Nd isotopic disequilibrium between minerals and Rb-Sr age of the secondary phengite in eclogite from the Yangkou area, Qingdao, eastern China

作者：Li SG^*; Sun WD; Zhang ZQ; Li QL

来源：Chinese Science Bulletin, 2001, 46(3): 252-255.

• eclogite
• Nd isotopic disequilibrium
• Rb-Sr dating
• Su-Lu UHPM belt

There are two generations of white micas in retrograded coesite-bearing eclogite from the Yangkou area near Qingdao, eastern China. The secondary phengite developed along the folliations in eclogite is the majority of the white micas. Nd and Sr isotopic disequilibriums between garnet and retrograded omphacite as well as secondary phengite have been observed. Consequently, the Rb-Sr ages ((193 +/- 4) Ma-(195 +/- 4) Ma) given by the tie lines of the secondary phengite + garnet or whole rock may predate the formation time of the phengite. The Rb-Sr age of (183 +/- 4) Ma given by the secondary phengite + retrograde omphacite is much closer to the formation time of the phengite indicating the retrograde age of eclogite instead of a cooling age of eclogite at 500 degreesC.

• 出版日期2001-2
• 单位中国科学技术大学; 中国地质科学院