Intrinsic Driving Mechanism of Land Rocky Desertification in Karst Regions of Guizhou Province
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Intrinsic Driving Mechanism of Land Rocky Desertification in Karst Regions of Guizhou Province
Bulletin of Soiland Water ConservationVol. 20, Issue 4, Pages: 1-5(2001)
作者机构:
1. 中国科学院地球化学研究所环境地球化学国家重点实验室,贵州,贵阳,550002
2. 贵州省区域地质调查研究院,贵州,贵阳,500005
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Published:2001
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ZHANG Dian-fa, WANG Shi-jie, ZHOU De-quan, et al. Intrinsic Driving Mechanism of Land Rocky Desertification in Karst Regions of Guizhou Province[J]. Bulletin of Soiland Water Conservation, 2001, 20(4): 1-5.
DOI:
ZHANG Dian-fa, WANG Shi-jie, ZHOU De-quan, et al. Intrinsic Driving Mechanism of Land Rocky Desertification in Karst Regions of Guizhou Province[J]. Bulletin of Soiland Water Conservation, 2001, 20(4): 1-5.DOI:
Intrinsic Driving Mechanism of Land Rocky Desertification in Karst Regions of Guizhou Province
The given eco-geoenvironmental setting has evident control action on land rocky desertification
rocky deserted land mostly distributes in the river-valley regions where karst very developed and tectogenesis was violent in Guizhou province. Warm and humid monsoon climate provides corrosion condition for rocky desertification;Tectogenesis sculptured steep and fragmentized karst land feature with sharp topographic relief
which offer rocky desertification a latent energy;Paleoenvironment supplied rich carbonate for rocky desertification
four carbonate sedimentary formations had developed from late Sinian to late Trias in Guizhou province
pure carbonate rock constitute the substantial foundation of land rocky desertification.