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Chinese Physics C> 2004, Vol. 28> Issue(6) : 675-678 

Measurements of Trace Elements in Melt Inclusions by Synchrotron Radiation X-Ray Fluorescence Microprobe Techniques

  •  Institute of High Energy Physics,CAS,Beijing 100039,China2 Information Department of Geological and Mineral Resource Bureau of Jilin,Changchun 130022,China3 Institute of Geology and Geophysics,CAS,Beijing 100029,China

  • The enstenite and its melt inclusions picked up from mantle xenoliths at Longgang volcanoes in Jilin province are measured by synchrotron radiation X-ray microprobe techniques. Some element contents, such as K,Sc,Ti,Cr,Mn,Fe,Co,Ni,Cu,Zn,Ga,Sr,Y are calibrated by NIST SRM 612. The relative deviations of element contents analyzed in enstenit between X-ray fluorescence microprobe and wavelength dispersive electron beam microprobe are 15%,5%,7% and 8% for Cr,Mn,Fe,Ni,respectively. Chondrite normalized transition metal elements distribution pattern of inclusion is similar to that of whole rock analyzed by INAA, which implies that primitive magma experienced partial melting or segregation during ascending.
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YU Fu-Sheng, YUAN Wan-Ming, HAN Song, JIN Ke, HUANG Yu-Ying, HE Wei, DONG Jin-Quan, JIA Xiu-Qin, CAO Jie and WANG Hong-Yue. Measurements of Trace Elements in Melt Inclusions by Synchrotron Radiation X-Ray Fluorescence Microprobe Techniques[J]. Chinese Physics C, 2004, 28(6): 675-678.
YU Fu-Sheng, YUAN Wan-Ming, HAN Song, JIN Ke, HUANG Yu-Ying, HE Wei, DONG Jin-Quan, JIA Xiu-Qin, CAO Jie and WANG Hong-Yue. Measurements of Trace Elements in Melt Inclusions by Synchrotron Radiation X-Ray Fluorescence Microprobe Techniques[J]. Chinese Physics C, 2004, 28(6): 675-678. shu
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Received: 2003-09-10
Revised: 1900-01-01
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Measurements of Trace Elements in Melt Inclusions by Synchrotron Radiation X-Ray Fluorescence Microprobe Techniques

    Corresponding author: YU Fu-Sheng,
  • Institute of High Energy Physics,CAS,Beijing 100039,China2 Information Department of Geological and Mineral Resource Bureau of Jilin,Changchun 130022,China3 Institute of Geology and Geophysics,CAS,Beijing 100029,China
  • Received Date: 2003-09-10
  • Accepted Date: 1900-01-01
  • Available Online: 2004-06-05

Abstract: The enstenite and its melt inclusions picked up from mantle xenoliths at Longgang volcanoes in Jilin province are measured by synchrotron radiation X-ray microprobe techniques. Some element contents, such as K,Sc,Ti,Cr,Mn,Fe,Co,Ni,Cu,Zn,Ga,Sr,Y are calibrated by NIST SRM 612. The relative deviations of element contents analyzed in enstenit between X-ray fluorescence microprobe and wavelength dispersive electron beam microprobe are 15%,5%,7% and 8% for Cr,Mn,Fe,Ni,respectively. Chondrite normalized transition metal elements distribution pattern of inclusion is similar to that of whole rock analyzed by INAA, which implies that primitive magma experienced partial melting or segregation during ascending.

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