MT.MA'AN[J]. Chinese Geographical Science, 1998, 8(1): 91-95.
Citation: Luo Chengde. A PRELIMINARY STUDY ON QUATERNARY GLACIAL LANDFORMS IN MT.MA'AN[J]. Chinese Geographical Science, 1998, 8(1): 91-95.

A PRELIMINARY STUDY ON QUATERNARY GLACIAL LANDFORMS IN MT.MA'AN

  • Publish Date: 1998-03-20
  • Mt.Ma'an (4288 m) is the highest mountain in the southwest edge of Sichuan Basin. It is situated to the south of the Dadu River. The geographic coordinates are: 28°58′N, 102°55′E. There are six peaks over 4000 m in elevation. Many quaternary glacial landforms in this mountain have been discovered. It's a typical example of fossil glacial landform in the east China. Its glacial stages are the last glaciation (Q33) and the neoglaciation (Q43). Mt. Ma'an and Mt. Luoji (4359 m) are similar in the fossil glacial landforms, but there are still some differences between them. For example, the ratio between the direct difference and the minus difference is different.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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A PRELIMINARY STUDY ON QUATERNARY GLACIAL LANDFORMS IN MT.MA'AN

Abstract: Mt.Ma'an (4288 m) is the highest mountain in the southwest edge of Sichuan Basin. It is situated to the south of the Dadu River. The geographic coordinates are: 28°58′N, 102°55′E. There are six peaks over 4000 m in elevation. Many quaternary glacial landforms in this mountain have been discovered. It's a typical example of fossil glacial landform in the east China. Its glacial stages are the last glaciation (Q33) and the neoglaciation (Q43). Mt. Ma'an and Mt. Luoji (4359 m) are similar in the fossil glacial landforms, but there are still some differences between them. For example, the ratio between the direct difference and the minus difference is different.

Luo Chengde. A PRELIMINARY STUDY ON QUATERNARY GLACIAL LANDFORMS IN MT.MA'AN[J]. Chinese Geographical Science, 1998, 8(1): 91-95.
Citation: Luo Chengde. A PRELIMINARY STUDY ON QUATERNARY GLACIAL LANDFORMS IN MT.MA'AN[J]. Chinese Geographical Science, 1998, 8(1): 91-95.

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