摘要
韧性变形岩石中动态重结晶石英颗粒边界形态具有自相似性 ,表现出分形特征。动态重结晶石英颗粒边界的分形维数随温度的升高而减小 ,随应变速率的增加而增大 ,可作为韧性变形温度及应变速率的标度计。适合重结晶石英边界分维值的计算方法有封闭折线法和面积周长法。鲁西青邑韧性剪切带中糜棱岩动态重结晶石英颗粒边界具有自相似性 ,分维值为 1.2 2 8~ 1.32 6 ,初步估算出古应变速率为 10 - 7.6~ 10 - 8.7s- 1,属绿片岩相。
Grain shapes of dynamically recrystallized quartz in ductile deformed rocks, characterized by fractal dimension, are statistically self_similar. The fractal dimensions of dynamically recrystallized quartz grains, decreasing with deformation temperature and rising with strain rate, can be an indictor for the deformation condition. Two methods of polygon and area_perimeter are applicable to calculate the fractal dimension of dynamically recrystallized quartz grains. Grain shapes of dynamically recrystallized quartz in mylonites within Qingyi ductile shear zone show statistical self_similarity, in which numbers of fractal dimension are from 1.228 to 1.326 and paleo_strain rates vary from 10 -7.6 to 10 -8.7 s -1 . Qingyi ductile shear zone experienced deformation under the conditions of green_schist facies and medium strain_rate.
出处
《岩石矿物学杂志》
CAS
CSCD
北大核心
2001年第1期36-41,共6页
Acta Petrologica et Mineralogica
基金
国家自然科学基金项目!"亚干变质核杂岩形成机制与构造热演化"(编号 :49872 0 72 )
原地矿部 1:5万田黄
土旺幅区域地质调查项目资
关键词
动态重结晶石英颗粒
分形
变形温度
应变速率
韧性剪切带
grain shapes of dynamically recrystallized quartz
fractal dimension
deformation temperature
strain rate
Qingyi ductile shear zone