摘要
利用ＭＤＤ模式得到的连续冷却曲线，可以定量地描述地质体的冷却（隆升）过程；采用我国７个不同地区中３８个钾长石ＭＤＤ模式研究结果证明，快速冷却事件存在的普遍性，不同的快速冷却速度可能反映了不同的构造事件；突变因子（δｖｉ）可以定量地描述地质体非平稳运动以及突变程度。
The continuous cooling curve obtained with the MDD model can use to quantitatively describe the cooling or uplifting process of a geologic body. The MDD model studies of 38K-feldspar samples from seven areas in China whow that rapid-cooling events or abrupt change events exist universally and that the cooling rates vary in different tectonic events. The abrupt change factor can use to quantitatively describe the nonstationary nature or abrupt changes in geologic events,and meanwhile makes the correlation of nonstationary geologic events possible.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
1996年第3期277-279,共3页
Earth Science-Journal of China University of Geosciences
基金
国家自然科学基金
地震科学联合基金
