新构造运动对贵州锥状喀斯特发育的影响

Development of Cone Karst in Response to Neotectonism in Guizhou

贵州属我国喀斯特最发育的高原区。在复杂的构造背景和有利的热带一亚热带气候条件下，发育了一套典型的喀斯特地貌，其中由峰丛洼地、峰林洼地和峰林溶原三大成因系列构成的锥状喀斯特最显著、最壮观。与其它地区相比，贵州的锥状喀斯特在第三纪末期以来受到新构造运动的强烈控制。在地貌结构和发育演化上表现出五大特征。

Guizhou Province contains the most karstic plateau of China.A suit of karst landforms are well develoment in the complex structure background and the favarable tropical-subtropical environment,of which cone karst with 3 morphogenetic systems of peak-cluster-depression, peak-forest-depression and peak-forest-plain is the most notable and spectacular. Contrasted with other areas, the cone karst in Guizhou has intensively controlled by the neotectonism since the Late Tertiary, which gives rise to 5 characteristics on the karst geomorphological texture and development.