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首页> 外文期刊>Chinese Geographical Science >CHARACTERISTICS, ORIGIN AND EVOLUTION AGES OF AEOLIAN SAND IN THE SAHELIAN REGION OF MALI
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CHARACTERISTICS, ORIGIN AND EVOLUTION AGES OF AEOLIAN SAND IN THE SAHELIAN REGION OF MALI

机译:马里萨赫勒地区风沙的特征,成因和演化时代

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摘要

The Sahelian region of Mali is one of the areas seriously affected by sandy desertitication in the world. Widely distributed aeolian sand lays a material basis for the development of sandy desertification. Aeolian sand in the Region is dominated by fine sand, followed by very fine sand. Sand materials contained in various sand dunes are differ- Ent in grain size to a certain extent and the mineral compositions of dune sand are dominated by stable and extreme sta- ble minerals, with high stability and maturity. Aeolian sand in the region mainly comes from the reactivation of ancient Sand dunes, the transportation of recent running water and the sand supply of dry lakes and arroyos. Since the Pliocene This region has experienced four major evolution periods of aelian sand, namely from the Pliocene to the early Quarter- Nary, last glacial period, the Holocene and present.
机译:马里的萨赫勒地区是世界上受沙质沙漠化严重影响的地区之一。广泛分布的风沙为沙质沙漠化的发展奠定了物质基础。该地区的风沙以细砂为主,其次是极细砂。各种沙丘中包含的沙料在一定程度上具有不同的粒径,沙丘沙的矿物成分以稳定和成熟度高的稳定和极稳定的矿物为主。该地区的风沙主要来自古沙丘的复活,近期自来水的运输以及干旱湖泊和阿罗约斯的供砂。自上新世以来,该地区经历了埃里埃砂的四个主要演化时期,即从上新世到纳纳尔季初,最后一个冰川时期,全新世和现在。

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