地质调查与研究
地質調查與研究
지질조사여연구
GEOLOGICAL SURVEY AND RESEARCH
2014年
2期
136-143
,共8页
何国建%金巍%胡为正%卢国安%曾佐勋
何國建%金巍%鬍為正%盧國安%曾佐勛
하국건%금외%호위정%로국안%증좌훈
运动学涡度%测量方法%极摩尔圆法%雁林寺韧性剪切带
運動學渦度%測量方法%極摩爾圓法%雁林寺韌性剪切帶
운동학와도%측량방법%겁마이원법%안림사인성전절대
kinematic vorticity%method of measurement%polar Mohr circle%Yanlinsi ductile shear zone
自然界中的剪切带通常是由简单剪切(simple shear)和纯剪切(pure shear)叠加的一般剪切带(general shear)。运动学涡度(kinematic vorticity)的引入提供了一个定量表示两种剪切成分的工具。通过测量剪切带的运动学涡度,可以清楚的了解一般剪切带中究竟是简单剪切还是纯剪切占优势。本文将运动学涡度的基本理论和极摩尔圆法对雁林寺金矿所在的湘东雁林寺韧性剪切带中所表现的运动学涡度进行测量,得出该韧性剪切带的Wk值为0.6,指示其变形以纯剪切为主,且简单剪切作用应变速率比纯剪切作用的应变速率慢。本文从微观运动学层面揭示了湘东雁林寺韧性剪切带对于雁林寺金矿的形成具有重要的意义。
自然界中的剪切帶通常是由簡單剪切(simple shear)和純剪切(pure shear)疊加的一般剪切帶(general shear)。運動學渦度(kinematic vorticity)的引入提供瞭一箇定量錶示兩種剪切成分的工具。通過測量剪切帶的運動學渦度,可以清楚的瞭解一般剪切帶中究竟是簡單剪切還是純剪切佔優勢。本文將運動學渦度的基本理論和極摩爾圓法對雁林寺金礦所在的湘東雁林寺韌性剪切帶中所錶現的運動學渦度進行測量,得齣該韌性剪切帶的Wk值為0.6,指示其變形以純剪切為主,且簡單剪切作用應變速率比純剪切作用的應變速率慢。本文從微觀運動學層麵揭示瞭湘東雁林寺韌性剪切帶對于雁林寺金礦的形成具有重要的意義。
자연계중적전절대통상시유간단전절(simple shear)화순전절(pure shear)첩가적일반전절대(general shear)。운동학와도(kinematic vorticity)적인입제공료일개정량표시량충전절성분적공구。통과측량전절대적운동학와도,가이청초적료해일반전절대중구경시간단전절환시순전절점우세。본문장운동학와도적기본이론화겁마이원법대안림사금광소재적상동안림사인성전절대중소표현적운동학와도진행측량,득출해인성전절대적Wk치위0.6,지시기변형이순전절위주,차간단전절작용응변속솔비순전절작용적응변속솔만。본문종미관운동학층면게시료상동안림사인성전절대대우안림사금광적형성구유중요적의의。
Abstact:In nature , shear can be decomposed into pure shear component and simple shear component. Kinematic vorticity can quantitatively evaluate the component of simple shear and pure shear. By measuring the kinematic vorticity number (Wk), we can clearly understand that in the general shear zone, the simple shear or pure-shear is dominant shear force. This paper introduces basic theory and several measuring methods of kinematic vorticity number, and measres Wk of Yanlinsi ductile shear zone by polar Mohr constructions. It shows that the Wk is near-ly 0.6, which indicates that the shear zone is exactly exist and dominated by pure shear, and straining rate of sim-ple shear is slower than pure shear. It reveals the important significance of the Yanlinsi ductile shear zone for the Yanlinsi gold deposit formation, in microkinematics.