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辉长岩部分熔融实验及地质学意义

AN EXPERIMENTAL STUDY ON PARTIAL MELTING OF GABBRO AND ITS GEOLOGICAL IMPLICATION

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【作者】 桑祖南周永胜何昌荣金振民

【Author】 Sang Zunan 1 Zhou Yongsheng 2 He Changrong 2 Jin Zhenmin 3 (1. Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou\ 510640; 2. Institute of Geology, China Seismological Bureau, Beijing 100029; 3.China University of Geos

【机构】 中国科学院广州地球化学研究所中国地震局地质研究所构造物理开放实验室中国地质大学地球科学学院 广州510640北京100029武汉430074

【摘要】 利用高温高压多功能三轴实验装置对四川省攀枝花辉长岩进行了动态和静态部分熔融实验研究 ,实验的围压为 45 0~ 80 0MPa,温度区间为 90 0~ 1 2 0 0℃。实验表明 ,差应力对辉长岩动态部分熔融程度有一定影响 ,初始熔体主要分布在不同矿物的颗粒边界和三联点 ,变形影响熔体分布 ,变形与辉长岩韵律层具有一定成因联系。本文为熔体对岩石流变学行为影响提供了实验约束依据

【Abstract】 This paper presented the results of a preliminary experimental study on partial melting of fine and medium grained gabbros from Panzhihua, Sichuan Province. The experiments were conducted in conditions of confining pressure of 450~800 MPa and temperature of 800~1 200 ℃. The following knowledges could be concluded from the experiment: 1)the amount of partial melting in dynamic state during deformation with diffrerential stress being more than that in static state with no differential stress; 2)the initial melt distributing on different mineral grain boundaries and emerging from the triple junctions; and 3)the melt distribution being influenced by deformation. Based on these, it was inferred that the gabbro rhythmic layering might be related to structural deformation. This study provided experimental constraints of melt effect on rheology behavior of gabbro.

【基金】 国家自然科学基金项目 (4 963 3 1 2 0 );国家重点基础发展规划项目“大陆强震机理研究”(G1 9980 40 70 4);中国地震局构造物理开放实验室基金;中国科学院创新工程项目 (KZCX2 1 0 1 0 4)共同资助
  • 【文献出处】 地质科学 ,Scientia Geologica Sinica , 编辑部邮箱 ,2002年04期
  • 【分类号】P588.1
  • 【被引频次】19
  • 【下载频次】360
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