摘要
笔者在简略论述反映古气候、古环境的多种代用指标的基础上,讨论其在揭示地质灾害信息方面的意义,并分析从中提取地质灾害信息的方法和思路。认为在沉积物粒度判别基础上,沉积物表现出的较低δ18O值,较低δ13C值和较低碳酸盐含量以及较高的有机质含量特征可能指示了地质灾害方面的信息。
<Abstrcat> The occurrence of geological disasters is interpreted to be closely related to palaeoclimatic and palaeoenvironmental changes. In this paper, the authors present a new analysis of palaeoclimatic and palaeoenvironmental indicators and their information on geological disasters as revealed by lake records. For a given geological environment, when the precipitates reach their upper limits, some geological disasters such as landslides, collapses and clastic flows may be triggered. In other words they are often initiated in the areas where the amount and strength of the precipitates are great enough to cause the cyclic systems of ground water to be saturated. The information on geological disasters may be detected from grain sizes, lower δ18O and lower δ13C values, lower carbonate contents, and higher organic matter contents of the sediments preserved in the lacustrine environments.
出处
《沉积与特提斯地质》
CAS
CSCD
2002年第1期40-45,共6页
Sedimentary Geology and Tethyan Geology
关键词
古气候
古环境
多种代用指标
地质灾害信息
湖泊记录
沉积物
palaeoclimate
palaeoenvironment
multiindicator
information on geological disasters
lake record
