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滇西褶皱带

滇西褶皱带,为云南地区的横断山脉,属于三江褶皱系向南延伸部分,由怒江澜沧江金沙江三大水系与高黎贡山无量山哀牢山等相间紧密排列而成[1]

特点

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滇西褶皱带又可分成南北两段,北部为高山深谷,南部是带状山脉的中山宽谷。山地从海拔3000米以上下降到海拔1300米,谷地从海拔1000米下降到海拔500多米。其山地土壤的水平、垂直带谱都很明显,自高至低,自北而南依次为棕壤、黄棕壤、山地红壤、赤红壤、砖红壤[2]。大农业生产结构为林业一旱谷一茶叶甘蔗粳稻橡胶热带作物、籼稻[3]

参考

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  1. ^ 云南省地方志编纂委员会. 云南省志 卷1 地理志. 昆明:云南人民出版社. 1998.01: 188–189. ISBN 7-222-02247-3. 
  2. ^ 云南省土壤肥料工作站,云南省土壤普查办公室编. 云南土壤. 昆明:云南科学技术出版社. 1996.12: 162. ISBN 7-5416-0534-4. 
  3. ^ 高昆谊,朱慧贤编著. 云南生物地理 Yunnan biological geography. 昆明:云南科学技术出版社. 2008.04: 45. ISBN 978-7-5416-2810-8. 
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滇西褶皱带
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