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多硅白云母压力计在退变质作用中的稳定性探讨
引用本文:王勇生,朱光.多硅白云母压力计在退变质作用中的稳定性探讨[J].矿物岩石,2004,24(4):20-27.
作者姓名:王勇生  朱光
作者单位:合肥工业大学资源与环境工程学院,安徽,合肥,230009
基金项目:国家自然科学基金资助项目(编号:40272094)
摘    要:探讨多硅白云母地质压力计在低温退变质过程中的稳定性,在对大别山东缘和苏鲁造山带西缘郯庐左旋走滑韧性剪切带糜棱岩中的多硅白云母残斑由中心向两侧边缘进行电子探针分析后发现:由中心向两侧边缘Si减少,Al增加,Fe,Mg略有降低,部分样品中K,Na有不同程度的增加.而Ti则显示不活动富集。这是由于退变质过程中流体的活动常会改变残斑白云母的成分.并且在流体活动过程相对短暂的情况下,使残斑白云母的成分不能发生充分变化.最终会导致白云母不同部位具有不同的成分。因而,经历了富流体活动的退变质作用后,岩石中的多硅白云母残斑已不能完全保存其形成时的压力信息。

关 键 词:多硅白云母  退变质作用  流体活动  苏鲁造山带  左旋走滑  韧性剪切带  糜棱岩  心向  过程  情况
文章编号:1001-6872(2004)04-0020-08
修稿时间:2004年5月20日

DISCUSSION ON THE STABILITY OF PHENGITE GEOBAROMETRY IN RETROGRADE METAMORPHISM
WANG Yong-sheng,ZHU Guang College of Resource and Environmental Engineering,Hefei University of Technology,Hefei,China.DISCUSSION ON THE STABILITY OF PHENGITE GEOBAROMETRY IN RETROGRADE METAMORPHISM[J].Journal of Mineralogy and Petrology,2004,24(4):20-27.
Authors:WANG Yong-sheng  ZHU Guang College of Resource and Environmental Engineering  Hefei University of Technology  Hefei  China
Institution:WANG Yong-sheng,ZHU Guang College of Resource and Environmental Engineering,Hefei University of Technology,Hefei230009,China
Abstract:For the purpose of studying the stability of phengites geobarometry in retrograde metamorphism.The porphyroclast muscovites in Tanlu ductile shear zone,eastern Dabie Mountains and western Sulu Mountains were analyzed by electron microprobe from the centre to the rim on the grains. The result showed that from center of porphyroclast muscovites to rim,Si,Fe,Mg decreases,Al,K,Na increases,and Ti is enriched,which were caused by the composition change of muscovite in retrograde metamorphism.When the process of metamorphism is short,composition of porphyroclast muscovite can only partly be changed,resulting in the variation of composition in the different domains of porphyroclasts.Therefore,it was difficult for the porphyroclast muscovite to reserve the information of paleo-pressure after the retrograde metamorphism.
Keywords:geobarometry of phengites  retrograde metamorphism  fluid
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